Prospecting for gold and silver in North America [microform]

Lakes, Arthur, b. 1844 · 1896 · Historical

THE kind reception given to " Prospecting for Gold and Silver" by the mining and prospecting fraternity, as well as the general public

This 1896 document, Prospecting for gold and silver in North America [microform], is preserved in the Mountain Man Mining Library for research and reference. Original source: archive.org.

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Arthur Lakes,

E 'PROFESSOR oF GEOLOGY AT THE STATE or Mines, GoLpEN Ciry, COLORADO, -

" Dodovits," . Cialeey of Colorado Coal : asain Deposits," Ete.

Second Edition.

Scranton, Pa. The Colliery Engineer ;

Moro ee te ee Hit eat oe th i ge ees ' me A as cath

Entered according to the Act of Congress in the Year 1896 i

By Tre Coitizry ENGINEER Co., '

Ia the Office of the Librarian of Congress, at Washington,

Preface To First Edition.

In preparing this little work the author has felt the difficulty which arises in a theoretical dissertation on so eminently practical a subject as prospecting. It seems like giving rules and prescriptions for hunting or fishing or any other natural or practical pursuit. Though theory and practice are not at variance wher: happily combined, yet either without the other proves very unsatisfactory. Thus, the reader of this book, should he start out armed only with its theory, will find himself for some time pretty much " at sea" when he comes to actual practice in the field. As, however, he baker obtains some piactical experience, he may find this little work of use to him. So, also, the seasoned prospector, who has hitherto trusted to luck, keenness of observation, intuition, and experience, may find himself in the future much better equipped by acquiring a little of the theory.

Whilst we have endeavored to give the prospector all assistance in our power, as to the best means of educating himself, describing his outfit, etc., we have devoted special attention to the description of such geo'ogical and other phenomena as he is likely to meet with in connection with his work, so that he may have an intelligent idea of them when he encounters them.

We have selected just as much material as we think would be most interesting and useful to him, saving him the time and trouble of wading through heavy tomes and laboriousiy picking out from a vast amount of, for his purpose, superfluous matter that which he will most require.

The work is intended to be a popular one, addressed to the average student, prospector, and miner, and to the

general public, ARTHUR LAKES. JANUARY 1, 1895.

Preface To Second Edition.

THE kind reception given to " Prospecting for Gold and Silver" by the mining and prospecting fraternity, as well as the general public, has made necessary a second edition. In this we have added to the text sketches of some of the principal prospecting regions of North America, which, besides illustrating the principles presented in the work, will, with their maps and illustrations, prove useful guides to prospectors who may venture into those districts. Having extended the scope of the work, we have accordingly given it a more general title, namely: " Prospecting for Gold and Silver in North America."

Respectfully, ARTHUR LAKES.

Boston Buiipinc, Denver, COoL., October 1, 1896.

Chapter

Contents.

aia PROSPECTING—PREPARATION AND OUTFIT FOR ORK, ry ° e e e

II.—TuHe Prospecror's Qantoey, : ; ' IiI.—Tue Prospector's PALEONTOLOGY OR Grove OF

FossiLs, . 4 e ; IV.—THE PROsPECTOR's Lrrnoxoey OR Srupy or Rocks, V.-—THE ProspecTtor's MINERALOGY, ' P e VI.—Ore Deposits, . : ° ' ° ' VII.—Various Forms or OrE Devosits, ' ° ' VIII.—RELATION oF VEINS TO Eruptive Forces, ' ° IX.—Go.p PLaAcgrs, . ' r ' é F ° ' X.—" Deep Leaps," . : ' XI.—Mininc REcions, SHowme EXAMPLES oF Ore Dr- POSITS, ; P i 'é

XII.—Ore Deposits IN Dapnatiecans 'Ronee: XIITI.—EXAMINING AND SAMPLING MINING PROPEKTIES, Pros-

PECTS OR MINES, . ; ' ' 4 XIV.—PrRospPecTING IN VARIOUS Rraions, ; ; ' ' XV.—GEOLOGY AND MINERALOGY OF ALASKA, . ' XVI.—BritisH AMERICA, ' i ; P .

XVII.—CALIForNIA, ' °

XVIII.—Montana, DAKoTAH, he AND New AMasicd,

XIX.—TuHE GoLD OF THE ORTIZ MOUNTAINS AND GALIs- TEO AND Rio GRANDE PtaAcers, N. M., XX.—Tue Goitp anv Sitver Ore Deposits oF THE MERcur District, UTAH, XXI.—SaA.tTinc Mines, . XXII.—Prospector's Too.s, AND How TO SHARPEN AND Temper THEM,

XXITI.—Some ELEMENTS OF iiine Law Riunarena TO Pros:

P ECTIN G , ° e e e e e e ° e

Page

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Prospecting For Cold And Silver In North America.

Chapter I.

On Prospecting—Preparation And Outfit For Work.

The regular prospector, as rule, has at some time of his chequered career had some actual experience in the mines themselves, from which he has learned by observation the appearance of different ores, their different values, how the veins appear on the surface, how to open a vein, and the uses of pick, shovel, and blasting powder. In a word he is a miner who has become too restless to stick to steady work, and so follows the more uncertain and precarious livelihood of seeking for new and undiscovered veins, many of which even in an old mining district may yet be discovered covered up by brush or debris, whilst a new district offers a most enticing field. These mineral veins or ledges may make him in a moment a comparatively rich man, and if he finds them, they will cost him nothing, only a simple compliance with the inexpensive regulations of the law. So the life of a prospector offers many attractions to one who is restless and loves to roam and loves to find something new and is not afraid of considerable hardship. To save a vast amount of time and labor, he should acquire knowledge. Thus, for instance, if he were prospecting for coal he would be wasting his time in hunting for it in granite, or if he wes hunting for the precious metals, he would lose time in looking for them among the

unaltered sedimentary strata of the prairie. This is merely for example, but an infinite variety of knowledge is necessary for him in his vocation, besides even that of the simpler elements of geology, such as the knowledge of different kinds of minerals, and their value, the kind of places and peculiar rocks they are associated with, their appearance on the surface, etc., etc., together with some knowledge of assaying or blowpiping or panning.

In 4 newly discovered camp, men will rush in for a few weeks, work a little in the different mines, sufficient to give tuem an idea of the kind of ores and rocks and other circumstances in the locality, and then will strike out on their own account aiid prospect around the camp for new veins or extensions of those already discovered. An extension, by the way, of a very rich discovered lode is not always to be reliedon. Nature seems often to concentrate her riches at one point, and leave the extension barren, as in the case of the Comstock of Nevada. But little wealth has been found outside of the great lode and mine itself.

The best education is in the mines themselves, so a novice on arriving at a tee region had better spend as much time as possible in practical work, in, and around the various mines, before he launches out prospecting. A prospector can ey carry about much assaying or other pi pines with him for determining the character or value of ores he may find, and hence it is well for him to accustom himself to these ores in the mines themselves, Also he should acquaint himself with the peculiar ores of each particular district, before he attempts to prospect in its vicinity, for an ore such as coarse-grained galena in one district may be generally rich, whilst in another it is remarkably poor in silver.

The best previous education for a prospector would be a course at a school of mines, where he will learn the elements of geology, mineralogy, assaying, etc., and next to that, practical work in the mines themselves, and lastly the

prospecting field. A little knowledge of blowpiping may also help him, which he may acquire at his school.

Having left his school, he should learn the practical use of the pick, drill, and blasting powder. By working around 2 toncentrator he will learn the difference between ore and gangue rock; and " picking" or "sorting" ores will

teach him at sight the values of ores. The prospector should know how to open his vein or ledge, when he finds it, with pick, shovel, and blasting apparatus. A little carpentry will teach him how to make a handwinch, and a ew lessons in blacksmithing will teach him how to sharpen and temper his tools, for there will probably be no blacksmith's shop, or carpenter's either, within miles of where he may go. Other prospectors will teach him how to use his pan or iron spoon for testing ores, and various other dodges and makeshifts. An important point is to learn how to arenes appronmatsty the quantity of ore in, and value of, a ledge when he has found one. Valuable ore on a ledge lies in poor strings, bunches, irregularly distributed through the quartz or other material of the vein; he should learn to tell at sight the relative proportion of ore and gangue. He would do well to study the result of working ores in a mill or furnace, such as trying to estimate the yield of bullion of the ores which are mined, taking them in weekly or monthly lots. With some such preliminary knowledge he is ready for the field.

His Outfit.

The following list of necessaries by Mr. A. Balch in his "Treatise on Mining" is as full as can be given by any one, and is more than the average prospector generally needs.

" First. Two pairs of heavy blankets weighing about 8 pounds each.

" Second. A buffalo robe or a blanket-lined poncho.

" Third. Sw.t of strong gray woolen clothes, pair of brown jean trousers, a change of woolen underclothing, woolen socks, pair of heavy boots, soft felt hat, three or four large colored handkerchiefs, a pair of buckskin gauntlets, toilet articles, etc. All should go into a strong canvas bag.

" Fourth. A breech-loading rifle or shot-gun and a revolver. Around his waist a strong sash to :arry his holster and knife, in a sheath. His ammunition, if his revolver is large bore, may conveniently fit both his rifle and revolver. Pipe and tobacco.

" Fifth, A sure-footed native or mountain pony. A Mexican saddle with its saddle-horn, straps, etc., to tie on various things, such as his pack, bags, water-canteen, etc.

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The left stirrup may be fitted with a leather tube, in which the rifle-barrel may be placed. A strap around the saddle horn will secure the gun-stock. The long lariat or stake rope for tethering his horse should be coiled up and tied by a strap to the saddle-horn.

" Sixth. For prospecting, a 'poll' pick and prospectingpan made of iron or a horn spoon should be carried. The pan is also useful besides for washing out sand, as a dish or bathing-vessel. A large iron spoon for melting certain metals is likewise to be carried, and in some cases a small portable Battersea assaying furnace.

A Prospector And His Outfit.

" Seventh. A frying-pan 8 inches diameter, of wrought iron, a coffee pot, tin cup, spoon and fork, and matches in tin box, pocket compass, a spy-glass, or pair of fieldglasses.

" Eighth. Provisions, bacon, flour, beans, coffee or tea, pepper, salt, and box of yeast-powder, all packed in strong bags, to go into a canvas sack. A few lessons in the kitchen on cooking will be advantageous before starting.

" Ninth. Packing the bronco. Place a folded blanket on the horse's back; on this lay the saddle. The saddle-bags contain smallthings. The bags with provisions are placed behind the cantle of the saddle; on top of this the of clothing. The pick goes on top tiedbyathong. Coffeepot and frying-pan are lashed on the hags."

A Prospector'S Tools.

1,2. Picks. 8. Pan. 3 Long handled Shovel. 9g. Horn Spoon. 45. Drills. 10. Iron Spoon. 6. Heavy Hammer. 11. Fuse.

Sometimes a prospector takes a horse to ride on and another as a pack animal, or a donkey only. For grass and water for his horse he must trust to the country. He will fix his temporary camp in some suitable location, where these are to be found, and thence, as from headquarters, prospect daily the adjacent country, returning nightly, it may be, to his camp.

Brief Sketch Of Prospecting.

We may divide the prospecting for the precious metals into two general classes: hunting for gold in gold placers; hunting for gold and silver bearing ledges or veins or deposits.

"Placers" are places where gold, having been torn from

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the ledges and rocks by denudation, by water and ice, is swept down by these agencies till it finally finds a restingplace. Gold, being heavier than quartz or country rock,

Panning Gold At Cripple Creek, Colorado.

sinks to the bottom first. If the streain is violent, it will carry the gold on, if fine, till it comes to an eddy or pool, where the waters are more quiet, und there it will sink. The water carries the clay and lighter stones still further

on. In this way millions of tons of rocks containing more or less gold disseminated through them may have been reduced and the gold set free, or the gold may have been derived from a few individual gold-bearing ledges or veins.

The prospector takes his pick, shovel and pan, and his horn spoon, and finds perhaps an old dry river-bed where the water has ages ago receded. At some point the sides of this old river-course widen out suddenly, forming a basin. " Here," says the prospector, " there must have been

Finding The Float.

an eddy," and he prospects it accordingly; at another point he finds a place where the water must have run over a rock and made a waterfall; at the bottom he digs again.

He loosens the soil with his pick, and shovels it out; ata certain depth, which may be from 5 to 20 feet or more, he strikes " bed-rock," which may be granite, shale, sandstone, or some other rock. Here he looks for nuggets, and with his knife digs into all the little crevices of the rock to hunt for them and for scales and wires of gold.

Also whilst sinking his shaft, he pans the gravel carefully at various depths, especially where there are streaks

of clay or "black sand." The latter are grains or little pebbles of magnetic iron-ore, a common accompaniment of gold, altered relics of the iron pyrites in which the gold was originally contained.

He fills his pan half full of water, throws into it a shovelful of dirt, first picking out the pebbles, stirs the mass with his fingers till the water is fully charged with the clay, and gradually winnows out all the clay. Filling the pan again with water, he gives it a peculiar circular motion and each little wave of sand passes off till the whole is winnowed off, and at last he sees specks of gold shining free in the bottom of the pan. Then it is not difficult to estimate approximately the amount of gold to the bushel or cubic foot of earth of the placer, and thus to estimate the approximate value of the placer. He then locates or stakes out his placer claim according to the regulations of the U. S. Government, which by a single individual cannot exceed twenty acres.

The second class of prospectors are those who try to discover ore deposits, ledges, or veins, "in place," that is, in the hard rocks of the hills.

The prospector's first effort is to find "float." A vein outcropping on the surface becomes oxidized and crumbles by action of the atmosphere, rain, etc.; pieces break off and fall down-hill. Scme of this float is barren quartz or country rock, others may be mineralized. Commonly "float" is a rusty, spongy mass of rock, showing besides iron often some copper stains, and in it there may be grains of galena, pyrite, or some other ore. He tries to trace this " float" to its home in the ledge whence it came. Of one thing he is certain, the " float" must have rolled down and not wp hill. If the " float" is fairly scattered over the lower zone of the hill, and no " float" is found above that zone, on the top of that zone he will hunt for his ledge. If the "float" is all over the hill he assumes the ledge is on the

top.

tt he finds his " float" at the mouth of a canyon or watercourse, he walks up that water-course, noticing not only the "float," and its diminishing or increase, but also any peculiar rocky pebbles, such as a peculiar porphyry, perhaps, which he may by chance recognize again further up in place, and give him a hint as to whence the stream

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derived most of its material of pebbles. He notices if the "float" fragments increase as he proceeds, and whether they suddenly cease at a certain point; at that point he hunts for the ledge on either side of the canyon, and breaks off any pieces that may look likely.

Having found the ledge and traced its croppings, he tries to find out its approximate value. This he does by breaking off at intervals along it likely looking fragments of the rock, grinding them up to about the size of peas. He mixes these well, and takes a half of them, reducing this to fine powder and again halving it, till of the whole ledge he can carry away an averaged sample of a few ounces. He may wash this in his pan to see if there is any free gold in it; other ores he will recognize at sight. These samples he will have assayed and the returns will show the approximate value. He measures the length and thickness of the vein, and examines the wall enclosing it.

He then proceeds to locate or stake it out by measuring off a parallelogram 1,500 by 600 feet. At the corners of this he places piles of stones, and in one or more of them places a stake of wood on which he writes his name, a description of his claim, and the date. At the nearest recorder's office he files a copy of this document. He must do a certain amount of improvement work on this annually, such as digging a ten-foot hole or putting up a cabin or some work equivalent to the value of $100, so as to hold it. He may also claim a mill-site on non-mineral land adjacent not exceeding five acres. Now the property is his to do as he likes with it.

The Geological Training Of A Prospector.

One of the first things for a prospector for gold and silver to acquaint himself with is the elements of geology. He can read this up theoretically in many excellent treatises and manuals, such as LeConte, Dana, and Shaler's Manuals, and Geikie's Hand-Book of Field Geology, etc., and become learned in the names of eras and epochs, and the jargon of scientific names of fossils and minerals, and varieties of rocks; but let him not imagine at the end of this process that he " knows geology."

Geology can no more be learned by means of a book,

without field-work and the actual personal contact with nature and rocks, than chemistry or assaying can be acquired without ever using a test-tube or a cupel. Tue student may, perhaps, be unfavorably situated for this practical field-work. There may be no mountains or upheavals of strata, or deep natural ravines within available distance to study. He is located, perhaps, on the great, monotonous, flat prairie. Very well, then, let him study what lies nearest him. This same flat, monotonous prairie has an interesting and wonderful history. Let him read up what he can find about this in his books, then go out and examine what he can of the few feet of horizontal strata exposed in some shallow water-course or dry ravine; examine minutely, both with eyes and microscope, the minerals composing these strata. Let him classify and collect and note the different kinds of pebbles scattered over the surface, or in the bed of a brook. Let him speculate as to the cause of the undulations of the surface, the deposition and peculiar character of the clays forming the soil. Let him study thoroughly the geology of his native village, his immediate surroundings, . The knowledge and practical habit of observation so acquired will lead later to more extensive studies in wider fields. A student may be shut up in a big city; let him study the pavingstones of the streets and visit the stone-yards of the masons. It will pay him better to take a trip to some distant mountain region than to buy another expensive book on geology after he has mastered the first bare elements. Nothing like field-work, eye practice, and hammer practice. The student should endeavor, whenever he possibly can, to verify by actual vision and personal experience whatever he reads in his books. When traveling, let him always carry a geological hammer with him, and at any station the train may stop for a few moments step out and try togeta specimen of the country rock; at the same time let him study all he can of the geology of the country he is passing through from the windows of the train, aided perhaps by a geological map. The genuine prospector is always looking about him, is everlastingly cracking stones, has always his eye wide open for "something kind o' curious."

If he is near some mountain region, where, as in Colorado, the whole strata of the earth's crust is upheaved and

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A Vertical Section of the Earth's Crust in Colorado.

exposed, along the mountain flanks, in the depths of the canyons, or on the summits of the peaks, after studying his manual, let the student get, if he can, some published geological report on such a per vebid such as those of the U. S. Geological Survey, abounding in illustrations and geological sections. Let him take this book in hand and go to the very place described and pictured as a geological section, and with his hammer study each member of the section closely. This will make him familiar with the different geological periods, formations, rocks, minerals, and fossils, as they actually appear in nature rather than as his imagination has supposed them to be from his study of the text books: book geology and field geology are not always in perfect harmony.

Having studied and learned ore local section well, such as that cut by a stream along the foothills of a mountain range, let him repeat the course at the other and more distant points. He 'vill find at each locality, though the main features are the same, there is always an interesting variety, such as new fossils, peculiar minerals, changes of dip, faults, or other structural peculiarities.

Along the flanks of a mountain range, a prospective pros-ector

cannot study too many of these geological sections.

aving become familiar with these foothill sections, he is prepares to plunge into the heart of the range itself. At

rst, and for long distances perhaps, he will encounter only gene rocks forming the axis and core of the range.

hese are well worthy of study and full of variety. Later the canyon may open into some mountain valley or park, where the strata he studied on the foothills or prairie border are again repeated and he finds himself again at home. Seizing upon some well-defined and familiar representative of a geological horizon, from this as a standpoint he soon reads off the succession of the rest. Here, however, the appearance and texture of the rocks will probably be different to what they were in the foothills. Heat has so changed or metamorphosed the sandstones and shales that they are scarcely recognizable. as the same rocks as those of the foothills. Yet even here a highly silicified fossil shell, or a leaf impression on shales, or sandstones changed into slates or quartzite, will give the prospector his clue and his desired and definite geological horizon, and

he will have little difficulty in again arranging and grouping correctly the rocky series. But a prospector has a "practical end" in view. He is " after the precious metal," gold and silver, not after "pure science' or "fossils or sich"; what practical use is there, he may ask, in this same careful study of geological sections, where probably there is not a speck of gold or silver? Simply that minerals and metals of economic value, such as gold and silver, are more frequently found in the rocks of certain geological periods than in others. Locally this is especially true. For instance, nearly all the silver-lead deposits of Colorado are found in: certain bed of limestone not over two hundred feet thick, to be found only in one geological period out of many others, viz.: the lower division of the Carboniferous. It would naturally then be advisable for a Colorado prospector to be able surely to identify this limestone, as well as the geological horizon in which it occurs, among the various other limestones of various other periods and ages in the mountains.

Again, gold is mainly confined to crystalline rocks of Archean age or to porphyries associated with these. A prospector should be familiar with these rocks and their varieties. Gold is also found in the placers derived largely from the breaking up of these rocks; the ability to distinguish the different pebbles may lead to the source whence the gold was derived. Familiarity with rocks of all kinds is a necessary prospector's education in itself.

Geological Sections Of Colorado.

In illustration of what we have said, let us take the two engraved generalized sections showing all we know of the crust of the earth as exposed in Colorado. Plates I and II.

Plate I is a vertical section of an ideal cliff, showing all the members of the various periods in a stupendous cliff resting on fundamental Archean granite at the bottom of canyon. Plate II represents the same rocks and succession of strata displayed in upturned " hog backs" along the flanks of the mountains and foothills on the border of mountain and prairie. Both of these are ideal sections " generalized" or "made up" of actual partial typical sections found in different localities in Colorado, the vertical

one in detached and sometimes widely separated districts in the heart of the mountains; the other at similarly distinct and different localities along the banks of the various rivers issuing from these canyons in the mountains, cutting their way through the upturned strata of the flanking foothills and debouching on the prairie.

It is very rare to find at one locality anywhere in the world a complete section of the earth's crust exposed. The nearest approach to this in Colorado is the remarkable section between Colorado Springs and Manitou, which shows along the wagon road the succession of strata from Archean to Quaternary.

One of the most remarkable vertica/ sections in the world is in the grand canyon of the Colorado River, where the stupendous cliffs show in one face, a thickness of some 6,000 to 7,000 feet of strata, representing several geological

eriods, but by no means a complete section of all that is nown of the earth's crust.

To show how difficult and rare it is to get a complete section of a// the pence. in the earth's crust, we may state that sometimes the rocks of a single geological period are

from 10,000 to 20,000 feet thick. A canyon might thus be cut to a depth of 5,000 feet, and yet be in only part of a

single earth-period.

By far the most extensive and available sections are, like those represented in the engraving, along the courses of streams on the flanks of a mountain range. It would bea formidable task to scale a cliff 5,000 feet high and examine minutely, in ascending, each of its geological divisions; whilst, on the other hand, in the foothill regions, a pros. pector may walk over and mark and study as much as 10,000 to 40,000 feet of strata along the banks of a river in a single afternoon. In the Weber Canyon in Utah, as much as 40,000 feet of strata, composing the flanks of the Wahsatch Range, can be seen by the traveler from the windows as he glides through in the railway car, and the inquiring prospector or geologist can examine and study this vast section leisurely on his mule or on foot, without doing any climbing and on a good road. Smaller partial sections can be similarly studied along many of the streams issuing from the Rocky Mountains among the foothills of Colorado. Such, for example, as at Boulder Creek, Clear Creek, Bear

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Creek, the Platte River, and, most complete of all, the one along Fountain Creek, near Coiorado Springs, which we have already mentioned. Similar sections can be found in most mountain regions, such as the Adirondacks in the East, and the Sierra Nevada and Coast Range in the West of America. We emphasize again that the close study of these is the best preliminary step we know of in a prospector's geological education. Let us now examine our ideal generalized Colorado section, which we will suppose to be all exposed along the banks or canyon of a single river. We will start from the Archean granite in the canyon, thus giving us a sure and known and lowest possible geological horizon to begin with.

The Archaan,

This Archzan we find to be composed toward its core, of solid, shapeless (amorphous) crystalline granite, which seems to have been fused out of all shape by water and fire, or aqueo-igneous fusion. With this, but more characteristic of the upper and outer edge of the Archean, the granite assumes a more stratified and bedded character. which we designate as " gniess" and interbedded with it at intervals are distinctly laminated or finely leafed strata, called schist: all these varieties are composed of the same minerals in different arrangement and quantity, viz., mica, quartz, hornblende, andfeldspar. As these rocks are semi-igneous or metamorphic, we find no fossils in them. Traversing all these Archean rocks and cutting them at all sorts of angles, we may notice some eruptive dykes of porphyry, which were once certainly molten and have ascended in that state through fissures opened in the rocks from depths and sources unknown. As we approach the edge of the granite we may even see some of these molten rocks, insinuating once fiery tongues among the weak places and bedding planes of the overlying sedimentary strata, as represented in the diagram, where one dyke is shown to have sent out so thick an intrusive sheet of porphyry (see Plate II ) between the overlying limestones, that where subsequent erosion took place, this thick sheet, by its superior hardness, was left to form the highest cap of the mountain, as on many of our prominent mountain peaks such as Mt. Lincoln and others in South Park.

Besides these rocks, the prospector will observe numbers of quartz and pink feldspar veins of all sizes, some mere streaks and occupying incipient fissures or weak places (veins of segregation), others occupying large, well-defined fissures or jointing planes (so-called true fissure veins). Some of these may or may not carry metal, gold or silver, lead or copper; at any rate he wili pay them especial attention, particularly if any of them louk at all decomposed or a or are in close proximity to an eruptive porphyry

yke.

The Cambrian.

Now the prospector emerges from the Archean granite and finds the first true sedimentary, water-formed rocks lying where the ancient seas placed them, on the eroded upturned edges of the granitic series.

If this section shouid be near the plains or foothills, this first sedimentary rock will be a sandstone, pure and simple, or a conglomerate of little pebbles, but in the parks and centre of the mountains where these ancient strata are most conspicuous, the first rock lying on the granite is a hard, white, semi-crystalline quartzite or metamorphosed sandstone. He may possibly find some obscure signs of ancient fossil shells in this series, which is called the Cambrian now, though formerly it was held to be only a lower division of the Silurian. In Colorado these Cambrian rocks rarely exceed 200 or 300 feet in thickness, but in other regions they are often very much thicker. In this series the prospector may look for precious ore, more especially gold. He will carefully look also for intrusions of eruptive porphyry in this series, as at the junction of this with the quartzite, ore is most likely to be found. He will also observe any rusty signs filling cracks, as good indications of gold-bearing ore. Silver also may be found associated with lead or zinc.

Silurian.

Walking along, he next comes to some 200 or 300 feet of drab-yellowish or light gray thin bedded limestone of a dolomitic character, characterized by numbers of little white flints or (rarely in Colorado) by some fossil shells,

which, by reference to the engravings in his manual, he finds to be Silurian, and so recognizes the series. Here he may find indications of lead, silver, or other ores, but not much gold, as a rule.

Carboniferous.

The next series of this should, according to the text-books, be the Devonian, characterized by fossil fishes and " Old Red" sandstones; but the rocks of this epoch for some reason are missing in Colorado. Instead of this, resting on the Silurian, he finds a thick bed of heavy-bedded, massive, "blue-grey" limestone, characterized by black flints, and at rare intervals by fossil shells and corals, which again, by reference to his book, he finds to be characteristic of the Lower Carboniferous. This limestone, when traversed by sheets of eruptive porphyry, has yielded at Leadville and at Aspen and New Mexico and Arizona some of the largest silver-lead deposits in the West. In fact, throughout the West it may be considered as the main silver-lead horizon. This limestone is generally between 200 and 300 feet in thickness and readily recognized by ts position relative to the Silurian below it, and the massiveness of the strata and their dark gray color. It is commonly called the " Blue Limestone" in Colorado.

Middle Carboniferous.

Next on this is a bed of dark black shales in which thin seams are sometimes found, and fossil plants like those in the coal strata of Pennsylvania, sufficient to show that it, too, belongs to the Carboniferous. This is followed by some 2,000 or more feet of "grits," rough, hard, gritty sandstones, partially changing into quartzite, akin to the " mill-stone grits" of the Eastern States. A few limestones occur in this thick Middle Carboniferous series, which locally, when capped by porphyry, produce silver-lead deposits; but generally speaking, the " grits" are unproductive in Colorado.

The Upper Carboniferous consists of beds of gypsiferous shale and heavy, brownish-red conglomerate sandstones.

Triassic " Red-Beds,"

From these we pass into a series of heavy-bedded, coarse conglomerate sandstones of a brick-red color, commonly known as the " Red-Beds" in Colorado; little indications of ore are to be expected in this series. The prevailing reaness of the series makes it an easily recognized geological horizon in Colorado and elsewhere. The thickness in Colorado varies from 1,000 to 2,000 feet.

Jurassic,

Next, the prospector comes to a softer and more variegated series, consisting largely of pink, green, red, or maroon marls and clays, with some thin limestones and red sandstones. This is the Jurassic series, in which some remarkable lizard remains, called Dinosaurs, have been found, proving the correctness of its Jurassic name. This is not a likely mineral horizon, generally speaking, in Colorado.

Cretaceous.

These softer beds are capped by a hard massive sandstone about 200 feet thick, forming by reason of its superior hardness a prominent hog-back in the prairie or foothill region. Fossil remains of leaves show it to be a land and fresh-water group, which is called the Dakotah group.

This group in Colorado forms the base of the great Cretaceous system; lying on it is an enormous thickness of drab shales with a few limestones characterized by fossil sea-shells, showing the group to be the marine Cretaceous, likewise a poor prospecting-ground. Toward the upper portion, these shales pass gradually into heavy-bedded sandstones, containing several seams of coal and many impressions of tropical foliage. This is the Laramie group of the Cretaceous, evidently of fresh-water origin, and noted as the main coal-producing horizon in Colorado and the West.

Tertiary,

On this, at a somewhat gentler angle, even to horizontality, rest thick beds of shale and clay and conglomerate, composed of volcanic detritus and pebbles, showing that at

the time these Tertiary beds were being laid down by large fresh-water lakes and marshes surrounded by tropical foliage, volcanic eruptions on a grand scale repeatedly occurred. Hence it is that many of the Tertiary beds are preserved from erosion by being capped with volcanic rocks, such as basalt, andesite, or rhyolite, as at the Table Mountains at Golden, on the Divide near Colorado Springs, and elsewhere in Colorado. One of these lava-capped "mesas" is represented in the section, Plate II. Fossil leaves and coal-seams are found in this period.

Quaternary.

Lastly, strewn indiscriminately over all the formations, is the "Quaternary drift," composed of loose pebbles and sands and clays, the material derived from rocks of all the periods through the agency of glaciers and streams.

Here the prospector will pan for his gold placer, and in his search may possibly come across the teeth or tusks of the great Mammoth or fossil elephant, together with the first indications of the presence of primitive man. The pebbles by their variety will form a fertile subject of study to determine to what class of rocks they belong.

This ends the prospector's first preliminary lesson in Colorado; but, taking this section as a type, he may, to his great advantage, similarly study other sections far remote from Colorado.

In Colorado, if he knows this section by heart, he has the key to nearly ail our mountain structure, and will be at home wherever he goes. He will be struck, too, to see to how small a portion of this great section the precious metals are more or less confined, principally to the Archean and Paleozoic rocks.

Chapter Ii. The Prospector'S Historical Geology.

In our last chapter we gave some hints to the prospector how to commence his geological studies, and gave him an example of a geological section of the foothills and mountains

of Colorado, and how to study it in detail practically. Having completed this study, if a thoughtful man, he will like to know more of the natural history of all this section of the earth's crust: what is the natural history of the Archean, the Cambrian, Silurian, etc., why do some of these strata contain sea-shells, and others land-plants, why are some evidently of marine, and others of fresh-water origin, and particularly why are some especially metalliferous, and others not so much so? We propose, therefore, in this chapter to give him a brief sketch of the earth's history as exemplified in the section, Plates I and II.

Hypothetical Origin Of The Earth.

The world was not "spoken inio existence ready made" in the state we now findit. It has attained this condition through a multitude of gradual changes and revolutions which have taken millions of years to accomplish. The remote history of the earth's origin is a matter of hypothesis and speculation. There are reasons for supposing that at one time its elements were in a gaseous condition, and that this planet was an incandescent luminous cloud revolving through space, gradually consolidating into a molten ball surrounded still by an atmosphere of gases, a condition perhaps not very unlike that of the sun, whose interior by some is supposed to be passing into the molten state, while its exterior consists of various incandescent gases arranged more or less according to their specific gravities. The spectroscope has detected the elements of some of our earth metals and minerals in the sun in a state of vapor. The ultimate source of the precious metals is again a matter of speculation, like the nebular hypothesis we have alluded to, by which the earth, as we have said, is supposed to have arrived at its present condition as the result from the gradual cooling of an incandescent mass; and as the specific gravity of the crust is much less than that of the whole mass of the earth it has:been inferred that the heavy metals must be in much larger proportion in the interior of the earth than in the rocky crust, though this greater interior specific gravity might be also accounted for by the rocks of the interior being much more tightly packed by enormous pressure than those near the surface. Volcanic

&

emanations and hot springs contain metallic minerals; so also do the waters of the ocean. But we know not from what depth the former came, nor from what source the latter derived them. As circulating waters take up and throw down their metallic contents under varying conditions, the same material may have been deposited more than once, and in more than one form, since it reached the rocky crust.

Upon the cooling of the ball, a crust formed like that on molten iron, crumpled and corrugated by contraction, due to cooling, into an uneven surface, with comparatively slight elevations and depressions, and doubtless broken through here and there by great fissures and volcanic craters, through which the molten flood beneath poured out in volumes, adding to the thickness of the congealing crust.

Upon such a surface the gaseous atmosphere, gradually cooling and condensing, descended as hot chemical rain, and filled the troughs of the crumpled surface with a hot, chemical, steamy ocean. Whatever land of primitive lava rose above this ocean was battered by the waves, reduced to sediment, and deposited as the first sedimentary strata in the bed of that primeval ocean, the eruptions from below the thin crust doubtless contributing largely to the same material.

Archaean Age,

Thus, perhaps, were formed the first stratified rocks of the world, which we have an opportunity of actually seeing and studying, viz.: the granitic series, with its varieties of gneiss, schist, syenite, etc., and as this is the beginning age so far as we know, we call it the Archean, the Greek for beginning. It would seem probable, however, that these granitic rocks forming the axes of our mountains may not, at least in part, have been the very first rocks of the crust, for we observe some of them, such as the gneisses and schists, to be stratified, and to show elements in them seemingly derived from other and still older rocks, which latter may or may not have belonged to the original cooling crust. Some geologists claim that the Archzean is the first cooled crust and attribute it to a molten origin. This may be true for the seemingly fused massive amorphous granites

(though these may be but the result of aqueo-igneous fusion of sediment or extreme metamorphic action), but scarcely for the stratified gneisses and schists, though it is to be noted that a sort of stratified or schistose structure is sometimes observed in truly igneous rocks and may be induced by peculiar arrangement of minerals, pressure, and cleavage, instead of water lamination.

The subject is a difficult one and too abstruse for the limits of this work.

In the scale of geological periods in the text-books, we sometimes find this great Archean divided into two or more groups, such as the Laurentian, Hurenian, and of late the

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PiaTE III.

Archean Rocks.

Algonkian. The Laurentian is the oldest and may be called the Archean proper, whilst the Huronian and Algonkian may he grouped generally as Pre-Cambrian, or series of rocks laid down after the Laurentian and before the Cambrian. All the rocks are of a highly crystalline order and have a peculiar and distinct general appearance, different, as a rule, to those of any subsequent geological periods and so not easily mistaken for them, consisting in the lower division mainly of granite, gneiss, and schists, and in the upper divisions of gneisses, schists, quartzites, slates, some marble, serperitine, etc. The upper or Pre-Cambrian series is not nearly so universally found as the Laurentian or

Archean proper. In Colorado we find the Pre-Cambrian represented locally in South Boulder and Coal Creek canyons, along the foothills, also near Salida in the Arkansas valley, in the Quartzite range, and on the road between Ironton and Ouray in the San Juan Mountains. The new Kootanie silver-mining district of British Columbia seems to be largely in these Pre-Cambrian rocks. This Pre-Cambrian is usually very thick, numbering many thousands of feet.

It is distinct from the Archean proper or Laurentian by lying on the latter at a different angle, in other words "unconformable." The rocks, too, do not contain so much of the heavy massive granites and heavy-bedded gneisses as the Laurentian, but are more characterized by quartzites, by conglomeratic gneisses and schists, and show clearly that, though highly metamorphosed and crystalline, they are of true fragmental and aqueous origin, for the pebbles in the gneiss are often very distinct, and ripple-inarks are not uncommon on the quartzites and slates and schists. The material was doubtless derived by waters from that of the underlying and older Laurentian. The whole Archean series, however, has evidently passed through an ordeal of heat, such as is called aqueo-igneous heat, and all its elements are in a highly crystalline condition. Its strata are intensely folded and crumpled. See Plate III.

Signs of life, in the upper series even, are exceedingly obscure and doubtful, such as graphite and possibly corals. Great iron-beds also occur, indirect proofs perhaps of the previous existence of life.

We have been thus particular with this Archean Age, because its rocks are of great importance to the prospector, being the main repositories of gold, silver, and the precious metals throughout the world. Moreover, many of the other and newer rocks containing gold and silver have been made from the detritus of this, and the gold placer-beds largely from the detritus of the rocks and porphyries found in this age. Thus the Archean may be considered as the parent of nearly all the other rocks. When later we have studied the origin of ore deposits, we shall see how eminently the Archean Age, with its attendant heat, chemical reactions, fissuring, metamorphism, and volcanic eruptions, was favorable . the diffusion and concentration of precious ores in its rocks,

' 30

Cambrian And Silurian Ages,

Cooling and consequent contractions still progressing in the globe, fresh and greater wrinkles and corrugations were caused on the surface of its crust, and some of these granite sea-bottom strata were crumpled up, till the crumples arose above the then universal ocean as low islands or reefs. The ocean had by this time cooled sufficiently to support low forms of marine life, and so along the flanks of these gigantic islands corals formed reefs, shell-fish swarmed and sea-weeds grew. Sands formed by Lj the waves from the material of the granite were laid down 14 as shore-line beaches, often mixed with shells; and in i] deeper water corals were forming limestones as at the ¢ 4 present day, both, by time and pressure, consolidating into hard rock, eventually, it may be, metamorphosed by heat into a semi-crystalline hardness, as in the case of the Cambrian quartzite and Silurian limestones, the latter sometimes changed to marble. If these Cambrian quartzites were formed from the detritus of the granite and the granitic series is the source of gold, it is not surprising that we find the Cambrian quartzites /oca//y rich in gold, as they were the auriferous sea-beaches (like those of to-day in California which are gold-bearing) of that period, later consolidated into hard rock. In Colorado the Cambrian quartzites are only locally prolific in gold, as at Red Cliff, but as they have hitherto been much overlooked by prospectors they are worthy of closer attention by the goldseekers. The limestone not being of a true fragmental origin, but formed by the slow work of corals, could not be expected on consolidation to bea recipient of gold, but later by its peculiar chemical composition, of which we will speak hereafter, and by its cavernous nature, it furnished a more convenient receptacle for silver and lead ores.

' So then in Colorado and in other regions, we find first ! the upheaved crumpled granite of the old Archean island,

and on these the Cambrian sandstone or quartzite beach of : " golden sands" with some fossil shells, and upon this again Silurian limestone with relics of fossil! corals and shells. So we call these ages the Cambrian and Silurian, because

3!

the fossil shells and corals are peculiar to those ages and distinct from those of later periods or the present day. North America at the beginning of these eriods was barely outlined by a few granite islands congregating mainly in the region now occupied by Canada, whilst one or two reefs or scattered ci:ains of islands marked the site

PiaTE IV.

America at Close of Archean.

of the Eastern ranges of mountains, and a few parallel granite islands outlined the site of the principal uplifts of future great ranges of the Western Cordilleras. All else was ocean, and that ocean was depositing its Cambrian beaches and Silurian coral limestones against or near these granite islands, destined in time to grow into lofty mountain ranges and to become the backbone of the American Continent. See Plate IV.

Devonian.

The Devonian, which should come next in order in the geological tree, appears to be absent in Colorado, but is well

shown at the Eureka Mines in Nevada. The rocks appear to be mostly marine limestone full of corals and shells and a few remains of gigantic fishes, for which this age was celebrated. Land plants and some coal are found in it in the East. Lead silver ores may be expected in the limestones of this age, and in Cornwall (England) Devonian slates traversed by quartz porphyries are the main rocks carrying tin ore, a metal very scarce at present in North America. These ages we are speaking of are separated or distinguishable from one another by decided and characteristic changes in the fossil, animal, and vegetable life existing

:

Plate V.,

Section Showing Unconformity of Geological Eras,

between one age and another; also in some countries by marked unconformability of the rocks, #.¢., the rocks of one age lying at a different angle upon the upturned rocks of a previous age, marking great oscillations between sea and land.

In America, however, these oscillations between sea and land seem to have been ...ss than in Europe, and we find a general uniform rise of the continent from the primitive oceans, and an orderly succession of strata lying against the flanks of the ever-rising granite nucleus of both mountains and continent. Hence to distinguish the different ages we are driven more to the study of fossils and lithological peculiarities than deriving any help from observed marked unconformability. See Plate V , in which the strata of the different eras lie upon one another at different angles, and the glacial and Quaternary drift pebbles and clays are strewn unconformably also over the tops of the uptilted and eroded strata of all the eras beneath.

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stinistic ting

Carboniferous,

In the Eastern States, as the American continent gradually rose from the sea, and to the granite islands had been added a Cambrian, Silurian, and Devonian shore, with further unequal elevation, a kind of wide trough or synclinal fold or depression appears to have been formed between the middle and eastern part of America, which was at first occupied by a wide arm of the sea, later, by continued elevation, by a great body of fresh water, and later by low marshes and low marshy islands barely above sea-level. Upon these low-lying lands grew a dense vey: tation, unlike any of the present day, but resembling somewhat the tree-ferns of our southern semi-tropical States. This low-lying region was subject to freshets and inundations from the surrounding higher regions, periodically deluging the swamps and swamp vegetation with river and flood deposits of pebbles and sand, under pressure of which the peat gradually turned into coal. Successive coal seams were formed by successive growths of vegetation between the intervals of periodic inundation or of subsidence, and possibly at times of upheavals, for these low lands, 'as sediments accumulated, appear at times to have sunk below the sea and again to have been either built up above it by fresh supplies of sediment, or to have been temporarily raised up by upheaving forces.

Finally, by a grand revolution which closed the Carboniferous age in America, the coal-swamps with their coal-beds and strata were crumpled up to form the present great Appalachian Chain.

Similar movements no doubt took place about the same time in the Rocky Mountain and Western region. But here the marine condition seems to have predominated over the fresh water one, for we find the Carboniferous in Colorado more represented by marine fossiliferous limestones and sandstones than by those of fresh-water origin, though the Weber-grits may have had a fresh-water origin, as in a few rare instances we find fossil plants like those in Pennsylvania together with a few insignificant small seams of coal, But in the West it is evident that the circumstances from one cause or another were not favorable for the production

and growth of extensive coal-beds as in the Eastern States. The coal-forming time was reserved in the West for a much later period, viz.: the Laramie or Upper Cretaceous. The Lower Carboniferous in Colorado, however, contains in its limestones much of our silver-lead wealth, as at Leadville and Aspen.

The Cambrian, Silurian, Devonian, and Carboniferous Ages have been grouped together by geologists into one great era, the Paleozoic, owing to a general family likeness in the fossil fauna and flora of these ages.

To the Archean and Paleozoic rocks the bulk of our veins and deposits of gold and silver are mainly confined, though both in Colorado and elsewhere, as will appear later, if certain peculiar conditions are present, the rocks of the later and newer periods may also in some regions produce precious ores. But the prospector should give his closest attention to these o/der rocks; hence we have devoted extra space to their description and history.

Triassic And Jurassic, Or Jura-Trias.

After the Carboniferous, followed the Triassic and Jurassic; sometimes in America, owing to the difficulty of positively separating the two periods, they are combined

under one name, the Jura-Trias, and in Colorado are locally called the " Red-Beds," owing to their prevailing red and variegated colors. The series is well represented in the celebrated Garden of the Gods, near Colorado Springs. The red conglomerate sandstone of the Trias proper has so far yielded no determinative fossils, but the variegated clays in the upper Jurassic at Morrison and elsewhere have yielded some remarkable Saurian remains of land lizards. It is probable from the presence of salt and gypsum in these red-beds, and the prevailing redness of the rocks, due to iron which was not leached out through the agency of organic life, and the general absence of fossil remains, that the lower portion of these rocks was laid down in landlocked salt seas, or salt lakes, shunned by both vegetable and animal life. The upper portions, however, show evidence of the existence of land of a low marshy character, with fresh water and probably large estuaries, as we find the remains of turtles, crocodiles, fresh-water shells, and

Dinosaurs or land lizards. The rocks of these periods are not generally prolific in ores. The Silver Reef sandstone of Utah is an exception, which contains chloride of silver disseminated through it. When pierced by eruptive rocks,

however, ore should be looked for in this series as elsewhere.

CRETACEOUS PERIOD. . Upon this followed the Cretaceous, a series of very thick

formations, numbering several thousands of feet in Colorado, consisting in its middle portion of limestones, and

PLaTE VI.

North America in the Cretaceous.

thick beds of drab shale. These are mostly marine, as shown by the sea-shells in them, but at the base is what is called the Dakotah group, or Cretaceous No. 1, a prominent sandstone hog-back in which the fossil impressions of leaves very like, but not identical with, those of the present day show that land and fresh water existed at the time. The limestones and clays of the middle or Colorado group, contain quantities of fossil marine shells, such as the Nautilus, Ammonite, Baculite, and Inoceramus.

The Laramie forms the uper group of the Cretaceous,

and contains our principal western coal-fields and abouiids in fossil remains of tropical foliage.

This Laramie group marks an important era in our Rocky Mountain region, for it shows that beginning of, the great Rocky Mountain revolution, by which the granite islands before mentioned, against which all the previous sediments had been forming, mainly beneath the sea, were elevated 10,000 feet or more into continental or mountainous masses, dragging up with them portions of the sea bottom and exposing it as land surface, draining off the shallow Cretaceous sea which had hitherto divided the Eastern half of the American continent from the Western, bringing on a land and continental condition, which was completed in the following Tertiary age and has continued to the present. See Plate VI.

The Jurassic, Triassic, and Cretaceous are grouped into one main division called the Mesozoic or middle-life era of the world's history. None of the rocks of this age in Colorado are celebrated for ore deposits, except locally under local conditions.

In California and portions of the extreme West where these rocks have been highly metamorphosed by heat and penetrated by igneous rocks, some of the leading ore deposits of gold and silver are found. The same remark applies also to the succeeding Tertiary in those regions, particularly in the Sierra Nevada and Coast ranges.

Tertiary,

The Tertiary age seems in the Rocky Mountains to mark an era of comparative rest in mountain elevation, for the strata forming some of the divisions of this age lie almost horizontally upon the tops of the earlier upturned periods.

These beds were formed by fresh-water lakes in Colorado surrounded by tropical vegetation. In the Coast ranges of California the Tertiary is upturned into mountain forms and metamorphosed, and, from the presence of sea-shells, is clearly of marine origin. The Tertiary in Colorado is best seen in outlying table-lands. In Wyoming the Tertiary lake formed the Green River beds and Bad Lands abounding in fossil mammals, leaves, fishes, and insects. The Tertiary was the world's tropical summer, a period of

beautiful lakes of semi-tropical foliage and a warm climate. In certain regions it was disturbed by gigantic revolutions which upheaved the Himalayas and the Alps. Such revolutions as occurred in our Western Cordillera system were marked by enormous ebullitions of lavas of various kinds issuing from fissures deluging Idaho, Nevada, part of Oregon, and Washington. Remnants of this same disturbance are seen in the form of basaltic overflows capping Tertiary strata in Colorado and New Mexico; and the vast volcanic region of San Juan in Southern Colorado is covered with successive lava overflows of the satue period.

The Tertiary rocks in Colorado are not generally good prospecting ground. The lavas, however, are (with the exception of the basalt, which for some reason is generally sterile) locally productive, as for instance the entire San Juan Region, also Cripple Creek Mining Camps and Silver Cliff. So the prospector, whilst he need not waste time among the sedimentary beds, will do well to examine any eruptive rocks of this period for gold especially, and also for silver. The varieties of lava are principally andesite, rhyolite, trachyte and basalt. In the Coast range of California, where the Tertiary beds have been metamorphosed by heat into slates, gold and cinnabar are found.

Glacial Epoch And Quaternary Age, -

The Tertiary Summer was closed by the world's Great Winter. The ice from the north pole, for some reason we will not discuss, extended its domain far south to latitude 40.- All the northern temperate regions of the world were ice-sheeted and the sheet extended itself as by long fingers down the, by that time, highly developed mountains, filling the ravines with glaciers. By the downward destructive grinding motion of the glaciers, the ravines, commenced by water, were deepened and widened by ice. Fissure-veins were thus exposed, both of gold and silver. The debris from their progress the glaciers carried on their backs and dumped at the outlet of the canyons; and when the temperature finally became warmer and the glaciers melted, all the long lines of traveling boulders scattered upon their backs, many of them containing gold robbed from the veins, were left as banks or " moraines," forming our " gold

placer" grounds along the sides of our streams and canyons, or sometimes a thousand feet above the present river-bed, marking the original height or thickness the great ice bodies once attained.

So were our canyons largely formed, and so did our goldplacers originate. After the Glacial Epoch, a warmer period set in, called the Quaternary. The ice melted. Vast bodies of fresh water were distributed in wide streams and monstrous lakes over large portions of this hemisphere. The rough " morainal" dumps of the glaciers were " sorted" or " modified" by water, rolled into pebbles and sand, and redistributed along the banks of streams or carried out into beds of lakes. In these pebbles and sand was much of the precious metal mined and rcebbed from the veins. The gold by its insolubility remains to this day in our placerbeds and " drift" or " wash" and is collected by. hydraulic mining. That the prospector for gold should closely study these Glacial and Quaternary deposits is evident.

So ends the history of our section. Still the agencies of nature are at work as of old. Continents are gradually rising or sinking. Mountains are being imperceptibly elevated. Water is still sculpturing them with canyons. Rivers are carrying down fragments robbed from the land and depositing them in the ocean to form strata for future continents.

The fires of the earth are not yet dead, for volcanoes still vomit lava. The earth, however, is still continuing to lose internal heat. Its crust is still contracting and wrinkling itself upward, for we find modern sea-beaches raised high on our seaboard cliffs. Shocks of earthquakes from time to time prove that motion of some kind is going on beneath us, and doubtless our mountains are still rising imperceptibly, as they appear to have done in ages past, giving additional lifts and elevation to old uplifted strata, and slowly elevating newer strata that since the Tertiary have lain apparently undisturbed. We say apparently, for not only are the Tertiary beds uplifted from five to ten degrees, but even the more recent Quaternary deposits, showing that movement has been going on comparatively recently and may still be progressing imperceptibly.

Chapter Iii.

The Prospector'S Paleontology Or Study Of Fossils.

A prospector in his roaming among the rocks is likely from time to time to come across a good many fossils or petrified remains of life that once existed on this planet. He will feel curious to know what these are, what class of animal or vegetable they may represent, to what geological era, epoch, or subdivision they may belong.

Fossils to a geologist are the labels of the rocks; show a geologist a fossil, and he will probably be able to tell ata glance whether the fossil came from a series of Paleozoic, Mesozoic, or Cenozoic rocks; whether it belonged to a very ancient geological period down near the primitive granite, or to a comparatively recent one near the modern soil, high up in the geological scale and nearer to the life of the present day. He may be able to tell not merely whether

it belongs to one of the great divisions, to the great eras, but also to the subdivisions of these eras, whether to the Silurian or Carboniferous, the Jurassic, or the Cretaceous, or even to minor divisions of these, called groups; whether, for example, it belongs to the Dakotah group of the Cretaceous, or to the Laramie group of the same period.

Practical Use Of Fossils.

The practical use of a general knowledge of fossils is obvious. A prospector finds iff certain strata a fern-leaf of the Carboniferous; this tells him he must be on the coal strata and forthwith he hunts for coal. Or he finds a Paleozoic shell or coral, which points to the fact that he is probably in the neighborhood of the precious ore-bearing rocks.

Later perhaps he finds a shell or coral characteristic of the lower Carboniferous blue limestone, the celebrated lead-silver bearing formation of Colorado and the West, and he is encouraged to look for these ores. The limestone by itself is but a poor guide, for there are many limestones

not unlike it in the different series of rocks, but this particular shell labels this as "¢he blue limestone" and no other. Hence a characteristic fossil may help considerably in following up in its extension an ore-bearing rock, and not only that locally, but in regions very far apart. Soon after-the celebrated ore deposits of Aspen were discovered, and the mines were in their infancy, some fossils were discovered that showed the deposits to be in the same limestone as that at Leadville, which had proved there so productive. This gave an additional impetus to the camp, "a second Leadville," so it was said.

Again, though a prospector may not find at once the particular geologicai stratum or period he is looking for, if he finds a characteristic fossil anywhere, in some other period, he knows from it whether the period he is after lies geologically below or above where he is looking.

Thus, if a prospector finds a Silurian shell he knows that the Carboniferous "blue limestone" must be close above this Silurian, or if he finds a Marine Cretaceous shell, he knows that the Laramie coal-bearing group lies above. On finding a Cretaceous or Jurassic fossil, he knows that the Carboniferous and Paleozoic series must lie considerably below him.

In the accompanying geological table, Plate VII., we have shown what rocks and what minerals and metals are likely to be found in the geological divisions and subdivisions; also, generally, what classes of fossil life are to be expected in each.

Then in the diagrams of fossils, we have selected pictures of the fossils most commonly to be found in all the great divisions, so that if the prospector finds a fossil, he may, by comparing it with the picturés, find what its name is, and to what great geological division or subdivision it belongs; it is not so necessary for him to remember the scientific " jaw-breaking" names of these fossils, as it is for him to be able, at sight, to recognize whether it belongs to one or other of the great eras, or, better still, to one of the minor subdivisions of these; whether it is Paleozoic or Mesozoic, whether Silurian or Cretaceous, whether it belongs to the Colorado marine Cretaceous or to the Laramie fresh-water Cretaceous, etc. If the fossil is a very peculiar one and cannot be identified as belonging to any of the common

CHA CTERISTIC Rocks. MINERALS, hte a FOSSILS.

Pebbles Sand Clay Placer Gold We

Hipoife fave oe " Fossil Leaves

conglomerates fila wearin Mammals ss Gays Eh Lh P aéthus omens of 1 Coldrado Granitic detritus 27 California Coal LGaves, Wes 8c. Sa Shells . Drab Shales, Clays Canon City Oi Horizon eamnites Bax Bacylites fi i pa ligceramis

lash oe frais

Na Di anata is 5 MOSAUFS CO Bi ae ca aeMit bey Pitan see f ra a iit ri Stone VOUS Of Salita wel Mite a n

fastern Coal Land Plants

Shales, Sanastones % msy/vamia Grits & Shales

Tertiar "i Miocene Pulocens

In California Marine Shes/ls

focene

rom

Drab ale Ligestone Jilver, Lead Hee Sel /ron Tolobres Corals

Gold. Silver We Lead, Zine, Copper pemive /ron

PuaTE VII.

Prospector's Geological Table of Western Formations, Showing Principal Characteristic Rocks, Minerals and Fossils to be Found in Them.

ones we have pictured, he had better send it to the office of the U. S. Geological Survey at Washington, or to some good paleontologist. We frequently have fossils sent to us to know whether this or that fossil is a likely indication of the presence of coal or other mineral, and sometimes our identification is a material help to the prospector; but with the above table the prospector could save himself the trouble and postage-stamps. ' ARCHAAN,

Starting, then, from 'the Archean 2s a sure and safe horizon

, the prospector will find no fossils, and only some in-

PuiaTE VIII.—CaAmBrRIAN FOssILs, 1, 2) 3, Trilobites ; 4, Track of Crustacea; 5, ''rack of Worm; 6, 7, Sea Shells.

direct probable evidences of past life, such as graphite, which may possibly represent ancient coal derived from some form of vegetation unknown to us. Limestone and marble are also indirect evidences of past organic life, most modern limestones being due to the remains of corals, etc. Whatever life may have existed in those primitive granitic rocks has been pretty well obliterated by excessive metamorphism and crystallization of the strata.

Cambrian,

Resting on the granite he finds the " Primordial" or "Cambrian" series, sometimes called the Potsdam Sandstone.

If this series consists of unaltered sandstones, he may be fortunate enough to find some of the shells and other traces of life of those old beaches as shown in the

diagram, but, generally speaking, in Colorado and the West

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PLaTE [X.—Sr.urian FoOssits, 1, 2, Orthis ; 3, 4, Spirifer; 5, Pleurotomaria ; 6, Murchisonia ; 7a, 74, Trilobite (Calymene); 8, Coral Fenestella ; 9, Coral Choetites ; 10, Graptolite; 11, Orthoceratite.

the Cambrian is so highly metamorphosed and altered into hard crystalline quartzites, that evidences of past fossil life are as scarce and indistinct as in the Archean, and probably for the same reason. The forms he may find are a little crustacea called a Trilobite, something like a "sand crab," also a few little shells and some marks of worms, Plate VIII.

Silurian.

In the next series, the Silurian, he may be more fortunate. He may find remains of sea-weeds, corals and shells, and fragments of a sort of sea-worm called a Crinoid, or sea-lily. The little discs with a hole in the centre forming a little ring about the size of a pea, constituting the discs or rings of which the stems of the sea-lily are com-

Tr Ars

Plate X.—Devonian Fossils.

1, Spirifer ; 2, Comecncd iit pa Gris b roniatites 3 5) 6, 7, Corals; 8, 9, posed, are sometimes very common in Silurian and Paleozoic rocks, though it is rare to find a complete Crinoid, and especially the beautiful comb-like flower or head of the sea-lily. He is likely to find also a more advanced type of the Trilobite and various Spirifers and other shells as pictured. Plate IX.

Devonian,

In the Devonian he may find the teeth or bones of fishes, and a few remains of peculiar land plants, neither of which are known in the Silurian below, also many corals.

Carboniferous,

In the Lower Carboniferous " blue limestone," corals and shells appear, especially Spirifers and Productus, together

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PLatre XI.—CARBONIFEROUS FOSSILS,

1a, 16, 1¢, Productus ; 2, 2, Spirifers; 3, 3, 3, Rhynconella; 4, Euomphalus; s, 5, Crinoids ; 6, Pleurotomaria ; 7, Bellerophon ; 8, Athyris Subtilita ; 9, Astartella ; 10, Goniatites ; 11, 12, Corals ; 13, 14, 15, 16, Plants ; 17, Spine of Echinus.

with Crinoids anc a very simple curled shell like a snake coiled up, a " Goniatite," one of the earliest of the Ammo-nite

class. At Aspen, associated with the ore-deposits we found in the blue limestone most of these, together with a

kind of snail-shell called Pleurotomaria. At Leadville in the same formation Spirifersand Productus are occasionally found. A very curious coral is one shaped like a screw, called Archimedes, after the author of the screw. Cupcorals are common.

In the Middle Carboniferous, associated with the coalseams, many curious remains of reeds, ferns, and other aquatic plants of that age are found, but these are scarce in Colorado and the West. The prospector will observe

PLATE XII.—JuRA-TRIAS FossILs,

1, Dinosaur Lizard; 2, 3, Footand Shoulder Bone}; 4, 4, Vertebra of Sea Saurian, Ichthyosaurus; 5, 6,6, Teeth of eet elemnite ; 8, Echinus ; 9,9, Ammonites; 10, Exogyra; 11, Trigonia Shell.

that there is a general family likeness between the fossils of each division of the Paleozoic and in the Paleozoic asa whole, and it may not always be easy for him to determine whether a shell is Silurian, Devonian, or Carboniferous, but of one thing he will be certain, that it is Paleozoic.

Triassic,

In the Trias throughout the West, he is not likely to find many fossils; the rocks are generally too coarse; but in the Eastern States, though he may not find any true remains, he may observe the tracks left by great Saurians as they walked on their hind feet, or on all fours, on the red sands of the beaches of those dreary salt Triassic seas, leaving " footprints on the sands of time" full of interest.

Jurassic.

In the Jurassic shales and limestones in Colorado, he may be equally unsuccessful, though in the upper Jurassic just below the Dakotah sandstone, he may light on the bones of gigantic Dinosaurs, or great land lizards, such as the author found in Colorado and Wyoming, monsters sixty to eighty feet in length and proportionally tall, standing from twenty to twenty-five feet in height. In the lower Jurassic in Wyoming, he will find great numbers of seashells and Ammonites, and a. round shell like a cigar called a" Belemnite," or spear-head, the internal shell of an ancient cuttle-fish. Plate XII.

Cretaceous,

In the Cretaceous, beginning with the lowest group, the Dakotah group, net-veined leaves of deciduous trees, such as the willow, oak, maple, etc., the earliest known leaves of those kinds of trees, may be expected in the sandstone and clays.

In the Colorado group of the Cretaceous, above the Dakotah, abundance of oyster-shells and large clam-shells (Inoceramus) are sure to be found in the limestones and marine shales. In the Montana group of the Cretaceous above this, consisting mainly of drab shales and some sandstones, great quantities of sea-shells are found, among them various peculiar forms of the Ammonite allied to the modern nautilus, and called Scaphites, resembling snakes or

worms uicoiling, together with shark's teeth and bones of sea Saurians.

In the sandstones of the Laramie Cretaceous, remains of sea-weeds are found; in the sandstones immediately below

Plate Xiii.—Cretaceous Fossils.

1,1, Inoceramus; 2, Cardium, 3,Corbula; 4, Mactra; 5, Margarita; 6, Fascio. laria; 7, Anchura; 8 Pyrifusus; 9, 10, Scaphites; 11, Crioceras ; 14, waculites ; 13, Shark's 'Tooth,

the coal-beds, and in those associated with or above the coal, are found great varieties of semi-tropical leaves, such as those of the palmetto, fig, beech, elm, magnolia, sassafras, etc. The presence of these leaves is a pretty sure indication of coal,

In the Tertiary fresh-water beds, similar leaves and thin beds of poor lignite coal are found, together with fossil insects and remains of'mammals. In the Marine Tertiary are sea-shells.

Tertiary.

PLate XIV.--TERTIARY FOssILs.

1, Palinetto ; 2, Cinnamon Leaf ; 3. Cardium 3 4, Insect; 5, Nummulite Shell; 6, 7, Fresh- Water Shells.

Quaternary Fossils.

3, Mammoth Elephaut's Tooth ; a Mastodon's Tooth ; 10, Flint Implement ; 11, Stone xrooved by Glacier.

Quaternary.

In the Quaternary drift, among the pebbles, sands, and

"wask" characteristic of gold-placer beds, an occasional

tooth, tusk, or bone of the great hairy Mammoth elephant

or the Mastodon elephant may be discovered, together with . the stone implements or bones of prehistoric man and pebbles grooved by glaciers.

Chapter Iv.

Lithology Or Study Of

ROCKS. A prospector wants to know a great deal about rocks.

The Prospector'S

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They are his constant companions in the field. His busi-

§t

ness isamongst rocks. He wants to be able to recognize them at sight, when he picks up a loose pebble, or confronts a mighty cliff. When traveling over the mountains, as he surveys the grand panorama from the.top, he wants by the peculiar forms and patterns each variety of rock is apt to take as the result of erosion and weathering owing to different degrees of hardness, to be able to make a shrewd guess fron a long distance, as_ to whether one mountain is made of granite, or another of limestone, or 2 third of porphyry. This habit of forming rough guesses as to the character of distant rocks decides him as to choosing his course for prospecting. "In those sharp granitelooking peaks," he says, " maybe I will find fissure-veins. Yonder cones, like the spires and minarets of a Gothic cathedral, must be porphyry or igneous rock, another likely locality, and mark where they break through the sedimentary strata, and tip them up all around them; at the junction of these sedimentarics with the igneous rock there may be limestone, and a 'contact blanket deposit.' Yon smooth grassy slopes are probably underlaid by sandstone or limestone, and the rolling valley beneath by soft shales. The latter are unpromising for precious ores." Or again descending from his perch into the canyon below, he recog-

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nizes the granite basis, and on top of it a series of sedimentary rocks. The lowest of these, by its rusty-white, masonry-like

; w p. White Porphyry.

(AND SECTION.) uartzite ; c, Silurian Limestone ; @, Lower Carboniferous

AMPHITHEATRE. Pineoin Porphyr

Limestone ; /4,

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a, Archzan Granite; 6, Cambrian

structure, he judges to be Cambrian quartzite, the thin-bedded strata above Silurian limestones, and the heavy massive beds above these, Lower Carboniferous blue limestone, whilst

a dark greenish-gray rock, running in and out irregularly among the strata, sometimes between the stratification planes, at others cutting across them, he judges tu be an intrusive sheet of porphyry, and looks again for " contact deposits." A rock running up like a low wall from the bottom of the canyon to the top may be either quartz fissure-vein or a porphyry dyke, and well worth examining. There are many ways of studying rocks, one by hand specimens, finding out all the minerals composing them, and then naming the rocks from which they came; another by observing the appearance of large masses of rocks in the field, and noting their mode of occurrence; and lastly, if we wish to be very accurate, making thin microscopic sections and a chemical analysis, but for the average prospector these last will be rarely necessary.

If aprospector bought a manual to study rocks, for practical purposes, he would find himself amongst asea of names of varieties of rocks, nine-tenths of which it is safe to say he would never meet with in his field experience.

Tosave him the trouble of wading through such books, we select just about as much as a prospector is liable to meet with in the field or find practically useful, saying little also about such cominon rocks as are familiar to every one.

Those that need most definition and are of most importance in the mining-field, are the crystalline rocks belonging to the class called metamorphic and igneous; the last especially needs careful determination.

Nearly all sedimentary rocks (limestone excepted) are derived from fragments of igneous and metamorphic rocks. Probably nine-tenths of the sedimentary rocks are derived from granite alone, the remainder from the igneous rocks, such as porphyry, basalt, etc. By describing the parent - rock, the derivative one is more easily made out.

Rock-Making Minerals,

Crystalline rocks are made up of certain distinct minerals, most of them of quartz, feldspar, and mica, with sometimes also hornklende and augite. Other minerals may locally occur as occasional elements.

QUARYZ scarcely needs description, being so well known.

The hexagonal prism of this crystal is too hard to be scratched with a knife and will scratch glass. This distinguishes it from calcspar and barite, for which it might be to age in the field; moreover it will not effervesce with acids.

THE FELDSPARS are nearly as hard as quartz. Their colors are white, grayish, and flesh-color. They are rarely as transparent as quartz, being generally opaque. Their form of crystallization is different from quartz, and in a vein they show one smooth face of their crystal, whilst the quartz is more like crushed loaf-sugar. Ina porphyry the feldspar crystals are very distinct, and give a characteristic spotted pe pene to the rock. Two varieties of feldspar are characteristic of the crystalline rocks, one called orthoclase or common feldspar, a potash-feldspar, the other called oligoclase, a soda-lime-feldspar. The former is very characteristic of granitic rocks as well as of igneous porphyries; the latter is rather more characteristic of more recently erupted igneous rocks, such as diorite, basalt, andesite, etc.

Orthoclase is generally in large crvstals, oligoclase in small. When the crystals are very small, it may take a microscopic examination to determine to which variety of feldspars they may belong. The oligoclase and plagioclase Cl oheaieg in igneous rocks are commonly but little white

ots.

To determine accurately, microscopic slides and chemical tests must be made, but this is scarcely within the scope of the prospector who wants to guess roughly at sight as to the name and character of a rock.

Mica, 'both black and white, needs no description.

HORNBLENDE differs from mica in being of a duller lustre ' and of a different form of crystallization, as shown in the plate. The color is a greenish-black; the greenish tint is distinct when the crystal is struck by a hammer.

AUGITE or PyROXENE is scarcely distinguishable from hornblende. In Colorado, augite is mainly confined to two kinds of rock, basalt or dolerite and andesite, both of comparatively recent volcanic origin. Hornblende and mica are common to nearly all the metamorphic and igneous rocks.

TALC amongst miners means almost any soft, sticky, or

slippery, decomposed rock, but strictly, talc is a pale green soft mineral like mica and is a silicate of magnesia. Steatite or soapstone is massive talc. Miners often wrongly call any soft clay or rock, soapstone also. -

CHLORITE is another magnesian mineral, of a green and soft character. Chlorite is again a name given to almost any greenish rock of a schistose and soft decomposed character.

CALCITE is carbonate of lime crystal, the element of limepha and is distinguished by softness and effervescing in acids.

DOLOMITE or carbonate of lime and magnesia is very like calcite and is the element of dolomitic or magnesian limestone. Dolomite effervesces with much greater difficulty than true limestone. To effervesce, the dolomite should be powdered and the acid heated.

Gypsum or sulphate of lime can be distinguished by its extreme softness, being scratched by the finger-nail; it does not effervesce like lime.

BARITE or " heavy spar" occurs in some veins, but not as a constituent of rocks. It looks like calcspar, but is heavier and will not effervesce with acids.

FLUOR-SPAR occasionally occurs in veins, in cubes or massive. It is easily scratched with a knife; its colors are green, purple, yellow, blue or white.

GARNETS, GREEN EPIDOTE, BLACK TOURMALINE, and other minerals or gems may occur, but not as important constituents of the rocks.

Crystalline Metamorphic Rocks.

GRANITE.—Beginning with the granitic series of the Archean age, granite proper is massive, shapeless, or amorphous, and shows no bedding-planes or other signs of former stratification. It is thoroughly crystalline, like lumpsugar. By some it is considered a true igneous rock, one that has been thoroughly fused by heat, as much as the lavas or molten iron; by others its crystalline amorphous condition is supposed to be the result of extreme metamorphism of originally sedimentary bedded rocks, such as gneiss or schist, the two latter being sometimes traced down through a gradual change into granite. The compo-

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sition of granite is mica, quartz, and feldspar with sometimes a little hornblende. The micas may be white mica (muscovite) or black mica (biotite). Both orthoclase and oligoclase feldspar may be present, but more commonly the former, which is often a pinkish flesh color. Granite, in its crystalline texture, differs both in character and appearance from porphyries and other igneous rocks, in the fact that its crystals are all jumbled up and crushed together like loaf-sugar, and none of the crystals are set like plums ina pudding, distinctly in a backing or paste of very small crystals of amorphous or glassy material, as in the porphyries or igneous rocks. Granite is probably the oldest and deepest rock known. It is often traversed by sparry veins, both great and small, which consist of quartz or feldspar or

Weak

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Wu

Pirate XVIII. both, in a more sparry condity sTriclinic Oligoclase Feldspar. tion than when diffused through 2, Monoclinic Orthoclase Feldspar, 3,Carlsbad Twins Feldspar, the parent rock, 'ti 4, Augite or Pyroxene. 5 and [These so-called quartz- 6, Hornblende. veins" are often called " granulite

" or " pegmatite" or " graphic granite." The quartz and feldspar are often arranged in parallel plates, giving on cross-section curious marks like Hebrew characters; hence the word graphic. The bulk of our so-called quartz fissure veins in the granite mountains may be called pegmatitic veins. The colors of granite vary from reddish to gray, or nearly white to black, according to the preponderance and colors of the micas and feldspars in them.

SYENITE is little more than granite in which hornblende supplies the place of mica,

GNEISS may be called "bedded yvranite,' showing a

bedded appearance. Gneiss is often curiously and prettily banded c- streaked by seams of mica dovetailing into each other. If mica preponderates, it is called " micagneiss," if hornblende " hornblendic gneiss."

SCHIST may be called laminated gneiss or granite, being

finally divided into lamina or leaves. This foliated struc-

"v KAA

4 'a ar Yvick é@ GRANITE Peomaritre PLatre XIX, PLATE XX, Puate XXI,.

ture is due to the arrangement of the flat-lying crystals of mica or hornblende largely composing it. It may be a mica-schist or a hornblende-schist.

SLATE is shale altered by heat into a hard crystalline structure.

QUARTZITE was originally a sandstone composed of quartz-grains, which by heat have been partially fused to-

Gneiss

Plate Xxii. Plate Xxiii. Plate Xniv.

gether at the edges, resembling granules of tapioca in a tapioca pudding. Quartzite differs from quartz in being a rock made out of pieces of quartz, and not the original mineral itself. Quartzite may be white like sugar, gray, brown, or rusty. It shows a true stratified structure.

MARBLE is limestone similarly changed to a more crystalline condition.

SERPENTINE is a green magnesian rock, sometimes found with marble and igneous rocks, and is formed by alteration of certain minerals in the latter.

Crystalline Igneous Or Eruptive Rocks,

These are rocks which are supposed to have been thoroughly fused or melted in the bowels of the earth. Some reach the surface by fissures or volcanic vents, others have never attained to the surface or overflown it, but have intruded themselves between the weak places in the underlying strata, or have collected and cooled deep down below the surface in great molten reservoirs called " laccolites" or lakes of stone. When these have been subsequently uncovered by erosion, they may present the forms of considerable mountain masses like the Elk Mountains, and Henry Mountains and Spanish Peaks. Geologists distinguish those rocks which have poured out on the surface from craters and volcanic vents as volcanic rocks, while those cooling below are called Plutonic.

Intrusive Plutonic Rocks,

The component minerals of these intrusive Plutonic rocks, such as are commonly called porphyries, are principally quartz and feldspar, with mica or hornblende. In color these rocks are some shade of gray, green, or maroon, or even white, but their most striking characteristic is a general spotted appearance. This arises from more or less large, distinct, perfectly formed crystals of feldspar or quartz, set in a finer-grained crystalline paste or background, standing out distinctly from it. This base or background may be comparatively coarsely crystalline, finely crystalline, or so finely crystalline that the crystals can be discovered only by a microscope, while the larger crystals seem set in the paste, like plums in a pudding. In the depths of a mine the porphyry is commonly much decomosed

by water action or mineral solutions, and even passes into a clay or gouge. The characteristic spotty appearance, from the presence of individual crystals of feldspar, may even then identify the rock, or by chemical analysis the very aluminous character of the decomposed rock may

determine its character. When feldspar is the main constituent, it is called a felsite porphyry, when a certain amount of quartz is present a quartz porphyry.

DioriTE, whose crystals are sometimes porphyritic in character, hence called porphyritic diorite or porphyrite, belongs also to this intrusive or Plutonian class, differing only from the others in the fact that its feldspar is of the triclinic plagioclase kind rather than orthoclase. Hornblende is a prominent constituent of this rock, and gives it, more or less, its dark olive-green tint. In appearance it resembles a dark syenite, but its occurrence as an eruptive, intrusive rock distinguishes it, as syenite is generally a metamorphic rock. The peaks of the Elk Mountains are, many of them, of diorite. Diorite or porphyrite is the so-called porphyry of Aspen, above the ore deposits.

Quartz Porphyries,

These are the commonest, and may be said to be the prevailing eruptive rocks associated with our ore deposits in Colorado, as forinstance at Leadville, felsite porphyries as well as quartz porphyries occur in the granite rocks in the Central and Georgetown mining hie districts. All these rocks are common A... abe through the West, and quartz porphyries POMTMBINTE are the most common eruptive rocks the PLare XXV, Prospector is likely to meet with in his search for ore deposits. We will describe in detail one or two typical species, though it must be observed that these porphyries are of endless varieties and shades of appearance.

4 QUARTZ PORPHYRY.—A quartz porphyry A is a porphyry that contains quartz crystals q large or small, in addition usually to large erthoclase feldspar crystals, generally of a vitreous glassy variety called " sanidin," together with small crystals of hornblende or mica. As a typical example we take that which forms the dyke composing the peak of Mt. Lincoln, Colorado, called Mt. Pare XXVI.

Lincoln quartz porphyry. This porphyry

ese oceeeanemaenemnsemreraerenseneraiitesssasrateranscecusenrsegveennnievacesenewevrsrsceseremoe seit tee Hi nt

and varieties of it are common in the western mining sections of Colorado.

In appearance it is a gray rock spotted with large and small crystals of orthoclase sanidin feldspar, which sometimes show an oblong face two inches long, by an inch wide; at other times a shape like the gable-end of a house, according to whichever part of the crystal happens to be exposed. Romasinns two orymale M*Linoown Quanre are seen locked together, forming what are called Carlsbad sine, When the rock is PLaTE XXVII. decomposed, these crystals not unfrequently drop out and lie as pebbles on the ground, With these may be also seen rounded ends of bluish crystals like broken glass. These are portions of perfect quartz crystals, which when extracted show a six-sided pyramid at either end. These larger crystals are set in a crystalline ground mass of much smaller crystals of the same kind, together with many little black cubes of shining mica, or duller lustred, longer, ay oblong crys-eet

ag tals of hornblende. This porphyry is Prave XXVIII. eruptive and intrusive, canntaa in dykes, intrusive sheets and laccolites.

LEADVILLE WHITE PORPHYRY.—At Leadville there is a quartz porphyry known as the Leadville white porphyry or "block porphyry" by the miners, which needs description, as it is the one that more especially is associated with the rich ore deposits,

It is a white, compact, homogeneous

looking rock, not unlike a shaly white

sandstone or quartzite. It consists of

feldspar, quartz and a little mica. Its

porphyritic or spotted character is so F

indistinct that one would be inclined — y,q2naenoeAusire dion to call it a felsite at sight rather than Pare XX1X

a true porphyry, but the microscope : ' reveals perfect double pyramids of quartz and individual crystals of feldspar set in a paste of the same minerals. It is often stained by concentric rings of iron oxide

Leaoville Wht E Quartz Orphvay

and marked with wonderful imitations of trees. The latter have earned for it the title of " photographic rock" or "dendritic porphyry." These markings are only the crystallization forms of oxide of iron or manganese, something like fern-frost on a window-pane. The porphyry is very shaly, and breaks up in thin slabs; hence called also " block iad i bk It is common at Leadville and is also found elsewhere. In the same region there

are many other varieties of quartz porphyry such as the "gray porphyry," the Sacramento, and the pyritiferous porphyry. The latter is often gold bearing.

Younger Effusive Volcanic Rocks,

These intrusive plutonic porphyries and diorites are generally older than the other class, which reached the surface and poured over it and which may be called for distinction " effusive" volcanic rocks.

bad ivy: of these we may cite the dark basalts and dolerites that often cap the table lands of the prairie region and overlie our coal beds. pinkish or dove-colored rhyolite also caps some of the mesas and in certain districts an andesite lava.

DOLERITE AND BASALT.—The la' 'er being scarcely more than a fine-grained variety of the former, are very dark rocks, consisting of dark, heavy minerals, such as augite, magnetite, and a plagioclase feldspar called labradorite.

Such minerals are said to be basic, and the rock composing them also basic. t

ANDESITE is very like dolerite, though (ygetiabscom generally a lighter gray or pink. Both fwvourelava augite and hornblende may occur in it, es more especially hornblende, sometimes mica PLATE XXX. also. The feldspar is called andesite feldspar from the Andes Mountains.

RHYOLITE, under the microscope, shows a peculiar flowing structure, hence its name from "rheo' to flow. The lighter rocks in Colorado and the West are generally rhyolites rather than true trachytes. Their colors are pale gray, white, pink, or sometimes dark.

Rhyolite consists of a fluent, vitreous, ground mass or

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paste, usually containing crystals of sanidin feldspar, or even of quartz. When these crystals are conspicuous so as to give the rock a porphyritic appearance it is called " liparite."

In some cases it may have even a granite-like ap-earance, the crystals of quartz, mica and feldspar being more or less intermixed; then it is called Nevadite. It is an acidic rock consisting of acid minerals mainly.

TRACHYTE, from trachus" rough, is alight colored rock, with a peculiar characteristic rough feel, due to microscopic vesicularity. It consists of a ground mass ¢ ° sanidin feldspar and augite, containing crystals of the 'acter. In ninety-nine cases out of a hundred, in Colorado at leas, also in the West, rocks which are popularly called " trachytes" are rhyolites or porphyries.

Amveoacoinat Scoria

Plate Xxxi. Plate Xxxii.

BASALTS and some of the other extrusive volcanic rocks assume a columnar form on cooling. Also, on the surface of the flow, the lava becomes minutely honey-combed like sponge, from escape of steam. This is called scoria, and when these holes are filled with almond-shaped white crystals, amygdaloid. At other times the rock is a volcanic breccia; that is, angular blocks of lava, great or small, are cemented together by lava. This probably was caused when the lava was pouring out of the fissure slowly, some portions congealed and were broken up by the onward flow, and again involved in the molten mass without being remelted. Enormous masses of volcanic breccia cover the San Juan region. Sometimes, by steam, the iava is blown into dust and descending with water, is worked up into a volcanic sandstone known as volcanic " tufa" or ' tuff."

OBSIDIAN is vitrified lava or volcanic glass.

epoeaenRmadadans BOON

Chapter V. The Prospector'S Mineralogy.

There are two classes of minerals in which the prospector is interested, one may be called the " earthy" minerals, such as quartz, calcspar, etc., associated with the precious ores; the other, the metallic minerals, constituting the ores themselves.

Both of these he wants to know at sight, or to determine with the simplest appliances. Generally speaking, his eyesight, his pocket-knife, his ore-glass and a little acid will be all he needs, nor need he concern himself about a great number of minerals, if he only knows the commoner ones well. The earthy minerals form the gangue or veinstone of the vein in which the precious ores are distributed.

Earthy Gangue Minerals,

These are principally quartz, calcite, or limespar, dolomite, fluorspar and baryta, all of which we have already described among rock-forming minerals. These crystals are nearly always to be found in the adjacent rock as elements of that rock, and their more sparry condition in the gangue of the vein is derived by solution from the enclosing country rock. Thus, a vein running through granite will contain mainly quartz, though calcite and fluorspar may be associated with it in small quantities. A vein passing through limestone naturally carries calcite or limespar. Sometimes baryta is associated with the calcite, especially if near the limestone ore deposit there are porphyries.

Baryta has been detected as an element of some porphyries which are probably ore-bearing, and when prospecting, we have found baryta to be generally an indication of ore near by, while calcspar, or quartz, alone, may or may not be barren. The float, or loose surface indications of ore deposits at Aspen is commonly made up of calcspar and baryta. FLUORSPAR in Colorado is generally confined to veins in

ene eeinentbinnte nates

the granitic rocks and in some of the eruptive rocks. Its presence is a good sign of ore.

OXIDES OF IRON AND MANGANESE.—These, often mixed together, form a large element in the gangue matter of a vein or ore deposit. Manganese can be recognized by its dark black color. beautiful rose-colored carbonate of manganese called RHODOCROSITE is occasionally met with, associated with quartz and metal in some veins.

CARBONATE OF COPPER is often associated with this gangue matter. It is readily distinguished by its bright green or azure blue color. "Float" is commonly rusty with iron oxide streaked with stains of copper

PLare XXXIIL. carbonate. Spathie Iron, SPATHIC IRON OR IRON CAR- BONATE OR SIDERITE occurs here and there in the gangue of fissure veins. It is very like brown feldspar, but heavier. 'These few common minerals cover nearly all that are generally met with as indications of, or in important connection with, ore deposits.

As a rule, most of these minerals occur in a massive state

rather than as individual crystals in a vein.

Metalliferous Minerals.

Through these gangues of various charaeteis, the precious metals are distributed in long, narrow patches or strings, or in large erysialline masses, or in seattered erystals, or in decomposed masses. The gangue matter is generally in the majority in a vein, amd the ore thinly, sparingly, and irregularly distributed im it. When a vein is said to be ten or more feet wide, it is not to be supposed that ten feet of solid ore is meant, but that this is the width of the gangue between walls. The ore bodw may be only a few inches wide. The streak or mam body of ore, called the " pay streak," has a tendeney to keep smear one wall or the other, or at times to cross from wall to wall.

7s Gee?

High And Low Grade Ores.

In gold veins, flakes or wires of "free" or " native" gold occur in the decomposed gangue, and sometimes in the pure, undecomposed quartz; "native" silver is found in much the same way, but more as specimens than as continuous bodies. Isolated patches of rare or valuable minerals, such as Ruby silver, Horn silver, Silver glance, etc., occur locally in parts of the vein, sometimes coating stalactites or crystals of a "vugh" or p. are XXXIV cavity lined with quartz or other crystals. Rabwait 1 An assay from such picked specimens bide tine id would give a very unfair average of a nine or prospect.

The bulk of the profits of a mine come from the commoner minerals, such as galena, pyrite, or lead-carbonate, and from the average grade of the mine. In California gold mines, the average yield of gold per ton is $16. In Dakota, $6. In the silver-lead mines of Leadville, $40 per ton is the average, and the ores are mostly low grade. A few knives of extraordinary high grade may yield from $75 to $100 per ton, but these are exceptional. Quantity of ore, facility for milling, cet of freight, the size of the vein, and its facility for working and nearness to market give the offset.

Decomposfd Minerals,

Sometimes the gangue matter contains a variety of decomposed ore in rich secondary combination intimately mixed through its mass and rarely discernible by the eye. Thus, yellow mudfrom a mine may assay high, from the presence of invisible chlorides or sulphurets of siiver. No accurate estimate of the value of a mine, or even of a piece of ore, can be found without an assay or mill-run. The reason for such richness in decomposed surface products is, that nature has been for ages leaching out, concentrating, and combining in richer forms the essence, so to speak, of the vein.

GRAY COPPER (TETRAHEDRITE).—Besides the ordinary galena and pyrites common in most mines, we sometimes

:

find considerable bodies of gray copper in mines, or intermingled

with other ores. This is generally a rich silver-bearing

ore, running from sixty ounces to some thousands

perton. It generally occurs massive, rarely showing its

pyramidal "tetrahedrite" crystals.

In appearance it is not unlike a

freshly broken piece of bronze. It

is more common in fissure veins in

granite and eruptive rocks than in

limestone. In Halls Valley, Colorado

, it is associated with baryta in a

vein in the gneiss. It occurs in

the Georgetown veins in granite.

In the San Juan district it occurs also

Pirate XXXV. associated with barytain the Bonanza

mine; and an ore not identical with

it incomposition, but very like it in

appearance, called bismuthinite, consisting of bismuth, antimony

, copper and silver, is characteristic of that region

and is rich in silver. Bismuthinite has a more shiny, tin-like

appearance than gray copper, and the red color which

bismuth gives to charcoal under the blowpipe readily distinguishes it from gray copper.

Local Variations In Value Of Ores.

There are locally in different mining districts considerable differences in the value of certain minerals and ores. In one district gray copper may rarely exceed sixty ounces of silver; in another it is invariably over one hundred ounces.

A coarse galena is generally poor in silver, while fine grained "steel galena" is generally rich in silver, but the reverse may also be the case. In some of the mines at Aspen, fine-grained galena, especially near the surface, is quite poor in silver, while in other mines in the same district it is exceedingly rich. Localities occur also where coarse-grained galena runs well in silver and is richer than fine-grained galena. This is the case at the Colonel Sellers mine at Leadville. So one mining district or even one mine is not a rule for another.

PyriTES.—Iron pyrites and copper pyrites, common in

most of our quartz veins in granite and in the eruptive rocks, may yield both gold and silver, but usually the former. There are certain districts more characterized by pyrites than others, such as the Central City district. These are generally gold-producing districts. Some of the mines at Breckenridge and South Park have strong pyritiferous veins in eruptive dykes, such as the Jumbo mine. These have of late produced a great deal of gold. The same district, however, produces large argentiferous leadveins. Pyrites generally favors the granite, eruptive and crystallized rocks. The quartzites of the Lower Silurian of South Park and Red Cliff are often pyritiferous and generally gold-bearing. In limestone the pyrites is rare or absent, its place being filled by some form of iron oxide. In the deeper mines of Leadville, however, this iron oxide is beginning to pass down into the iron sulphide or pyrite from which it was derived. Iron pyrites can generally be distinguished from copper pyrites by its paler, more brassy color, by its superior hardness, and by its crystallizing in cubes. Copper pyrites is much yellower and softer, and crystallizes in a more pyramidal form. A vein may glitter with showy pyrites and yet be quite valueless. It usually yields more gold in its decomposed, oxidized condition than in its unaltered state. In the one case the gold is free-milling, and in the other it must be smelted at much greater expense.

SULPHURETS.—This term among miners is loosely used, and often means some decomposed ore whose ingredients cannot be determined at sight, but which somehow assays high in silver. True sulphuret or sulphide of silver is a name embracing a large family of rich silver ores, among which are stephanite or brittle silver, argentite or silver-glance, sylvanite or graphic tellurium, and polybasite.

All these rich ores are compounds of sulphur and silver and other ingredients in varying proportions. They are somewhat alike in appearance and not always so easy to distinguish.

ARGENTITE, silver glance, or sulphuret of silver, is of a blackish, lead-gray color, easily cut with a knife, and consists of an aggregate of minute crvstals. Its composition in 100 parts is sulphur 12.9, silver "7.1. Under the blow-

Pipe it gives off an odor of sulphur and yields a globule of silver.

STEPHANITE, or "brittle" or " black" silver, is closely allied to argentite. Its composition is sulphur, antimony, and silver, silver being 68.5 per cent. The crystals are small. Under the blow-pipe it gives off garlic fumes of antimony and yields a dark globule from which, by adding soda, we get pure silver.

POLYBASITE, common at Georgetown and in some of the Aspen mines, such as the Regent or J. C. Johnson, on Smuggler

PLATE XXXVI. Hill, is like the others, but of a more flaky, Stephanite. scaly and graphitic appearance. It is not unlike very fine-grained galena,

yielding 150 to 4oo ounces of silver per ton.

These sulphurets sometimes line little cavities in limestones with a dark sooty substance, which under the microscope proves to be crystals of one of the sulphurets of silver. Sometimes also a rock is stained all through a blackish gray by these sulphurets. Iron or manganese may produce much the same effect, but an assay will soon reveal the difference. Associated with such a rock we may see flakes or wires of native silver,that have emerged from the sulphide state.

Chlorides,

CHLORIDE OF SILVER (" Horn silver," or Cerargyrite).— This is another result of secondary decomposition from a sulphide state (s'lver sulphide). It is a greenish or yellowish mineral, like wax, and easily cut with a knife. It is a very rich ore, running 75.3 per cent. silver, the remainder being chlorine. As a secondary product of decomposition it is generally found near the surface or in cavities, sometimes deposited on calcite or other crystals. In the mines at Leadville it is commonly associated with other decomposed ores, such as carbonates. In the Chrysolite mine, a mass weighing several hundred pounds was found. Chloride, bromide, and iodide of silver are closely related, being compounds of chlorine, bromine, iodine and silver. It is

ERA PRP IS eT

noticeable that these salts are the elements of sea water, and that these ores are often found in marine limestones. According to Mr. Emmons, the change at Leadville from sulphide to chloride was produced by surface waters; these waters are found to contain chlorine, which they probably derived from passing through the dolomitic limestones which contain chlorine in their crystals, and these limestones perhaps originally derived it from the sea water in which they were deposited. Chloride of silver is found at Aspen and abundantly in the outcrop of mines in New and Old Mexico.

Sulpharsenites.

Ruy SILVER (Pyrargyrite and Proustite).—Composed of sulphur 17.7, antimony 22.5, silver 59.8=100. Crystallizes in rhombohedrons, is seen in spots or crystals on a mass of ore of a deep red or blackish tint. When scratched with a knife it shows a bright or deep red color. In some mines this very rich ore occurs only as specimens, but in others it is present in sufficent quantity to largely influence the value of the ore in bulk. In parts of the Granite Mountain Mine in Montana, it constitutes the principal ore, associated, however, with other minerals. It there occurs in large masses and accounts for the extraordinary richness of that celebrated mine. Proustite is much the same, only lighter red, and consists of sulphur 19.4, arsenic 15,1, silver 65.5=100,

Carbonates.

This term also embraces a large family, the commonest being carbonate of lead (cerussite) and carbonate of copper (malachite and azurite).

CopPpER CARBONATE Can never be mistaken, owing to its brilliant green and azure blue color. Copper stains are among the common surface signs of a "lead." It is generally associated also with rusty stains. Both are the surface products from copper and iron pyrites forming a vein below ground which may or may not be profitable. Copper stains are common enough in many rocks, but do not always lead to bodies of ore. In South Park the red Triassic sandstones

7°

are so stained, but yield no ore. Along our foothills there is quite a stained belt from Golden to Morrison and through Bergen Park. But few promising deposits of copper or other ores have been found, although handsome specimens of native copper have been discovered near Golden.

At the Malachite Mine on Bear Creek, near Morrison, a prospect was at one time opened showing a good deal of silicate of copper (chrysocolla) and malachite, but for some reason it has not been worked since.

CopPER in its native or uncombined state is rare in Colorado, and so far we have &as yet no true profitable mine. A great deal of copper is found associated with other ores, and is extracted by some of the smelters. Carbonate of copper is commonest in the limestone districts, as might be expected from the carbonating influence of limestone upon minerals in it, or mineral solutions passing through it. Carbonate of iron (spathic iron, or siderite) constitutes part of the gangue matter in some of our veins, and may also be found associated with coal seams generally, in the latter case in an oxidized condition.

CERUSSITE (Carbonate of lead).—This is mostly found in the limestone districts, such as Leadville. Itis there known in two forms, one called "hard carbonates," the other "soft" or "sand carbonates." The crystals of this ore are small prisms, sometimes combined into a cross shape, of a pale grayish white, and might be taken for some form of carbonate of lime or gypsum; their weight, however, soon shows the difference. They are a secondary product of decomposition, consisting of carbon dioxide and lead oxide; as a carbonate they effervesce in nitric acid, and yield lead when heated. Cerussite is exceedingly rich in lead, carrying seventy-five per cent. The white lead of commerce has the same composition. In Leadville and elsewhere in Colorado it is silver-bearing also, and, though low in silver, the facility of its treatment at the smelter makes it a very desirable ore. Asa rule it contains less silver than the unaltered galena, but is more easily treated than the latter. The process of change or derivation from a sulphide state (1.c., from galena) to a carbonate, is well shown sometimes in a piece of Leadville ore. A central cube of galena is surrounded by a grayish green ring of sulphide of lead or anglesite, and outside this may again occur crystals of lead

7!

carbonate. Thus the process is from a sulphide to a sulphate, then to a carbonate. The so-called "hard carbonates" is a brown mass consisting of a hard flinty combination of iron oxide and silica, impregnated with crystals of lead carbonate, with which are often silver chlorides, also. The "sand carbonates" result from the decomposition and

Plate Xxxvii.

Simple and Compound Crystals of Carbonate of Lead (Cerussite),

breaking up of the hard carbonates, or from a mass of pure crystals of carbonate of lead, which are, by nature, loose and incoherent. The Leadville mines are getting below these products of decomposition and entering upon the original sulphides of galena and iron. The yield, however, is said to be equally good.

ZiNC-BLENDE '(SPHALERITE) " BLACK JACK").—Common in most mines mixed with other ores. As it is a very refractory mineral in smelting, much of it is not desirable ina mine. It is easily recognized by its brown resinous look, or when very black by its pearly lustre. At Georgetown, near the surface, brown " rosin-zincblende" carries silver, and is associated with rich ores, oe me polybasite and gray copper. ith depth the zincblende Rasornes more Sbunidant and PiLare XXXVIII. blacker, and loses much of its silver Zinc Sulphide (Zine

properties. Zinc-blende may run from

nothing to twenty dollars silver, and rarely as high as $100

er ton.

. In some mines in the San Juan it occurs abundantly near the surface and fades out with depth. We have no true zinc mines in Colorado, the zinc being mixed with other ores. In some mines in Pitkin County the zinc predomi-

:

napenesAdenibaaaauibiaaiin dnaichs dani tomas cents ree ee

nates over all other ores, and though it runs high in silver the smelters do not care to take it, on account of its refractory character. In the Eastern States where zinc smelting is a specialty, such ore might be separated and both silver and zinc saved. In Missouri zinc and lead are found together.

In Colorado there are no mines of one mineral alone, as in some other parts of the world. We have no true lead, zine or copper mines; these baser metals are either argentiferous or auriferous, and their baser qualities are sacrificed for their richer ones.

Chapter Vi. Ore Deposits.

Theories Regarding The Origin Of Ore-Deposits.

A prospector will find both a practical as well as scientific interest in considering the origin of ore deposits. Where do the precious metals come from? What is their origin? How are mineral veins formed and how do precious metals get into them?

The remote origin of metals is a matter of speculation. They may have formed part of that gaseous mist from which, according to the nebular theory, our planetary system was evolved. As this passed into molten condition the metallic vapors may have separated into various combinations, and consolidated and been arranged in the general make-up of the world according to their specific gravity. Some have thought that the interior of the earth may be more metalliferous than the surface crust, since the earth grows heavier toward the centre. Volcanic rocks coming up from depths unknown contain a large per cent. of the heavier metals, particularly iron. But we turn from these speculations to theories of more practical interest to the prospector.

A prevalent theory among miners and prospectors is what may be called " the igneous theory" or the fiery origin of veins and metals. They are apt to attribute the fissures themselves to some violent volcanic outburst, and consider

the quartz gangue or veinstone, together with the metals, as molten volcanic emanations, filling at one time a wide, gaping fissure.

Others demand an intense heat, considering that the metals in the veins were reduced in the bowels of the earth by intense heat to a vaporous condition, which, ascending through the fissures, condensed and consolidated in a crystalline form in the upper and cooler portions of the fissures, as certain sublimed mineral vapors from a smelting furnace sometimes collect and recrystallize in the flues.

By many prospectors every indication or surface appearance of a vein, or even a likely-looking rock, is called "a blow out," a term suggestive, at least, of some sort of volcanic explosion at that point. With them, the "fire and brimstone" origin of ore deposits is as deep seated as the veins in the rocks.

These ideas contain a measure of truth, and ° were naturally suggested by observing that our ore deposits are so generally associated with volcanic rocks and evidences of past heat; and it cannot be denied but that we presence of these volcanic rocks had a more or less to do with PLATE XXXIX.

the ore deposits. Fold Passing fifo Fault Showing. by be

aracter of Fau issure an acen

The modern study of Rocks Producing Later a Brecciated ore deposits inclines to Vein and ' Horses.'

the belief that we need

not draw directly upon the unknown profound supposed ignited regio.us of the earth's interior for the direct source of metals found in the veins, nor entirely from violent explosive volcanic agencies, nor from very intense heat, but rather that we may look nearer home for the immediate source of both metals and veinstone, namely, in the elements of the common country rock adjacent to the ore deposits; and for the medium of distribution and concentration

of ore and veinstone from nothing more violent or volcanic than water, more or less heated and alkaline. Nor is it so absolutely necessary to suppose that the filling of a vein fissure with quartz or metal must needs come uf from profound depths, and from a foreign source; but quite as ete from the adjacent sides of the fissure, or even from above the position later occupied by ore.

Veins of whatever kind are not vents for molten volcanic matter, but simply courses for water, more or less heated

PLATE XL. PLate XLI.

Tight ° m A acto be acteneee ae Gash Vein Fissures in Jointed Erup- Finally a Narrow Fissure Vein— tive Sheet, Small Dots Ore Solutions,

and alkaline, in fact, channels of mineral hot springs carrying earthy minerals and metals in the same solution, and depositing them, partly by cooling and sometimes by chemical precipitation and mainly by relief of pressure in such openings or weak places as may be found convenient.

The origin of these openings and weak places in the earth's crust is various. The class of great fissures holding "fissure veins," cleaving our mountains from top to bottom to an unknown great depth, were caused by the fracturing and faulting of rocks, in the gradual process of folding upward, and elevation of the mountain system, a process so slow and gradual that it may be even progressing now without one noticing it. The relief of extreme tension from folding results finally in faulting; though the fault fissure may extend to very great depths, it was probably not violent but gradual. From time to time, the

shock produced by the grinding together of the walls of a fissure, in a slip or jerk of only a few inches, may have given rise to severe earthquakes on the surface.

A great fault fissure, too, was likely to be accompanied by minor adjacent faults, and also by small incipient fissures or loose fractures of the rocks, producing parallel fissures and zones of fissure veins. Other openings, occu-

Lay 4 ag a: ee ro a jo WD, PLaTE XLII. PiatTE XLIII. Joints and Bedding Planes. Jointed Granite.

pied now by fissure veins, may be compared to those joints common to all rocks, the result of contraction and shrinkage of the granitic or volcanic rocks from a soft, semiplastic condition to one more solid and compact. But in no case, we think, were the fissures now occupied by veins 50 to 100 feet wide originally wide open chasms like that which swallowed up Korah, Dathan and Abiram in Bible history, but rather cracks fitting very tightly together by enormous lateral pressure, such as we see in fault cracks of the present day, not yet occupied by vein-

PLaTE XLIV. stone or gangue or metal matter. Jointed Slate. These narrow cracks were worked upon

by alkaline and acid solutions and

enlarged vy the process, the rock gradually eaten into being replaced by gangue and metal matter, a process often further assisted by the shattered character of the rock comm :n- ly found adjacent to a great fault: this shattered cavity was sooner or later eaten out, so to speak, and replaced by mineral

matter. Some of the broken rock, being not consumed in this way, was left, forming fragments in the vein, which when small are called " breccia" and when large " horses." The great "gash" fissures, such as we find occupied by socalled fissure veins in volcanic sheets such as those of the San Juan region, Colorado, appear to be due not so much to great earth movements, like the last, as to openings formed by cooling and contraction of the lava, somewhat as may be observed on the cooling of iron in a slag furnace. Ore deposits of lead and other minerals forming

PLATE XLV. PiatTeE XLVI.

Joints in Columnar Basalt. Centact Ore Deposits Between Porphyry and Limestone.

bedded deposits in limestones find their way in solution through the vertical joints common to ali water-formed rocks, resulting from contraction in consolidating from a soft, muddy condition. Such fissures are short, but they act as channels to a more important line of weakness occupied by the main body of the blanket ore deposits, viz., the dividing line between one stratum and another. Another line of weakness for the attack of mineral solutions is at the juncture of a porphyry sheet or dyke with some other rock, The interval between them is often occupied by a" contact vein." The heat of the volcanic matter together with steam may have influenced the solutions, even if the porphyry did not actually supply the metallic element in te vein.

Folding And Faulting,

In the many and great upheavals of the earth's crust, resulting in ccniinents rising above the sea, and on those continents still greater and sharper upheavals forming mountain ranges, rocks have been much broken and fractured, from great fractures, forming fissures miles in length and depth, down to little cracks of but a few inches. Much of this fracturing has been caused by the folding and crumpling upward of strata into mountains, accompanied by great crushing and mashing together of the rocks. When this lateral tangential folding and compression of the rocks reaches its maximum intensity, the rocks break, and a fault or slip is the result, with its attendant fault-fissure. This relieves the strain for a while, but the shock, doubtless at the time accompanied by earthquakes on the surface, resulted in a general breaking up of the adjacent country into many parallel and smaller faults and cross faults, besides a general shattering of the ground intermediate to the faults. A region thus faulted and shattered is justin the desired condition for forming a future mineral belt or mining region, when the cracks and scars thus made have been headed and filled up by mineral matter, brought in through the agency of watery solutions more or less alkaline or heated.

Intrusive Igneous Rocks.

When these fault-fissures descend to a very great depth, taey may tap the molten rock reservoir supposed to lie beneath great mountain ranges, and the molten lava or porphyry rushes upward through the weak line of the fissure, fills it with its matter, which on cooling becomes a dyke instead of a mineral vein. These eruptive rocks may or may not reach quite to the surface and overflow it in a lava sheet. Jf they do not, they find relief by intruding themselves laterally between the layers of stratified rocks, whose leaves or bedding planes may have been partially opened, like the leaves of a crumpled book by previous action of folding. In such cases the porphyry dyke or intrusive sheet may, if it be mineralized, answer all intents and purpose of a mineral vein, or the ore may be found on one or both sides of such a sheet, in the line of separation and

a

weakness between it and the adjacent strata, or it may permeate and mineralize by a" substitution" process an adjacent porous or soluble rock, such aslimestone. Thus both in the dyke or intrusive sheet itself, as well as at its contact with other rocks, the prospector should look for signs of precious metal.

If the dyke or sheet should be decomposed, clayey, and rusty, .t may contain free gold disseminated through it, which, at a depth which may or may not be ever reached by mining, passes into the auriferous iron-pyrites from which the free gold originally came. 'In this case the ore will be no longer " free" or " free-milling," but of a character that must be subjected to the more expensive treatment of roasting or smelting. Little stringers or veinlets of quartz, if observed in such an eruptive rock, should lve carefully examined as the most likely source of the richest gold ore. Some of our most noted gold mines in the West are in these "rotten" mineralized dykes or eruptive intrusive sheets. "Likely signs" in such would be rusty " gossan" stains of green carbonate of copper and gouge or clay matter. It is worth observing that the dyke may be only valuable as a mine as far down as the decomposition lasts and as long as the ore continues in a free state. With depth, the pyrites of the undecomposed lower portion of the dyke may be found too poor in gold to pay for smelting even.

As this desirable state of decomposition is the result mainly of the action of surface waters, a prospector may consider sometimes, where, on the outcrop of such a dyke, the rock is most likely to be deepest a:fected by surface action; for example, more probably below the old stream bed than on the top of a mountain, but this is not always the case. Most dykes and intrusive sheets when mineralized are mineralized by pyrites rather than by galena; hence they are generally more gold-bearing than silver-bearing. The contact deposits adjacent to a volcanic rock may have been aided in their deposition by steam issuing from the molten mass, or by heated waters or steam ascending with it, or generally by the heat of the dyke, as heat together with moisture is a great solvent of rocks and promoter of chemical action. —

In granitic rocks, if a " contact" deposit occurs adjacent to a porphyry dyke, it is usually a quartz vein, or a vein com-

f

posed of quartz and feldspar, commonly called " pegmatite." Such contact fissure veins may be on one or both sides of a dyke. The telluride veins of Boulder and the gold and silver veins of Idaho Springs, Central and Georgetown in Colorado are often so situated.

Contact Deposits,

When a porphyry sheet intrudes itself into limestone as at Leadville, the ore may be looked for on either side of

PLatE XLVII.

'*Contact Blanket '' Ore Deposits and 'Contact Fissure Veins,"

this sheet; but more commonly below it. At first the ore seems to permeate the limestone immediately at the line

of contact, but from this somewhat horizontal line it is apt to run down through joint cracks in the limestone, enlarging the cracks by solution, and substituting or replacing the dissolved rock with silver-lead ore, by a process called " metasomatic substitution."

" Metasomatic" means literally "an interchange between one body and another." In this case it is an interchange between metal and limestone, by which the limestone is gradually replaced, molecule by molecule, with metallic matter. Thus we may suppose, that as the mineral solutions were working on the limestone, rotting and soaking and dissolving it, as each molecule of lime was dissolved it was replaced or substituted by a molecule of metallic matter, until a large body of the rock: was replaced by ore. This appears to be the true way in which most of our ore bodies were formed in limestone and either soluble rock, rather than that they were " washed in" and " deposited" in " pre-existing large cavities" as some have supposed.

Blanket Deposits On Bedding Planes,

The solutions, having worked their way down through these vertical joints, may reach a second line of weakness, viz., the bedding plane or line of stratification between one bed or stratum of rock and another, and deposit along it as ona floor. This may be between one heavy bed of limestone and another. If it is between two dissimilar rocks, such as between limestone and quartzite, or even between limestone and magnesian limestone called dolomite, it comes under the name of a "contact" deposit. Thus it is noticeable that besides great fissures, lines of weakness or "bedding planes" are favorite places for ore deposits, to which the natural vertical joints often act as feeders, as well as themselves containing large " pockets" or " chambers" of ore. When the deposits are confined to these "pockets" and there appears to be no "blanket" deposit, the mine is said to be " pockety," and after a " pocket" is exhausted an immense amount of money and work and blind " gophering" often follows in hunting for another pocket. There is in this case little rule to guide the prospector. Locally, by experience in the mine, he may notice that some fine line of gypsum, calcespar, or iron stain is apt to lead to a pocket and follow it. In the mines of Aspen,

BOSSE ION eR ete a Say

ET ae

AE a 8 RL SN teas a NEO NRO HR ree Perm DO

where the mineral zone lies irregularly but generally near about the line where the limestone becomes dolomized, a miner, when his ore " plays out," follows as closely as he can this line, which he is able to do by the different hardness of the limestone and dolomite, the latter causing his ick to "ring." In every mine there is generally some ocal sign to assist the miner in following up his lost ore.

Surface Signs,

The prospector in hunting on the surface outcrop for signs of such contact or blanket or pocket deposits must look out for signs of decomposition along the line of con-

f Lo be rs sd V go an ow. 'eo Gee a SES

z, 'Sunem

oe

"a ibe

Ore Zone pie ae

Prospecting with Diamond Drills.

tact, such as lead carbonates, carbonate of copper, oxide of

iron, together with crystalline matter, such as calespar,

gypsum, or baryta. He may also observe, in the vertical

joints leading down from the surface into the body of the limestone, rusty clay fillings and iron stains. in these "blanket" bedded deposits,

Ky SS prospects on a large scale may gy £3 Y, sometimes advantageously be Ga f made by drilling with diamond

NS V drills from the surface down SS through as many of the strata N as are suspected of being ore NS bearing; the "cores" brought N up will show if an ore body has

been penetrated, together with

its approximate thickness at a certain point, andif this process is continued over a certain

area, the approximate areal

PuatE XLIX. limit of the are ey may be as- Brecciated Lode with Quartz certained. This work may fol-

: low upon a close examination

first of mineral signs along the outcrop. it is sometimes done after an area has been exploited for some time by

PiaTE L, Brecciated Vein.

actual mining with a view of discovering new bodies or continuations of the ore.

Yrue Fissure Veins.

Whilst profound fault cracks may be filled by lava, those not descending to such great depths doubtless lay open, till they were gradually filled by solutions carrying in earthy vein-stone and metailic matter; in a word they were

Waelder sconeromact ty bse

fe re ee me

the channels of mineral or hot springs. It must not be supposed that these fault cracks were ever "open chasms" commensurate in width with the wide dykes and veins now found in them, but rather in some cases very close-fitting cracks, mere lines of weakness, the walls appressed closely together by prodigious lateral pressure. In other cases the fissure would be rather a shattered zone passing down through the strata, than one definite line of fissure. Doubtless when the molten lava ascended through these fissures it greatly widened them to admit of its volume. In the case of true fissure veins, the fissure or shattered zone was enlarged by the corroding, substituting power of acid mineral solutions till we have to-day a fissure vein twenty to fifty or more feet in width. In the shattered zone, this substituting process would go on easily and rapidly, until nearly all the shattered fragments were replaced by mineral matter except a few "indigestible" pieces, which, if small, would cause what is called a brecciated vein, and if large, "horses" in a vein. These fragments are not so much pieces that have fallen from above into an open fissure gradually filling up with solutions of quartz and vein matter in which they became entangled, but rather undigested, unsubstituted fragments of the wall rock, immediately adjacent to the fragments, for at times some line in the fragment corresponds to a line in the adjacent wallrock without evidence of any serious displacement. Again, the shadowy outlines of fragments can be observed partially but not entirely replaced by quartz or vein matter. Sometimes the "breccias" are surrounded by rings of quartz or metal, and called " cockade ores."

Horses,

In the San Juan region in Colorado, where we have wonderful opportunities of observing extensive sections of yreat fissure veins descending the faces of cliffs on either side of a canyon for two or three thotisand feet, such broad veins at intervals split up into two or three arms enclosing large fragments or " horses' of the lava country rock, and again unite to form the main vein. These veins occupy a once shattered fissure, the walls of which were originally neither straight nor regular, but shattered and cracked.

The vein matter insinuated itself between the shattered portions, sometimes forming a "breccia" of small fragments, at others "horses" of hove ones.

The appearance of these great San Juan veins from a little distance is that of broad yellow stains of oxide of iron contrasted with the sombre gray of the lavarocks. Insome places in this region the quartz, vy reason of its superior hardness, stands up above the softer lava like a low, rusty, or white wall. Again, at other localities instead of being a bold outcrop, the vein is represented by a sharp, shallow depression forming a narrow little ravine or trench, the path of a rivulet and zone of abundant vegetation. In this Pill case the vein was full of decom- " fi kPAT posable minerals, such as pyrite,

PiateE LI. whose oxidation decomposition products were washed out leaving a depression in the rocks.

So, amongst some of the indications of a fissure vein to the prospector we may note:

ist. Brown or green stains on rocks.

2d. A bold quartz vein like a wall above the country.

3d. A narrow ravine or gulch.

4th. The path of a rivulet and exuberant growth of vegetation.

Horse or Rider.

Signs Of Faulting.,

As these fissure veins are generally the filling of fault cracks, and the fissures are mainly due to faulting, a prospector should be able to recognize the surface and other signs of faulting.

Faulting, as we have said, is generally the result of extreme folding. So, in entering a mountain region by way perhaps of a canyon cutting right through it on the exposed face of the cliffs, he may observe some of these folds or arches, low and gentle at first, but gradually, as the range

is penetrated further, increasing in sharpness, steepness, and closeness; with this increase we may expect faults. The presence of the fault may be indicated by a little "sag" or depression in the outline of the hill, or by a line of rubbish and broken rock descending the face of the cliff, or by a zone of exuberant vegetation, or by the pathway of a little rivulet. He will observe a general fractured tendency of the rocks as they approach the fault line. By closer search he may notice pieces of rock polished or slickensided by the movement of the walls of the fault slipping and grinding upon one another. Slickenside isa sure proof of motion having taken place in the rocks, and is often observed on the walls of fissure veins. A much faulted region is often marked by a step-like outline, each step representing the fallen or risen side of a fault block. These fault-lines should be carefully examined for mineral indications, especially if the fault line is occupied by a porphyry dyke or a vein of quartz or calespar. Sometimes these fault lines are totally barren, both of quartz, veinstone, or metal. liferous matter. They may be filled up with clay, rub- Piate LIL.

bish, and broken reek, or Vein a Faulted by Cross-Vein B. the two walls may be actually

welded together by pressure accompanied by a certain amount of heat, producing local metamorphic action.

Faulting too in some regions may have occurred comparatively recently, or at least after the period most marked by deposit of mineral solutions and ore deposits, in which case the fissures may be barren or at present occupied by hot or mineral springs making veins for the future. A stupendous, comparatively modern fault runs along the west base of the Wahsatch Mountains in Utah; its line is marked by a series uf hot springs.

Along the face of a canyon wall the prospector may notice some peculiar stratum mear the top of the cliff and its counterpart out of place near the bottom, showing that a fault has occurred, whose amount of slip he can easily estimate or measure; but when a fault of many thousands of

PiatTeE LIII. Folded and Faulted Structure of Mosquito Range, Colo.

feet occurs, a knowledge of the different geological periods involved in the slip is necessary to estimate the amount of fall. Thus, if a prospector by his geological knowledge should recognize a Cretaceous rock, brought up in close juxtaposition to a Silurian rock, he would know that a stupendous fault had occurred at that place, involving the entire thickness of the rocks composing the periods intervening between the Silurian and the Cretaceous.

That a faulted region is one in which great folding due to lateral tangential pressure has taken place, the folds eventually breaking down in faults, is well seen in the structure of the Mosquito Range in South Park, Colorado, which embraces the Leadville mining district.

The comparatively horizontal strata of the Park as they approach the Mosquito Range begin to fold gently, the folds gradually increasing in steepness and closeness as they approach the axis of the range. As we pass up Four Mile Canyon, which shows a complete cross section of the range, we find the axis to be formed by a magnificent and very steep arch, well shown on the face of Sheep Mountain, which, having arrived at its utmost tension, breaks down in

ee

ee

what is called the London mine fault, traversing and splitting the range for twenty miles. The line of the fault is shown by a depression between Sheep and Lamb Mountains. In nearly every canyon along the flank of this range, the line of the fault is easily traced by similar arches and "sags," and by a peculiar wavy look of the turfed strata as they bend down toward the fault. As we penetrate further across the range, we pass a series of such faults, each one formerly represented by a steep fold that preceded the faulting. ence it is that we descend from the top of this range down into Leadville and the Arkansas Valley by a series of gigantic steps or benches, each bench representing a fallen faulted block. Faults have their points of maximum depth and disturbance, from which they are apt to die out at either end in folds or rounded hills. Great faults are accompanied by minor parallel and cross faults.

The ultimate cause of this folding and faulting is attributed by some geologists to the interior of the earth growing colder and contracting, causing the surface crust to shrink and fold in adapting itself to the shrinking interior. Prof. J. F. Kemp says: " The strains induced by cooling and contraction of the earth are the most important cause of fracture. The contraction develops a tangential strain, which is resisted by the arch-like disposition of the crust. Where there is insufficient support, gravity causes a sagging of the material into troughs or synclinal folds which leave corresponding arches or anticlinal folds between them. Where the tangential strain is greater than the ability of the rocks to resist, they are upset and crumpled i :'o folds from the thrust. Both kinds of folds are fruitful c.u3es of fissuring cracks and general shattering, and every slip from yielding sends its oscillations abroad, which cause breaks along all lines of weakness."

Joints.

Joints, common to all rocks, appear to be due not so much to faulting and motion, as to shrinkage of the rocks in passing from a soft matter or muddy condition to one of consolidation. A good many so-called fissure veins, even in the granite series, appear to occupy extensive joint cracks, rather than fault planes. These may be due tu the

we anata ge npr ny pe a

4:

W, . "ee

general shrinkage of the whole mountain mass in consolidating from a semi-plastic or aqueo-igneous state of soften- a to one more consolidated and rigid.

he joints in lava sheets forming curious columns, like those of the Palisades of the Hudson, are due to the same shrinkage from a molten state. Such joints may sometimes be mineralized for a short depth, forming what are called "gash" veins, rather than true fissure veins. The joints in sedimentary rocks are due to consolidation from a soft, muddy, incoherent condition; such joints may similarly be occupied by gash veins, or may lead to pockets or wide blanket deposits.

The line of weakness between one stratum or one set of strata and another, often a favorite line for blanket deposits, is due to one stratum being first laid down and parwey consolidated before the next was laid later on top of it.

Impregnations.

Rocks made up of loose material, such as porous sandstones and conglomerates, are sometimes permeated by ore solutions, as, for example, the " Silver-reef" sandstone of Utah. Sandstones are frequently impregnated with iron and copper stains. In fact, if we consider that ore bodies were deposited from aqueous solutions, we have only to consider the various opportunities the rocks afford by their texture, structure, etc., for this process. Veins, in a word, are filled waterways of many and various kinds.

Chapter Vii. Various Forms Of Ore Deposits. Ore Beds,

"Ore beds are metalliferous deposits interstratified between sedimentary rocks of all geological ages. They lie parallel to the planes of stratification and follow all the contortions of the enclosing strata; hence they are thrown into folds, troughs, arches, saddles, or basins. The upper

oo

portions of the arches may often have been removed by erosion, or the strata may be faulted." The ore deposits or beds at Aspen occupy a faulted synclinal fold or basin. The enclosing rock is limestone, in part dolomitic. At Leadville the deposits occupy part of a series of faulted anticlinal arches and synclinal troughs, of which the

Mosquito range is the main axis. The beds lie Diutead a agian fiiai ana between dolomitic lime-pair "Beactal wae

stone and sheets of porphyry

. The ore beds partake of all the folding, faulting and other contortions which the enclosing rocks have suffered in the upheaval of the mountains.

The thickness of such deposits varies much and may gradually thin out and disappear, but may also continue iong enough for all mining purposes.

Often there are no sharp limits between an ore bed and the enclosing rocks, or between the ore bed and the walls, if walls exist at all. The ore appears to impregnate the surrounding rock by a chemical interchange between the elements of the rock and the ore. Such a " metasomatic'" interchange, "substitution," or "replacement" appears to have taken place in the argentiferous lead deposits of Leadville wor Aspen between the ore and the limestones.

According to Phillips, "a true ore bed never produces a 'combed' or 'ribbon' structure made up of symmetrical layers, such as is common in so-called 'true fissure veins,' and is usually without the crystalline texture observable in veinstones."

Unstratified Deposits, Fissure Veins, Etc.

Mineral veins are changeable in character, and their appearances of a perplexing and complicated nature. There is a gradual passage from one form to another, so that it is difficult to classify them. There is often no such sharp distinction between one form of ore deposit and another, as

go

legal disputes would sometimes demand, and a witness should hardly be called upon to assert on oath that such a vein is a" true fissure," or another a " bedded vein," or a third a "segregated vein." "Nature abhors straight lines" and sharp distinctions, and delights in blending one form imperceptibly with another.

Phillips divides veins into two classes, "regular and irregular veins." " Regular unstratified deposits include true veins, segregated veins and gash veins. Irregular deposits include impregnations, fahlbands, contact and chamber deposits."

Veins are collections of mineral matter, often closely related to, but differing more or less in character from, the enclosing country rock, usually in fissures

PLaTE LV. formed in those rocks after the A Split Vein. rocks had more or less consolidated.

All veins do not carry metals; some are merely barren quartz, feldspar, or calcspar, like the barren veins we so often see traversing granite or limestone rocks,

Veins may divide, "split up" or thin out, and are irregular in shape and structure, owing to the irregular width of the fissures and to other causes.

Definition Of Mining Terms.

The rock in which a vein is found is called the " country rock," ¢.g., limestone, granite, porphyry.

The portions of country rock in direct contact with the vein are called respectively the "hanging wall," or roof, and the "foot wall' or floor. This is only in inclined or flat veins, as a vertical fissure vein can have neither roof nor floor, but only two walls, east and west, or north and south, according to the compass. The inclination of a vein to the horizon is its "dip." The horizontal direction of a vein at right angles to its dip is its "strike." The latter may commonly be observed along the surface outcrop, the former either in the workings of the mine or where the vein is exposed on the side of a canyon.

2p ec Tina inisaeatecteie aloe arenes shits PT ni,

gI

Both dip and strike of a vein often vary much, the former with depth, the latter with extension across the country. Avein or ore deposit will not unfrequently begin with a gentle dip, and increase rapidly in steepness with depth. The ore deposits on Aspen Mountain commonly begin with a dip of 25°, and at a depth of less than a thousand feet reach 60° or more.

As fissure veins commonly occupy fault fissures, their irregularities in dip and strike correspond to those we have already spoken about, under faults

The angle of dip is usually taken from its variation from a horizontal, not a perpendicular line. Thus, a dip of 75° means one that is very steep, while one of 10° is a gentle inclination.

A layer cr sheet of clay called " gouge," or selvage, often lines one or both walls of a vein between the country rock and the gangue or vein proper. It is derived from the elements of the adjacent country rock, decomposed by water, and sometimes by the friction of the walls of the fissure against one another, or against the vein matter, in the

rocess of slipping and faulting, which is often shown by its being smoothed, "slickensided," polished, or grooved. Gouge often contains some rich decomposed mineral in it, such as sulphurets of silver. It sometimes occurs in the heart of a vein, especially if that vein has been re-opened anew by movements of the strata. The "Chinese tallow" gouge of Leadville results from the decomposition of the feldspars in the adjacent white porphyry, and is a hydrous silicate of alumina.

In the granite veins in Clear Creek County the gouge is derived from the feldspars of the granite. Gouge is sometimes useful in defining the limit of the vein between walls, thus preventing unprofitable exploration into the "country." It is also a guide for following down a vein when mineral and gangue may be wanting or obscure.

Both walls are not always clearly defined by slickensided

surfaces, by gouge or other mark, and so at times the vein

is lost.

False walls, caused by movements in the adjacent strata, by joints, etc., also mislead.

It is not uncommon for a fissure vein to have but one clearly defined wall, the other, if it exists, being obscured

g2

or changed by mineral solutions. Sometimes two cracks or fissures occur parallel to each other and the intervening country rock has been altered and mineralized into a vein. It is probably in this way that many wide veins were formed.

Mr. Emmons has found that fissures are formed by great movements of the earth's crust or by local contraction of the rocks, and that a fissure is not necessarily one with well-defined walls at considerable distances apart, filled after the formation o1 the fissure, but that the ordinary cracks or joints in granite quarries, extending regularly to great lengths or depths, illustrate the original fissures which have been changed by percolating waters carrying mineral solutions into veins and deposits of ore. In all crystalline and sedimentary rocks, these cracks or joints run parallel to each other at various distances apart, often plentiful and close together. Incases where percolating waters were charged PLatE LVI, With the proper metals and veinstone matter and the necessary chemical and physical conditions existed, the rocks lying between those cracks or joints were

Tpregnationot Rock y Vein.

altered into ore.

As one element was dissolved another took its place; so, according to this authority, it would seem that even a fissure vein may be only a sort of " metasomatic replacement" of rock by mineral. Hence, what is commonly accepted as a "wall" of a vein is not necessarily one, and cross-cutting, in order to determine the lateral boundaries of the ore, is safer than to rely on supposed walls. so-called "slip" has often been followed by a miner as a supposed wall, until by accident he broke through and found good ore on the other side. If veins are formed according to Mr. Emmons' theory, the occasional loss of one or both walls is easily accounted for.

Cross veins of a more recent age sometimes cut or fault an older vein. The point of intersection is generally rich in mineral. Cross veins must not be confounded with "leaders," which are the filling of minor cracks extending

¥ y % wv it e

#

DR ters.

off from the vein, and are sometimes sufficiently profitable to work. While they sometimes lead a prospector to the main vein, they may also lead a miner underground astray from the true vein.

The splitting of a vein by a " horse," or large fragment of the country lying in the vein, may be mistaken for a true cross vein, or the original fracture of the fissure may have been in the form of a star or like the spokes of a wheel radiating from the hub.

In such cases there are no true cross veins. But when, as in the San Juan district, we have two well-defined sets of veins, one striking northeast by southwest, and the other northwest by southeast, they cut each other diagonally, the cut vein being the older. These opposite sets of veins have been formed at different times. Many contain a characteristically different class or variety of minerals. Thus, in Cornwall, England, one set carries tin and the other lead.

Signs Of A True Fissure Vein.

True fissure veins show signs of motion or slipping on the sides of the fissure, such as slickensides, gouge, crushed walls, " horses," or " breccia," the latter being small portions of the country rock surrounded and cemented by vein matter. In the Comstock, the quartz is ground to powder. The vein itself, though occupying a healed fault fissure, may be itself faulted by later movements in the mountain after the vein was formed. Some of the fissure veins on Engineer Mountain, San Juan,

"yyy ZW

Z

are so dislocated. ' The vein-filled fissures be-ute 3 apa ahh weiss ing aline of weakness, may be "tre with Quartz Geode.

reopened by mountain movements, and other or different combinations of ore introduced into the heart of the vein. Such a reopening would be

marked by a succession of "combs" or banded ribbon-like deposits of ore, and by gouge matter.

Outcrop Of Veins.

The outcrop of a vein is that which appears at the surface and usually attracts prospectors to the spot. Sometimes it may be, as in the San Juan district, a bold vein of hard white or rusty quartz, standing up in relief, by its superior hardness, above the surrounding country, like a low wall. Or again, in the same district, from being composed of softer or more soluble substances than the prevailing eruptive lava sheets, instead of a wall, it causes a depression or trough on the side of a hill, forming the pathway for a rivulet and marked by luxuriant vegetation. Commonly the outcrop consists of a decomposed mass of rock, stained with oxide of iron and streaked here and there with green or blue carbonate of copper, and is called "float" or "blossom" by the miners. This float is the chemically changed or oxidized portion of the true and unchanged vein lying deeper below the soil. On Aspen Mountain the float is generally a rough crystalline mass of calcspar and baryta stained with iron and copper.

In this "blossom rock" free gold is not unfrequently found, but unaltered sulphides, such as galena or iron pyrites, are rarely met with on the outcrop. In the San Juan district, on Mineral Point, we have, however, found galena at the grass roots, and broken off large chunks of it from a quartz vein outcropping on the surface.

In gold-bearing veins such an oxidized condition is desirable if it continues down to any depth, for, so far as it continues, the gold is free, and the ore is a free milling one, easily treated, and often exceedingly rich in gold, as in the celebrated Bowen mine of Del Norte; but as soon as the hard white quartz and the unoxidized pyrites of the true vein is reached, the ore is no longer free milling, but must be smelted. The gold may still be found free, perhaps, in the hard quartz, but if the pyrites should not prove rich in gold, the palmy days of the mine may be considered as past. Many such rich deposits on the surface, abounding with specimens of free gold, have proved great disappointments with depth.

F

WIDTH OF VEINS, ; F , é ; H Veins may vary in width or thickness from a half inch to a hundred feet. They also pinch or widen at intervals in

q 4 i f ql

q fi i: it (7 id if j Piate LVIII. i" Metalliferous Veins Exposed to View near_Howardsville, San Juan, Colorado, Showing Two Byatems of Fissure Veins Crossing One Another, a their downward course. The widest "mother" veins are i not always the most productive, though they are very per- i tk a te +f HW

sistent in length, and we may suppose in depth also. In the San Juan district the " mammoth" veins of quartz, often a hundred feet wide, are not the favorites for development, the ore being found too much scattered in them, and the development less easy than in those 10, 20 or 30 feet wide, where the metal is more concentrated. These mammoth veins in the San Juan are easily traceable for miles over the surface of the country and down the sides of the deep canyons. Their limiting depth has never been reached, and probably never will be by mining.

Definition Of True Fissure Veins.

True fissure veins are popularly defined as filling fissures of indefinite length and depth, commonly occurring in parallel systems, traversing the surrounding rocks independently

of their structure or

stratification, and commonly,

though not necessarily, at an

angle different from that of the

stratification—in other words,

cutting across the planes of

stratification. These veins originated

in fissures, not necessarily

wide open ones, but on

Piate LIX. the contrary rather narrow

Fissure Vein Conforming in Part cracks, descending, however,

to the Bedding Planes of Stratito great depth, such as those

fication, in Part Crossing them. produced by faulting, or the

general cleavage lines of the

mountain. The latter may be frequently observed in every

canyon, and also in the sedimentary rocks of the foot-hills

and even along the flat surfaces of the plains. They are

very conspicuous in the plains around Trinidad, and are

there not unfrequently occupied by series of narrow parallel

dykes of basalt instead of by mineral veins. Cleavage lines or joints are familiar to every stone-quarry man.

These cracks are caused by extensive movements of the earth's crust in the process of mountain uplift, and also on a smaller scale by contraction of the rocks in cooling from a heated or molten condition, or even in consolidating from a soft or muddy condition.

The two walls enclosing a vein do not generally concide, as might be expected, if the vein occupies a line of fault. A true fissure vein may in some part of its course coincide with the dip of the surrounding strata. As the plane of stratification or line of division between one stratum and another is a natural line of weakness, a crack once started would be liable to follow it for some distance. And when uplift occurs such places are liable to slip one upon the reat sage Ay bir partin 'Bsn — rs conformable to the prevailing dip. Suc Y a vein might appear at first to belong to the class of so-called " bedded veins," but Uy if with depth it should be discovered to be Y cutting across the strata it would be pronounced a "true fissure vein." The appearance of slickensides or other signs 7 of motion on the walls of the apparent- ; ly " bedded portion" would then prove it to belong to the "true fissure" class, and that actual fissuring had taken place prior to the vein-filling.

Cause Of Pockets In Fissure Veins. Y

As a fault fissure in its downward course usually pursues a zigzag rather than a straight course with smooth sur- Y faces on either side of the crack, the in- Y equalities of one face of the crack are brought into opposition to the inequali- Y Y tics on the other face, as one or the other U3 side of the fault slips upor down, and py arg LX. thus are produced pinches and wide cavi- ., 44, a pike ties, which give rise to the " pinches" and " Tesuiting from Slip. " bonanza pockets" so common in fissure pin be neven veins. Aso-called true fissure vein may °° "Sure: sometimes have advantages over some other forms of vein occurrence, from its persistency and comparative regularity to great depths. It must not, however, be expected that it will continue equally rich or equally poor throughout its course. There may be comparatively barren spots and rich spots, pinches and widenings, local c ribinations

of richer or rer varieties of mineral. But the vein asa rule is not likely to entirely give out.

Richness With Depth.

There is no scientific reason why a vein should " grow in richness and size with depth." This is a popular fallacy, originating from the now less accepted theory that veins were formed by the precipitation of precious metals, by heated rising waters, or vapors, and hence that the greater concentration would take place at greater depths. The "lateral secretion" theory, now by some accepted, ascribes the deposition of ore to solvent waters reaching the vein from ground quite near to it, and coming naturally from above and thesides quite as often as it is ejected upward by pressure from below.

In Idaho Territory, says Mr. A. Williams, "the rule is rather that veins grow less rich and strong with depth, though strong veins may continue metalliferous to a greater depth than mining can ever reach.

The thickness of the earth's crust which we are able to explore isvery limited. Increase of heat, as in the deep Comstock mine, and other natural difficulties, limit us to a few thousand feet—3,o00 at most. These deep mines have not, as a rule, proved richer with depth, but to the contrary. Some veins have been worked through alternate zones of richness and barrenness. The Comstock, which has been cpenne for four miles in length and toa depth of 3,000 feet, shows the ore bodies to be scattered irregularly and the barrenest ground is at the bottom. On the other hand, some of the most celebrated mines derived their wealth from rich ores encountered near the surface and have proved most disappointing with depth."

Atmospheric action for along period has often reduced the ore to its richest compound, and when the hard material is reached leanness setsin. This, as we have observed, is commonly the case with gold veins. The richness of the Leadville mines is derived from their decomsed

compounds. Again, as the surface crust can be so ittle explored by mining, it is to be remembered that the erosion by glaciers and waters has already removed thousands of feet of the vein, so that we are able to examine

only a small fraction of it, while an unknown quantity lies in the depths below. If these veins, then, continue to the supposed great depths below, we are very far from their starting point, and erosion ayo removed their upper portions, we cannot find their surface finishing point; in other words, it is not a fresh "ready made" vein we find, but portions of an old vein already extensively mined by the processes of nature.

So far as our Le ae gee goes in Colorado, after a moderate depth is reached below surface action, or below the "water level," a fissure vein may grow richer or poorer, wider or narrower with depth, without any law except local experience in a district.

° Veins In Groups,

Fissure-veins occur in clusters and nearly parallel groups, forming a mining district, and again in that district certain peculiar veins may be grouped together, forming a " belt," Thus, Boulder district occupies a certain isolated area, outside of which few mineral deposits occur for a long distance. We have also in that district several distinct belts carrying different characteristic ores, such as the telluride belt, marked by rare telluride deposits, the pyritiferous gold-bearing belt, and the argentiferous galena belt. The Central City region is characterized by auriferous pyrites belts, Georgetown district, not far distant, by argentiferous belts, and Idaho Springs, lying between the two, by both gold and silver belts.

Chapter Viii. Veins To Eruptive Forces.

Relation Of

The ultimate cause of the richness in veins of a district or locality is, that local dynamic and eruptive forces were nore energetic there than elsewhere, causing great disturbance of the rocks, accompanied by fissures and eruptions of porphyry.

Thus at Leadville, the Mosquito range is violently folded and fractured, eruptive rocks have issued abundantly, and

associated with such phenomena we find great lead and silver deposits.

Further south the great San Juan district is split up in an extraordinary manner with great fissure veins. The region is an eruptive one, consisting of prodigious flows of eruptive rocks, traversed, not unfrequently, by newer eruptive dykes.

In the Gunnison district the strata have been overturned, disturbed, folded, and faulted in an extraordinary manner by the intrusion of great masses of eruptive rock forming the peaks of the Elk Mountains. The strata everywhere are riddled by dykes or intrusive sheets, and the evidence of heat is apparent in the general metamorphism of the entire region. Mineral veins abound. The same phenomena are repeated more or less in the neighboring region around Aspen, and at Pitkin and Tincup.

At Boulder, Central, and Georgetown there is a concentration of eruptive dykes locally in each district, and a few dykes or eruptive rocks outside of those districts. On the other hand, we have no ore deposits in the undisturbed rocks of the plains or the flat basins of our parks, and notably our mining districts are for the most part well into the core of the mountains, where, in the nature of things, folding, crumpling, faulting, eruptions, and metamorpbic heat were more energetic than along the flanks and foothills of the range which have usually proved unproductive.

The older eruptive rocks, such as the quartz, porphyries, and diorites of the Leadville, South Park, and Gunnison districts, are more favorable to the production of ore deposits, as arule, than the more modernly erupted lavas, such as basalt or dolerite, which we commonly find occurring in dykes and surface overflows, traversing or capping our Cretaceous and Tertiary coal fields along the foothills as at the Table Mountains at Golden and Trinidad.

Some of the lighter colored and somewhat recent lavas like the tufaceous rhyolite, which caps so many of the Tertiary mesas on the Divide between Denver and Colorado Springs, have also hitherto proved barren. Yet the volcanic rhyolites, andesites and phonolites of Silver Cliff, Cripple Creek and Creede are productive of both gold and silver. A large portion of the eruptive rocks of the San Juan region, productive of gold and silver-bearing fissure

as

veins, are in andesitic breccias of comparatively modern date. The older eruptive rocks, as we have stated, are nearly all of an intrusive character, never having reached the surface, while the newer ones bear evidence of having flowed over the country like modern lava-streams, as is shown by spongy scoria on their surface, and may be called " effusive."

In Colorado the ore body is not usually found in the heart of an eruptive sheet or dyke of porphyry, so much as at the line of its contact with some other rock, such as limestone, granite or gneiss.

Contact Deposits.

The "contact" ore deposits of Leadville occur at the contact of quartz, porphyry anc dolomitic blue limestone.

Some of the veins at Boulder, Central and Georgetown are at the contact of porphyry and granite or gneiss.

Exceptions occur, however, where mineral is found either in the heart of a dyke, or the whole dyke may be so impregnated as to constitute in a sense a vein. These exceptions are generally confined to pyritiferous goid deposits, and telluride gold deposits as at Cripple Creek.

Gold-Bearing Dykes.

Suppose a dyke or mass of eruptive rock to be thoroughly impregnated with gold-bearing pyrites. Near the surface and often for a considerable depth the rock is decomposed and the pyrites oxidized into rusty iron ore, liberating the gold which is entangled in the " gossan" in wires, flakes or even small nuggets. As long as this decomposed or oxidized state continues, the ore is free milling, but with depth the dyke is found in its primitive hardness, studded with iron pyrites, which may or may not prove rich enough for the more expensive treatment of smelting. Such goldbearing dykes are found at Breckenridge, South Park, also in Idaho Territory, Cripple Creek, Colorado, and in old Mexico, and many other gold-bearing regions.

The Printer Boy gold mine at Leadville is a vertical deposit in a jointing or fracture plane in a dyke of quartzporphyry, rusty and much decomposed near the surface, where it yielded free gold; with depth this passes into cop-

t

t

er and iron pyrites. The vein is from an inch to four feet in width; stringers carrying ore extend into the porphyry, which is highly charged with pyrites, which doubtless supplied the vein with mineral through the agency of surface waters. In Arizona, near Prescott, at the Lion mine we find a green dy ke. f eruptive diorite penetrating granite. This dyke is traversed by numerous small veins of white quartz which near the decomposed and rusty surface are rich in free gold. At slight depth the quartz veins become charged with unoxidized Sci WL ch ta Yas emai iron pyrites sufficiently rich in Dyke, showing Oxidized and Old to merit treatment by smelt- Unoxidized Portions. ing. The surface ore is treated by a simple " arrastra," and is, of course, free milling. The gold seems to be mostly confined to the quartz veins.

PLatre LXI.

Fissure Veins In Igneous And Granitic Rocks,

The San Juan district is an exceptional case where immense numbers of fissure veins penetrate igneous eruptive sheets. The fissure veins consist of hard gray jaspery quartz traversing lava sheets whose united thickness is from 2,000 to 3,000 feet. The veins produce lead, bismuthinite, gray copper and other silver-bearing ores.

In Colorado true fissure veins are most characteristic of the Archean granitic series. In fact, all the veins in that series are fissure veins. Locally they occur as in the San Juan, cutting through eruptive rocks. Outside of these formations few true fissure veins occur.

An exception may be made of the Gunnison and Elk Mountain region where the fissures traverse all the formations from Archean granite to the top of the Cretaceous coal beds. Nearly all other minera! occurrences, such as those in the limestone regions, come under the class of bedded-veins or blanket-veins, pipe-veins or " poc' ets," and show none of the characteristics of slipping motion or fissure

er

5 /m_m—hchTlUAlhWHTClCUPO O/C."

aS ww."

2 CSS OE — Oe ee

action. Under this latter class the Leadville and Aspen deposits may be grouped.

Ore deposits commonly occur at the junction or contact of two dissimilar rocks, as between quartzite and limestone or limestone and dolomite.

Lodes occur also between the stratification planes of the same class of rock, sandwiched in between two layers of limestone, and sometimes impregnating the layers on either side for some distance from the dividing line between the two strata, which is commonly the line of principal concentration of ore, and often descend from this concentration line, through the medium of cross joints, to form large pockets in the mass of the limestone. The Aspen and Leadville deposits are of this character. Also when ore bodies occupy a true fissure, 7. ¢., one cutting across the stratification planes, they may locally, for a short distance, impregnate the adjacent walls or country rock more ot less. Our fissure veins in granite and gneiss often impregnate the walls to a small extent.

N''neral deposits favor as a rule the older rocks, such as the .irchzan and Paleozoic series, propably because heat and metamorphic action are commoner in these older rocks, which have felt all the throes of the earth from past to presence cimes, than in the more recent ones, and such circumstances, as we have stated, are peculiarly favorable to vein formation and mineral deposition.

The bulk of our precious minerals in Colorado comes from the older Archean and Paleozoic series of rocks, the exception being the Gunnison region around Crested Butte, Irwin and Ruby, where ore comes from fissure veins in the Mesozoic Cretaceous rocks. The exception is accounted for by the local metamorphism, heat and eruptive phenoinena of that region.

The veins in the San Juan have also been ascribed by some to the Tertiary Period, owing to their occurrence in certain supposed Tertiary lavas covering that district.

Besides heat, metamorphism, dynamical disturbances and eruptive agencies, other minor circumstances may favor ore deposition. Certain rocks, such as limestones, may offer, by their tendency to solubility and chemical reactions, more favorable conditions than others for mineral solutions to deposit by " metasomatic" interchange between

;

mineral and limestone, until the limestone is gradually replaced by ore, much in the same way as the elements of a water-logged trunk of a tree are replaced by silica in the process of fossilization.

Change Of Minerals With Depth.

Lodes often change in the character of their minerals with depth, not only after they have left the zone of secondary decomposition and surface action, but also far below it. Thus, in the San Juan, some of the mines abound in zincblende near the surface, which with depth almost disappears, giving place to gray copper and other superior ores. In Cornwall, England, the shallow workings yield copper, and with depth, tin; and locally many such changes may characterize a particular district, but cannot be formulated as a rule for other localities.

Influence Of Country Rock.

In most mining regions, to which Colorado is no exception, a relation has been observed between varieties of "country rock" and ore deposits. Veins in passing from one country rock to another are liable to change in the size or variety of the ore, widening in connection with some rocks, and pinching or growing narrower in connection with others.

Certain rocks are notorious ore-bearers, whilst others are notoriously barren over large regions, or in special localities.

The presence of certain rocks adjacent to other different rocks has an enriching tendency on the ore bodies.

As regards rocks that are good ore-carriers or receptacles of particular classes of ore in Colorado, we may say: That quartzites and silicious rocks generally carry more pyrites, and are gold-bearing.

That veins in granitic rocks carry a greater variety of minerals than others, and may be both gold and silver bearing.

That certain limestones carry much argentiferous galena.

That sandstones and other unaltered rocks carry little ore of any kind.

The influence of country rock on veins may be from several different causes, for instance:

Certain rocks are by their structure better adapted than others for forming regular fissures. Thus, massive limestone is better fissured than slate or shale, leaving wider open spaces for the ore to collect in.

Other rocks may be more porous, and admit mineral solutions through their pores. Of such a kind are some of our porphyries, andesites and phonolites.

Others, like limestone, are easily acted upon by solutions dissolving out the rock and replacing it with mineral by substitution.

Some are better conductors of heat, and therefore would assist chemical action and mineral solution.

And lastly, if modern theories of "lateral secretion" be true, viz.: That most ore comes from the adjacent country rock and is precipitated, substituted, or collected in the vein fissure, and further, that the metals themselves are derived from certain metallic elements in the ordinary constituent minerals of the country rock, such as mica, hornblende, or augite, it is clear that a rock composed largely of such minerals would be liable to influence the vein as an ore generator. Granite, porphyries and andesites are largely composed of these minerals.

The frequent presence of eruptive porphyry rocks near veins and ore deposits in Colorado shows that they have an important influence on those deposits, which may be of various kinds.

First, that in their component minerals and mass they actually contain the elements of the precious metals subsequently deposited in another form in the fissure vein or in the soluble limestone in contact with it.

Second, by the heat which they retain for a long time after they have congealed and hardened, they would assist in the reactions of any chemical or' mineral solutions that might be on hand. Lava, at the time of its eruption, is always highly charged with steam and other gases. By reason, also, of the chemical composition of porphyry, waters passing through it would be alkaline and assist in dissolving silica and other gangue or veinstone matter, and when the porphyry has thoroughly cooled it is exceedingly porous, and being much jointed and cross-fractured,

2 aap tes ECS i

Sport a, ah to S"> aoa

iy

becomes like a great sponge for the absorption of all surface waters. This may be noticed at Aspen, where all the mines that are at present penetrating through the . porphyry cap" are much troubled with water, far more so than in the underlying limestone. Surface waters, then, becoming alkaline by passing through this rock, and also more or less charged with carbonic acid, chlorine, and other solvents, would be ready to dissolve both gangue and vein ingredients out of the porphyry and redeposit them in the vein fissure, or, by metasomatic substitution, in the limestone usually beneath it.

Water circulating in fissures, changes or dissolves the ingredients of the surrounding rock. The rocks enclosing lodes are always so altered, and this decomposition and alteration is not always merely local or confined to the close proximity of the ore body, but we often find a whole mining district, such as Leadville, Aspen and San Juan, pervaded by this feature. So much is this the case that it is often difficult to get a fresh, unaltered specimen of porphyry or some other country rock within the district.

The brilliant red, yellow and maroon tints that color so much of the mining district of San Juan result from the oxidation of pyrites and other iron-bearing minerals pervading

the eruptive rocks, and it is noticeable that this color, resulting from alteration and decomposition, is most prominent in those parts where lodes have been discovered, as, for example, the gorgeous tints of the Red Mountain area around the celebrated "National Belle," " Yankee Girl," and Ironton mines, between Silverton and Ouray. The rocks in Geneva Gulch, Hall's Valley, Buckskin Canyon, and in other mining centers, display the same beautiful tints of oxidation in the vicinity of the mines.

"In lodes a mutual exchange takes place through the reaction of the ingredients of the rock and the materials of the vein. Thus, when water containing carbonates comes in contact with rocks or minerals containing alkalies, a chemical reaction takes place. When these last are combined with silicic acid, these silicates are decomposed by the carbonic acid and the bicarbonates. This explains both the crystallizing out of the carbonates and the so frehaha decomposition of rocks containing lodes, especially those which, like our veins in granite, are feldspathic."

The same principle applies to other ores and minerals in lodes. Thus the precious metals, in the mines of Leadville in their original condition, have been proved by depth to have been in a sulphide state, such as iron pyrites (sulphide of iron), or galena (sulphide of lead,) etc. Surface waters charged with carbonic and other acids, passing through the overlying porous alkaline porphyry and entering the underlying limestones, have, as we have previously observed, changed the sulphides into sulphates, oxides, and carbonates.

The presence of a dyke near to or cutting a vein has been found often to enrich the latter at the point of contact.

In the " Colorado Central" mine at Georgetown a narrow : dyke of brown obsidian traverses a large dyke of ore-bear- 4 ing porphyry. The valuable ore is found close to the obsidian dyke. 'This might be the result of greater heat y at that point. The "black dyke" in the Comstock mine is q a somewhat similar case.

if

;

;

Prejudice In Favor Of And Against Certain Rocks.

There is often a prejudice amongst miners in favor of certain rocks and formations, and against others. Miners who have worked perhaps in the great Comstock mine of Nevada or the Leadville mines of Colorado, or the fissure veins in granite of the Old World, are apt to look out for and favor certain rocks and formations they find like those g they have been accustomed to. Thus, as Mr. Williams t says: " The peculiar 'porphyry' of the Comstock was hunted up in other districts, but did not prove metalliferous. Solid t granite was looked upon by others as unfavorable, gen-if erally, because locally some granite above the gold belt of California had proved barren. Yet some of our best veins are in granite.

" Limestone was at one time a very unpopular rock and supposed only locally to produce lead, till the discoveries of Leadville, and Eureka, Nevada, overturned the scale in its favor."

In the Leadville " excitement" not only was the particular Carboniferous limestone of Leadville hunted for and prospected, but every other limestone in the South Park region, no matter what its geological age or position, was

cotrestrannetiedtsesmneeinemnsit at ape

] neared e P ERP NE I PB TORT PTET RES ay

extensively prospected without results, miners not recognizing the fact that it was not limestone generally that produces rich ores, but a particular limestone of a particular geological period (the Lower Carboniferous) not over 200 feet thick, that happened locally to be rich near Leadville, and the reason of its being locally rich at that point was owing to the concentration of eruptive energy at that point and the intrusion of an unusual amount of porphyries, which in point of fact are far more responsible for the ore than the limestone, which happens to be merely the receptacle.

It was also quite common after the Leadville excitement to find shafts in all sorts of improbable and hopeless localities, whose owners would tell you: " At Leadville it didn't matter where a man 'went down.' It was all luck whether you 'struck it' or not, and so they might as well 'go down' where they were as elsewhere." It was often said "that Leadville had exploded all so-called scientific theories about ore being in one formation or locality more than another. It was all a case of luck."

The excuse for this is to be found in the fact that in the immediate vicinity of Leadville it did scarcely matter "where you went down," seeing that that area was practically underlaid by bedded sheets of mineral, but that such would be the case elsewhere and everywhere or -anywhere, experience unfortunately has shown to beuntrue. Itisnota particular rock or formation, but a combination of favorable circumstances, that alone can make a rich mining district.

As experience advances, geologists and miners have proved that ore deposits have a much wider range than was once supposed. Formerly only the Archean granite series was supposed capable of bearing ore deposits, because in the Old World, tin, copper and lead came principally from fissure veins in those rocks. Then deposits were found in the Paleozoic series and supposed to ascend no higher. But in the present day, and even in Colorado, they are traceable even to the Tertiary.

It is not the rock, nor the age, but a combination of circumstances, principally heat and metamorphism, that may make any rock of any period an ore-bearing one. And in prospecting in new regions it is these combinations rather than any particular rock that should be looked for.

Strike And Dip Of Veins.

The dip of veins approaches more nearly the vertical than the horizontal, usually from 75° to verticality. Nearly all our ore deposits, in Colorado, even those of the bedded class, dip more or less steeply from 25° to 75°.

For a few feet from the surface, on the steep slope of a mountain, it is common to find an ore deposit dipping quite gently or even folded over and dipping in a contrary direction to that which it assumes with depth. This appears to arise from the weight of the strata above it tending to bend it over downward in tl .. direction of the slope of the hill.

Th re is generally a prevailing dip and strike amongst a number of parallel fissure veins of a district. In the San Juan, the bulk of the fissure veins have a prevailing northeasterly strike and dip to the southeast. The angle of dip is generally between 60° and verticality.

Cross-Cutting Uncertain.

The dip, as we have said, not unfrequently changes considerably with depth, usually becoming more and more vertical. From the degree of uncertainty as to the continuity of the dip, it is not always safe, on the discovery of an outcrop, to endeavor to cut it at a much lower point, so as to get the coveted depth, and better opportunities for stoping, drainage and other developments of the mine. Owing to a change of dip or fault, perhaps, the miner may have to make a much longer cross-cut tunnel than he had calculated upon be- Pirate LXII. fore striking the vein. Ninel a

f owing How Cross-cut 'Tunnels and Sometimes, too, he may Shafts May Miss Veins by Change of miss the vein altogether, Dip or Faulting. cutting it perhaps at some point where it is exceedingly thin or poor, so poor in fact that he passes through it without noticing it or believing

it to be the same vein whose outcrop looked so promising

on the surface. Cross tunnels through " dead rock" should

hardly be undertaken until the vein has been proved to be

a strong one for aconsiderable depth. As we have already

shown, great depths may not after all be so desirable in

even a fissure vein, as there is no certainty whatever about

veins becoming richer or poorer with depth. Extensive

cross-cut tunnels have seldom proved paying concerns.

The greatest in the United States, the Sutro tunnel, six

miles in length, which tapped the Comstock fissure at a

depth of 2,000 feet, did not prove a financial success, and

had it tapped the fissure still

lower, at 3,000 feet, it would

have found the vein in the

impoverished condition it is

today. It is not uncommon

for a miner to strike a rich

outcrop on the top of some

mountain, and on the

strength of its richness induce

company to run along

cross-cut tunnel in "dead

: rock" half through the moun-

Pare LXIIL. tain to cut this vein, and the

Fissure Vein Exposed from Outcro ee a

to Dip. P nearly exhausted in so do:

ing, while the vein itself

gives no returns, owing to its being left idle. Finally,

perhaps, the vein is missed, or if struck, proves far poorer

than was anticipated. Of course there are exceptions where cross-cut tunnels in "dead rock" may be advisable.

If a fissure vein, as in the San Juan, should outcrop near

the top of a mountain and be exposed on its dip all the way

to the bottom, there may be some reason for opening a

tunnel in it near the base, thereby facilitating drainage,

development and exportation. In that case the miner is ov

the vein, with no fear of losing it; but even here, there is

no guarantee that it will prove rich all the way to its outcrop

a thousand feet above. "Follow your ore, and be

careful how you leave it for any experimental theories," is

acommon and wise saying among experienced miners.

We remember a tunnel in the Gunnison region which was

run several hundred feet at a cost of many thousands of dollars, all through " dead rock," in the hopes of cross-cutting a certain ore body that had proved rich near the surface. At last it was given up, and subsequently a short cross-cut was made from it, and the original vein was found only a few feet from the tunnel, which had been running parallel with it all the time. The cause of the mistake was an unforeseen fault in the vein that had shifted its dip much further on one side than had been calculated upon.

Chapter Ix.

Gold Placers. Prospecting For Placer Gold And Gold Veins,

Having given in preceding chapters a sketch of veins and ore deposits in the rocks, it follows in order to speak of gold placers, because these are derived from the former by the agencies of water, either in the form of glaciers of old, or of ancient or modern streams,

Plate Lxiv.

Open Placer Grounds in Canyon.

The glaciers in olden times heavily mined the rocks and the veins, by cutting broad gashes through them, thus originating the canyons. In this way millions of tons of rock were mined, together with the gold-bearing veins in

them, and also the precious metals minutely diffused and scattered throughout their masses.

After the glaciers, the rivers took up the work, deepened the canyons, broke up the boulders and sorted them, setting free the gold and other metals they contained, and again sifted and sorted them and deposited them along their banks and in their beds.

Of the various metals thus handled by nature's jigging process, many were dissolved and destroyed by various acids in the waters, and by acids of vegetation and iron salts percolating through the placer dumps after they had been laid down. So with the exception of a few very hard minerals, such as magnetite, diamonds, garnets, rubies,

Plate Lxv.

Section in Gold Placer.

etc., little remained in the placer but the imperishable gold, and even that appears to have been refined of its alloy of silver which it contained in the original vein, for placer gold is generally much purer and more valuable than that in the original vein.

In some cases, too, the fine gold disseminated through the placer appears to have been acted upon by certain salts, such as the persalts of iron, and concentrated and amalgamated into large nuggets. Some contend, however, that these nuggets are only waterworn pebbles of gold, brought direct from the vein, the result perhaps of concentration there of the contents of large masses of goldbearing pyrites; it is to be noted, however, that whilst gold-bearing nuggets of various sizes are to be found, not

uncommonly in gold placers, they are very rarely found in gold veins.

With the gold in placers is commonly found what is called " black sand," which is composed of grains or pebbles of magnetic iron ore, relics of the old. gold-bearing pyrites chemically changed. ae near in gravity to gold, and originally associated with it, the two are generally found together in a placer, and a prospector in surveying a bank of placer-material made up of sand, pebbles and boulders, generally looks for a streak of " black sand" as a likely place for gold. Also by reason of the gravity of gold he is inclined to look for it more down on bedrock than in the upper looser strata.

Ancient river beds as well as those of modern rivers may be found gold-bearing, rivers that have long ceased to flow, by reason perhaps of change in the configuration of the country. In California and Australia many of these ancient gold-bearing river-beds have, at a period not long distant, been deluged and covered by lava, and the gold is extracted by tunnelling beneath the lava-sheet or by shafting down through it to the gravel below. These are called deep leads, whilst the ordinary uncovered gravels are called " shallow placers."

Almost anywhere along ancient or modern water courses not far from mountains, a prospector by panning can get colors of gold even on the pebbly " wash" covering the surfaces of large portions of our plains, or even on the tops of table lands that once were plains, over which broad rivers and glaciers and large bodies of water distributed their debris, but as a rule it will only pay to work where the "wash" or "drift" or "alluvial" matter is plentiful and thick, and more than this, only where water is accessible to the work.

Prospecting,

A prospector hunting for a gold placer follows up the water channels in which he finds specimens of all the rocks in the neighborhood. In Australia, the prospector looks amongst these to find samples of granitic, porphyritic and quartzose rocks or clay-slate as likely signs, and also pieces of quartz honey-combed and rusty, which we have described

before as " float or blossom." Plenty of broken up quartz he considers a good sign, but very pure, hard, dull white quartz is generally considered as " hungry" or " barren;" the size of the fragments denotes his nearness or otherwise to the reef, #.¢., the vein.

A prospector examines ciosely the fine sandy matter of the stream bed, especially where eddies and backwater have been formed. A likely deposit should be scraped up, even down into every crevice and depression in the bed rock or solid rock bottom over which the river, modern or ancient, has worn its channel. This material should be panned. Gold, too, is often found on points and slopes of the bed rock as well as in the deepest portion. Nuggets

PLATE LXVI. Shallow Placer—Gold Sand in Potholes A, A and Below a Hard "Bar ' B.

found on high reefs above the level of the stream, imply that their weight enabled them to remain in their position, during the deeper erosion of the neighboring streams, and that the original vein from which they came is not far off. Asa rule, large nuggets and coarse gold are found much nearer to the source whence they came, than fine or "flour" gold, which is often carried to unlimited distances away out on the plains.

The character of quartz veins and of their enclosing rocks in the immediate vicinity, decides the character, too, of gravels derived from them, hence sometimes a peculiar pebble may be traced up to the peculiar rock whence it came, and the gold vein be found near it in place.

It has been observed that "leads" following the course

co

or lines of a gold-bearing reef, maintain a more continuous yield than those crossing a number of gold reefs at intervals.

Gold occurs in pockets and "shoots" at intervals, with barren portions between, which accounts for what we have stated above. In a country where the gold quartz veins are small, though rich at wide intervals, the gravels will also be small.

In very deep ground where the " wash" is very heavy a series of borings or even shafts are made to test the quality of the bank. The following points have been observed as worthy of note in prospecting for gold placers.

1. Streams crossing the lamina or stratification planes of gold reefs at right angles are likely to be richest.

2. Gold is rarely found plentiful where there are indications that the current was strong, but rather in the lee under projecting points of rock, where beaches are usually formed and the water was slack.

3. Goldin streams is deposited in crevices of the " bed tock," which should be laid as dry as possible and picked up to such depths as the sand descends between the laminations.

4. Terraces are shelf-like excavations and deposits upon hill slopes above valleys, and are the remains of old glacier or river beds. The prospector should discover the inlet and outlet of the terrace and examine the gravel. The "wash" sometimes contains gold in layers one above the other.

5. Whilst working up stream attention should be paid to the banks on each side where sections are exposed so that no outcropping vein be overlooked.

6. Alluvial gold should if possible be traced to its source whence the "float" came. When the gold is large and plentiful and the boulders large and angular the reef is likely not far distant.

7. Sometimes there isa distinct peculiar feature in all the veins of a district, such as a peculiar band of a definite color.

8. Coarse alluvial gold is not always incompatible with fine reef gold as a source, because the reef gold may be so fine in general as to lend itself to very wide distribution when once it is liberated, while the rarer coarse grains would not be transported far.

g. Alluvial placers are richest where the current of the stream is interrupted by diminution in fall, by sudden change of direction, or by entrance of a tributary, also by reefs, bars, eddies, etc. Absolute richness depends upon local circumstances and the size and weight of floated masses.

PLATE LXVII. Shallow Placer--Gold Sand Behind Bar on One Side of Creek.

10, Creases, holes and fissures of bed-rock over which the stream passed are favorite places.

11, The lowest layers of each separate period of deposition are the richest.

Sometimes several different periods of deposition have succeeded each other.

12, The courses of present streams and of ancient channels are placers.

" LOAMING" is a form of prospecting. It is preliminary to such prospecting as cutting experimental trenches, or sinking trial shafts or boring. It consists in washing surface prospects from the bases and slopes of the ranges, until specks of gold, or specimens are found to be obtainable with tolerable frequency, within certain limits. The prospector then proceeds to trace the gold up hill to its source, narrowing the limits of his work as by patient search he approaches the vein, whence the gold has been derived. When he can obtain surface prospects of gold up to acertain point, or line, but no farther, he then proceeds by means of trenching to search for the gold vein. The prospector has often to work along a steep scrubby mountain side, selecting his prospects, numbering them,

ame 9 APMIS NSH a ott a ral

ab nea Ao ins Ne CA ASLRINhha ndcSimctne tan,

A ah lade

and placing samples in iis "loam bag." If he discovers prospects of gold, he finds his way back to the spots the samples were taken from, so as to continue his up-hill search, and trace the gold to its source or vein. Sometimes there is no indication of a vein, soil and bushes and debris covering its out-crop, but by loaming, the prospector ascertains its position, so as to expose it by a trench not many feet in length.

We remember an ingenious way in which a valuable and long sought for vein was at last discovered. Prospectors had long found very rich " float" at the base of a hill whose surface was so deeply covered with loose debris that no trace of the vein could be found. prospector found a small lake on top of this hill, and conceived the idea of cutting a trench from this body of water to the edge of the hill, and by damming up the trench, and then suddenly letting out the water to full force, it cut a deep trench through the loose debris down to bed rock and the vein was discovered. This process is called " booming."

The cleavage of quartz is said to be freer, sharper and better defined, in gold-bearing quartz than in that which is barren. Pyrite isa good indication. A soft, fatty clay or gouge often flanks the vein in its gold-bearing portions.

The mountain spurs should first receive attention for veins; if the quartz is hard, it stands up, if soft, as it more commonly is, it will leave a streak-like depression. On finding such, the prospector should first wash out some of the decaying rock. If only a trace of gold is found in the quartz, there is probably a gold vein in the neighborhood, and trenches should be dug and exploration systematically followed up. Gold is generally near one wall of a vein, seldom all through the stone. Quartz gold occurs in "shoots" with barren spaces.

Before setting a valuation on a discovery, the facilities for working the mine, such as we have alluded to, should be considered. Placer mines as well as other mines are often supposed to be " worked out." These are sometimes well worth investigating and examining by cross-cuts or other means. Sometimes it happens that more gold is obtained from "leader" veins that had been overlooked, than from the main worked vein.

Quite commonly, especially in the lower part of a placer,

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the pebbles and sand are firmly cemented together into a coarse conglomerate by infiltration of iron oxide and clay. This may consolidate into a false-bottom and not be true "bed rock." Generally two or three such false-bottoms, with intervening strata of greater richness, alternate with barren ones. So, many old diggings, thus supposed to have been exhausted, may be worked again, the true bottom not having been reached. These conglomerate bottoms may lie just upon bed-rock, with a white clay rich in gold beneath them. Gold occurs also in the conglomerate and must be stamped out.

Modern rivers frequently cross in their course old river courses, and redistribute their golden sands.

Placers are richer in their richer parts, thaa the veins from which their gold was derived.

When shallow placers are due to the wearing down of quartz veins, no placer will be found above these veins, or above the point where the vein crosses the placer. In the Sierra Nevada there is but little alluvium, the gold comes from veins near by.

Gold placers may sometimes occur below silver mines. Thus the Comstock vein was discovered by following up placer gold to its source. This vein has produced a goldbearing silver-ore, the silver rapidly disappearing and leaving the gold behind.

Example Of A Placer.

In Ballarat, Australia, the " wash-dirt" runs in a series of "leads" of varying width, starting from the same pvini, and trending in different directions towards the "deep leads." The "reef wash" is about 100 feet deep, the "pay dirt" 5 feet. The barren drift wash overlying the "pay dirt' is of black clay. The reef itself is of green slate, the bedrock is sandstone. Gold lies sometimes on thin layers of sand or " pipe clay" on the surface of the " bed-rock," more often in crevices of the bed-rock itself, which is more or iess rotten. This bed-rock is broken up for some 12 to 20 inches and the gold is found in " pot-holes" in it 15 to 18 inches in diameter and 6 to 1o, inches deep, cut out of the solid rock. The alluvial gold is found chiefly in bed-rock of slate, dipping 90 degrees. Some of these slates are soft and rotten, others are indurated. On the soft rock only is

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the gold found. Nuggets are found in the soft clay lying on "bed-rock." Slate forms natural "riffles" for catching the gold.

Deep pools under waterfalls in gold-bearing streams tarely carry much gold. So in rivers, gold is found in "liars" or points rather than in deep pools o7 bends.

Chapter X. "Deep Leads,"

A "deep lead" lies deep below the surface, often covered by beds of lava, especially in California. These lava beds may be many in number, and hundreds of feet in thickness. The "deep lead" is an ancient river bed.

In the Sierra Nevada the gold is derived from metamorphic crystalline rocks of the range, partly from quartz veins in the slates, and partly from gold distributed in minute quantities all through the metamorphic rocks. The quartz veins lie between the planes of stratification of the slates, also in irregular bunches and lenticular masses of limited extent. In many localities, the rocks are penetrated in every direction by little irregular quartz veinlets, which often carry gold, and in spots are extremely rich, even where the quartz vein is only an inch thick. In some California districts, wherever a basalt capping exists, the drift beneath it is auriferous.

In California the modes of occurrence of auriferous gravel deposits are various.

" Sometimes they exist in well-defined ancient river-beds under a capping of basalt which has filled the channels of the rivers in past ages. Again, they appear in isolated mounds or hillocks, evidently the reinains of such channels, which, being unprotected by a covering of lava, have been broken up by the action of the elements, also in basins or flats have received the wash of these disintegrating rivers, also in low, rolling hills near the base of the Siertas, and beyond the reach of the lava-flows." One of the most remarkable and important gold leads is that beneath Table Mountain in Tuolumne County. "The waters percolating through these lava-flows and reaching the gravels

beneath, are charged with alkali from the lava. These alkaline waters are charged with silica in solution from the same source. Hence the fossil drift-wood of these ancient rivers has all been silicified by these silicious waters. The gravels are also cemented by the same material. These percolating waters also contained iron, for iron pyrites is found in contact with the silicified woods. In this iron-cement, gold is found in rounded grains and in minute crystals, and threads deposited by a solution of sulphate of iron at the moment of the reduction of the latter to a sulphide."

Pirate LXVIII.

Deep Placer, T'able Mountain, Cal.—A A, Ancient River Channel, with Gold-bearing Gravel ; B B, Sandstones and Shales with Fossil Bones and Silicified Wood.

The dead rivers of California are on the west slopes of the Sierra Nevada, from 500 to 7,000 feet above sea-level. The largest and richest lead is the " Big Blue Lead," traced 65 miles and even 110 miles. It is parallel with the main divide of the Sierra Nevada. The live modern rivers run at right angles to it, cutting canyons 1,500 to 3,000 feet deep. The " Blue Lead" runs across these ridges from 200 to 1,000 feet below theirsummit. The lead was discovered by following up surface washings. Miners found that the modern streams were richly gold-bearing up to a certain

oint, increasing as this point was neared but ceasing when it was passed. These parts were in the line of the different streams, and by following up indications, the lead was eventually struck on several sections and tunnelled on. The deposit is 300 feet deep, composed of gravel, boulders, clay, and sand, on strata distinguished by degrees of fineness

, by the character of the rocks, and the amount of gold, also by colors, the prevailing color being a blue-gray. Gold is coarser near the bottom, and contains a greater alloy of silver. The silver in the gold in the upper strata has been eaten out by sulphurous acid resulting from decomposition of iron pyrites. The whole deposit is like that in existing rivers, showing banks, bars, eddies, falls, rapids and riffles. Thereis much gold in the eddies, and but little in the rapids. The space between the boulders is filled with sand and contains gold, the bed-rock is slate.

Where dead-rivers meet, the " wash" is generally rich. Where a lead becomes very narrow, dips fast, and is inclosed between steep walls, the gold will be very sparingly distributed in holes and behind ridges and will be coarse in size.

Very large and abundant boulders in gold-bearing stream beds are often a serious obstacle in getting out the gold, from the difficulty of handling them. Morethan one placer has been abandoned from this cause alone.

Hydraulics.

Placer banks are worked on a large scale by " Giant nozzles' or Hydraulics. Before commencing such work the total depth of the placer deposit should be examined and ascertained, and the richness of the strata throughout tested. Shafts should be sunk here and there to bed-rock for this purpose, and topograhical surveys made to ascertain what fall and head of water can be obtained, and what outlet also for the tailings, as the latter would soon choke up the work; the ground sometimes may be too flat to dispose of the tailings by stream-power. The choking of outlets is a fertile source of abandoning placers.

Beach Mining.—' The beach sands of the Pacific and elsewhere contain minute scales of gold and sometitines platinum, together with a great deal of magnetic iron ore. Winds, tides, and surf act as natural concentrators or separators in parting the light and useless material from the heavier. Wind drives heavy swells on the beach at high tide together with sandy matter. At ebb of tide, the surf lashes the beach and carries back light portions of the mass with the undertow, leaving some iron sand, gold and plati-

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num, whose weight enables them to hold their place. At low water, miners go down on the beach, scrape up the iron sand, which is generally left in thin layers, stacking it back from reach of the surf, and subsequently washing out the gold." In some beaches much of this sand contains titaniferous iron ore, and if attempts are made to use certain processes to save the finer gold the character of the iron may be a formidable obstacle.

Example Of Colorado Placer Gold Mines.

California gulch, the site of the present Leadville, furnished 4 great amount of gold in the early days till the discovery of the lead-silver deposits in place. This discovery, also, was due to placer mining. Whilst examining the gravel in the gulch, Mr. Wood, an intelligent prospector, was struck by the appearance of what the miners called "heavy rock," some of which he assayed. His specimens yielded 27 per cent. lead and 15 ounces silver to the ton. He put prospectors to work to find the croppings of the ore deposits, and in June, 1874, the first "carbonates in place" were found on Dome Hill. This was practically the beginning of Leadville. It is said that upwards of 2,000,000 dollars worth of gold was taken out of this gulch in one summer before the mines in place were discovered or opened up.

It is noticeable that California gulch alone furnished almost all this placer gold, whilst Iowa and Evans gulches adjoining it on either side and carved out of the same series of rocks, yielded little or nothing. Why should the smaller gulch contain exceptionally rich gravels and its neighbors be barren?

The richest portions of California gulch were found at bends in the course of the gulch. In one place near Oro in the narrow bed of'the gulch, a gold-bearing cement was found containing hydrated oxide of iron, below the gravel, yielding an ounce of gold to the ton. The gulch-gold was worth $19 per ounce whilst that from the mines in place only $15. The Printer Boy porphyry containing actual gold veins in place may have been the source of some of the gold in the gravels, together with the oxide of iron resulting from the decomposition of pyrites in the pyritiferous porphyry asa cementing material. Alsothe Weber-grit

" sandstones at the head of the gulch have been found to carry small gold veins, and from their abrasion also gold-bearing gravels would have been carried down the gulch. Also of late the rich gold deposits of Breece Hill at the Ibex and Little Johnnie mines have been found.

"Tt is doubtful," says Mr. Emmons, " whether in general, all or even the greater part of the gold contained in placer gravels is derived from the abrasion of actual gold veins. Traces of gold may be found in a very large proportion of the massive rocks which form the earth's crust. Gold veins are concentrations of this mineral in sufficient quantity to attract attention and yield a profit. But doubtless there are a vast amount of smaller concentrations which may escape notice. As the rock disintegrates and is worn away by atmospheric agencies, the gold from these smaller deposits

as well as from the larger is set free from its inclos- ,

ing rock and subjected to the concentrating action of mountain streams.

" Placer deposits are the results of nature's vast sluicing processes. To bring them into the condition in which they may be made available by man, requires not only the goldbearing rock, which her agencies may grind up into sand and gravel, but the sifting power of rapid streams, which may carry down the lighter and coarser material, and a suitable channel in which the heavier particles may lodge, as in the rifles of a sluice box. All mountain gravels, all sands of rivers coming from the mountains, contain a certain amount of gold, but it is only under peculiarly favorable conditions that the gold is so concentrated as to tender the gravel remunerative.

" Among the most favorable of these conditions is a comparatively narrow channel having a hard and compact bedrock, and ridges or bends in its course, which by causing a partial arrest in the rapidity of the current shall allow the heavier particles of gold to settle to the bottom, and hold them there when once they have settled.

"From this point of view there is a very evident reason why California gulch should have furnished rich placers, and why the gold which may exist in Iowa and Evans gulches should not yet have been extracted even though the detrital material which has been carried down the gulch should originally have been equally rich in gold.

"California guich is a valley of erosion, formed entire] by the action of running water, and since the glacial period. It has therefore a bottom or bed of hard rock. Its transverse section is V shaped and therefore favorable for the concentration of heavy particles at its bottom. When comaratively

full of water, its numerous bends formed eddies in the down-flowing currents, and allowed a longer time at these points for the settling of the surface particles, and as it cuts across many different formations in its course, its bed must have transverse ridges, which have caught some of the gold and prevented it from being carried farther down the stream.

"Evans and Iowa gulches on the other hand are glaciercarved valleys. Their courses are straight, their bottoms broad and comparatively smooth. The glacial moraine material with which they are largely filled has not been subjected to the sifting or jigging process to which gravel is subjected in the bed of a stream. The lower part of their present beds is cut, not out of rock, but out of the loose gravelly formation of the 'Lake beds.' This later bed, along which the material brought down by post-glacial erosion has been carried, has not a sufficiently hard and permanent bed-rock to allow of the concentration of gold on its surface." :

A. .A And Fairplay Placers, South Park.

Along the banks of the Platte river are enormous masses of glacial morainal matter consisting of boulders and sand brought down partly and principally from Mount Lincoln and receiving contributions from side glaciers of the Mosquito range. This material forms undulating banks on either side of the river. This placer "wash," from 50 to 100 feet thick, is worked for gold principally at Alma and Fairplay.

At Alma the heavy bank of " wash" is mined by the giant nozzle. The banks are also cut back into blocks of ground, by water from a flume, which is let out at intervals along the bank above; at each place it cuts a narrow ravine in the loose debris and at the same time makes the banks easier to be attacked by the water of the giant nozzles, which rapidly undermine them. The water and sand from

these streams run down into the sluices, whose bottoms are paved with discs of wood, forming " riffles" to catch the gold, whilst the lighter sand is carried onward by the stream. Intheir "clean up" in the stream bed, they not only wash down to bed-rock, but after hunting with their knives in every crack and crevice of the latter, they dig it up for a foot or two, and further examine it. The rock is a jointed sandstone.

Quicksilver is thrown into the sluices, to collect the finer gold which is afterwards retorted. Whilst gold is found all through this bank of " wash" from " grass roots" down to bed-rock, the greatest quantity of gold and largest nuggets are found at " bed-rock" or in its interstices.

The source of some of this gold may be a series of large, but not very productive quartz veins in granite, near Mount Lincoln, whence the main glacier originated. It is also probable that a good deal of the gold came, as said before, from the breaking up of the various rocks in which it was disseminated, more especially the porphyries and crystalline rocks.

In the winter, owing to freezing of the water supply, the work has to be discontinued till the following spring.

Chapter Xi.

Mining Regions Showing Examples Of Ore Deposits.

Fissure Veins In Granitic Rocks.

Having described in previous chapters the nature of veins, ore deposits, etc., and how to prospect them, it will be of interest as well as profit to the prospector, to learn something of the mines and mining regions themselves. For this purpose we propose giving a sketch of some of the leading mining regions of Colorado and the West, as instructive illustrations and examples of what we have written in previous chapters. As we said in our advice as to the education of a prospector, the best education for him is to go to, and spend as much time as he can in, the mines and mining regions themselves.

We will take first the regions characterized by Assure veins. These veins are in the granitic andig:ieous districts of Colorado. In the granitic ranges, the mining districts of Boulder county, Gilpin and Clear Creek, are the most noted, the bani a mining towns being Boulder, Jimtown, Georgetown, and Central and Idaho Springs.

Boulder Mines,

The geological features of Boulder consist in a series of ridges or hogbacks rising up from the prairie and flanking the granite mountains. These represent Mesozoic strata consisting of sandstones, limestones and shales, containing beds of coal and other economic products, but no precious metal. Volcanic action has occurred in their vicinity as shown by a large dyke of basalt at Valmont. These hogbacks, so universally present, flanking the granite mountains, are, in Colorado, destitute of precious ores. Inside of and west of these is the Archean granitic front range, consisting of heavily bedded granite-gneiss, profusely traversed by veins of " pegmatite" or very coarse sparry granite, consisting of white feldspar and quartz, with very little mica, and from a few inches to 4o or 50 feet in width; with these also occur some dykes of eruptive rock, some of it a dark black rock like basalt, called "diabase"; others are lighter colored quartz porphyries and diorites. In the telluride belt, whilst pegmatite veins are abundant, eruptive rocks are scarce, but west of the telluride belt, which is more or less confined to a special area underlying the Magnolia, Sugar Loaf, Gold Hill and Central districts, enormous masses of eruptive rock are foun'. but no tellurides. In the non-telluride districts, such as Caribou, Ward and Jimtown, rich silver ores are found associated with galena, gray copper, etc., and gold ores associated with copper and iron pyrites. Thus there are two or three distinct belts in the region, a telluride gold belt, and a silver belt, and a gold pyrites belt. It is noticed that the entire region has been locally disturbed by volcanic forces, and volcanic rocks abound; outside of this disturbed region there are no mines for a long distance.

The Boulder mines are celebrated for the occurrence of telluride minerals, some of the richest and rarest ores occurring

in nature. These ores are confined toa belt occupying the eastern part of the district, and nearer to the hogback region of the plains than any other important ore deposits in Colorado.

West of this belt in the Caribou district the ores are argentiferous galena, with brittle silver. In the Ward district pyrites abound, and where it is decomposed the gold is free. The pyrites though gold-bearing are difficult of reduction.

The peginatite veins containing the ore stand ata high angle and are often very wide, but the rich ores, especially the tellurides, are concentrated in thin streaks and not very continuous bodies. The gangue or vein material is simply an alteration of the adjacent granite, or gneissic country rock, into a more sparry, larger crystalline form, consisting of quartz feldspar and some mica, This is impregnated with rich mineral whose source is probably not far to find, the metal elements being microscopically or chemically diffused through the mineral elements composing the adjacent country rock, which is sometimes porphyry, and at others gneiss. This impregnation has taken place either along the contact of an eruptive rock with the country rock granite, or else in a pre-existing vein of pegmatite, or along some fault cr jointing plane in the country rock itself which has been favorable to the concentration and precipitation of metallic minerals from their solutions. The direction of the veins is generally between northeast and northwest, or east and west; their dips are steep or vertical.

The quartz of the pegmatite gangue, when impregnated with telluride ore, has a pale, bluish-gray and rather greasy appearance, streaked here and there witha dull blackish, greasy stain, upon which sometimes the true telluride minerals, such as sylvanite, can be seen, generally in long thin crystals of a bright tin-like appearance. It is sometimes called graphic tellurium, because the crystals crossing one another assume the form of Hebrew characters. Sylvanite is a telluride of silver and gold. There are many varieties of tellurides, some rich in silver and others in gold, and some with both combined. When a piece of gangue containing tellurium is roasted, the gold comes out in good sized globules on the surface.

Two g. gat nother-veins, called the Maxwell and Hoosier veins, traverse the telluride district for several miles, easily traceable by their rusty color. One carries pyrites and tellurides, the other silver ore and gray copper. Gold Hill district, in the telluride belt, is traversed by the Hoosier yangue. Several veins cross the Hoosier gangue and are richer in its vicinity; in some, the ore is a telluride at the surface, but with depth passes down into gold-bearing pyrites.

The Ward district outside the telluride belt carries copper and iron pyrites bearing gold. Caribou is silver-bearing ; its ores are galena, copper pyrites and zinc-blende occurring in gneiss near a dyke of eruptive diabase. The No- Name vein crosses and faults the Caribou vein. Its ores carry both silver and gold; the ores are silver glance, brittle silver, gray copper, galena, copper pyrites, with native and zuby silver. The copper pyrites carries more gold than silver.

The granitic rocks near Boulder are thrown into a series of parallel folds, one series cut diagonally by another. The telluride veins run along the slopes of these folds. The veins are in cracks and fissures coinciding with this folding, some of the main fissures being filled at once by porphyry dykes, the others more gradually by vein material. The veins occur along, on, and near these dykes, along lines at the junction of the more massive granite with the bedded gneiss, along and between stratification planes of schist, and along the joint planes of granite. The veins are due to percolating alkaline waters dissolving metalliferous material and veinstone from the surrounding rocks. It is noteworthy that alkaline springs still exist in the neighborhood, as they do also at the mining district of Idaho Springs. The veins occur where the foldings are abrupt, and the direction of the veins is parallel to the strike of the stratification. Asarule the veins are not of great extent. A single vein can rarely be traced on the surface or beneath it for more than 600 feet. Before that distance is reached, the vein spurs off again into another.

Where veins cross at a small angle or where a spur branches off from the main vein, accumulation and enrichment of ore takes place. There are two courses of veins, one east and west, the other northeast by southwest; the

former system appears to be the older, as the latter faults it.

The ore occurs in chimneys or pockets, with a good deal of barren ground between.

Small veins run parallel with each other for some distance, the interval filled with granite or pegmatite. Sometimes a vein pinches out entirely (contrary to the general habit of true large fissure veins occupying great fault fissures). The ore streak is from 1 to 20 inches wide containing more of this blue, greasy, fine-grained "horn quartz" than the country rock. Some of the veins interlace like arteries in a human body. Minute particles of pyrites (marcasite) often produce the dark stains we have noted on the telluride quartz. By moistening the stone, the telluride minerals and pyrite appear distinctly.

A Typical Boulder County Mine.

A good typical and very instructive example of a contact fissure, gold-bearing vein is that of the Golden Age at Jimtown, north of Boulder.

" At Jimtown a quartz-diorite dyke occurs, of light color containing much hornblende and titanic iron, running nearly through the street of the village. The cliffs at Jimtown, over 500 feet high, are of quartz porphyry, of white color, consisting mainly of large crystals of quartz and feldspar, set in a fine grained crystalline ground mass or paste."

Golden Age And Sentinel Veins.

From the town, the road winds up a steep mountain composed of coarse gray granite, with occasional belts of gneiss. Here are located the Golden Age and Sentinel mines.

The Golden Age covers the outcrop of a quartz-porphyry dyke cutting through the granite. This dyke varies in width, from a few feet to about fifty. The outcrop of the main ore chute of the Golden Age extends along the " contact" on the lower side of the porphyry dyke. Ata depth of 100 feet the main shaft discloses a split in the vein. The hanging wall of the vein continues into the dyke, but with porphyry hanging and footwalls, until a depth of 330 feet, where it enters the upper contact between the porphyry and

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granite. The dyke has been much acted upon and decomposed by vein-forming agencies in the upper workings, but in the lower it is less decomposed and shows considerable pyrites. The Golden Age veins are well defined, presenting a banded or ribbon structure. They are inclosed in distinct walls with gouge or selvages, which at times show slickensides. The seams and feeders that have enriched both veins come in from the porphyry dyke.

The ore from the Golden Age contains rich and magnificent specimens of free gold. Itisafree milling ore. When rich, the gangue is a hard, flinty, vitreous white quartz. The gold is seldom accompanied by pyrites. It is generally imbedded in the white quartz as bright, yellow gold, in size, from coarse grains to nuggets several ounces in weight; after it reaches the lower contact between the porphyry and granite and enters the granite, there is an increase in the baser metals, such as zinc-blende, galena and pyrites, but the ore still retains its value in free gold.

Returning to the surface, the Sentinel location covers the apex of a vein, which there appears enclosed in a belt of schistose or gneissic rock.

This vein dips south at an angle of 70° and passes through the Golden Age vein on its course.

The Sentinel vein ore is entirely distinct from that of the Golden Age. It is the characteristic bluish horn quartz of the tellurium veins of Boulder County, with characteristic chalcedony quartz crystals and finely disseminated pyrites. The value is in metallic gold and such tellurium ores as petzite and sylvanite. Whilst most of the gold was deposited as native gold, a portion has evidently been rendered free by partial decomposition of the tellurides. This ore is very rich. The richest ore usually occurs in two narrow seams or streaks from a foot to ten feet apart, the intervening space being more or less mineralized country rock. It is richest when in the schistose rock, and poorest when it passes through the porphyry dyke. The crossing of the Sentinel vein through that of the Golden Age is very clearly marked; it very slightly faults the Golden Age vein.

The gold mines of Boulder Count belong to two distinct periods of vein formation; to one belong the nontelluride ores, and to the other those producing tellurium. The tellurium veins appear to be the later of the two.

The ores of the Sentinel tellurium vein are lower grade where the vein passes through the porphyry dyke. This is due to the Golden Age vein being formed first, and draining the dyke of its disseminated mineral values. The Sentinel received its mineral from the schistose or gneissic rocks, and is consequently richer where enclosed in those rocks than when in the dyke.

Prospectors look for richer or larger bodies of ore when veins unite or cross each other. In the Golden Age the two veins unite about 100 feet below the surface. There are similar veins of the same age, and large and rich ore bodies are found at their junction. On the other hand, the Sentinel vein of later age, passing through the earlier

PLaTE LXIX.'

Section of Golden Age Vein, Jimtown, Boulder Co., Colo.

Golden Age vein, produced no enrichment of the ore bodies, Tc form such ore bodies, the veins should be of contemporaneous origin.

The ore deposits of Gilpin and Clear Creek counties are very similar to those of Boulder, only they do not produce tellurium ores. The country rock is the same granitegneiss, penetrated here and there by porphyry dykes. The pegmatitic veins are either in the gneiss or between the dykes and the granite. In some cases the porphyry dyke constitutes a vein in itself, such as the Minnie, which

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is a felsite porphyry. and the Cyclops, a quartz porphyry. In Gilpin County, around Central City, the ores are a mixture of copper pyrite and iron pyrite with a very little galena and zinc-blende. All are gold-bearing.

The richer ore occurs in streaks not over a foot wide, in a compact, fine-grained mass of pyrite. Copper pyrite is richer than iron pyrite. The rest of the vein, often many feet wide, carries pyrite irregularly disseminated through decomposed country rock. The bulkof these ores are difficult to treat, and are milled, the loss being 4o per cent. higher in the unoxidized ores than in the oxidized. The veins follow the cleavage planes of the gneiss, cutting the stratification planes at right angles with a vertical dip. The porphyry dykes are older than the veins, as the cleavage planes intersect both the porphyry and gneiss alike. For an interval of 20 miles between these mining districts and the plains, there are no ore deposits of any importance known.

In Clear Creek County the ores are mainly silver-bearing ; the silver is derived mainly from galena and gray copper. Dykes of obsidian occur in one of the mines parallel with the vein, which is itself a porphyry dyke. The richest mineral is close to the obsidian dyke.

Fissure Veins In True Igneous Rocks,

Whilst most of our fissure veins and ore deposits generally are more or less associated with the presence of igneous rocks, there are some which are essentially zz igneous eruptive rocks alone.

The most remarkable of these are the fissure veins of the San Juan region in southwestern Colorado.

This region consists of an enormous plateau of lavas of great thickness resting upon and originally overflowing a low mountain range or plateau of granitic and upturned sedimentary rocks, the latter representing most of the geologic periods from Cambrian to Tertiary. The thickness of these great lava flows, which were erupted about the Eocene period of the Tertiary, is upwards of 1,500 feet; this lava mass has been cut up by glacial and river action by profound canyons, into a rugged mountain range, the summits of some of the: castellated mountains reaching a

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height of 14,000 feet above the sea. The lava sheets are also traversed to a depth of 1,500 feet, more or less, by an extraordinary number of great quartz-fissure veins. These veins appear to fill shrinkage cracks resulting from the contraction on cooling of the lava sheets; strictly speaking they are rather "gash veins" on a larger scale than " true fissure veins," for they are mostly /imuited to the thickness of the lava overflows and cease when they reach the underlying granite.

There appear to have been two principal eruptions; the first, during the early part of the Tertiary, covered the higher region of the San Juan mountains to a depth of 1,500 feet with an overflow of brecciated andesitic lava, which on cooling developed fissures of contraction traversing the lava mass in all directions; these were subsequently and slowly filled with a hard bluish quartz containing more or less ore.

Following the first grand overflow were others of less magnitude, consisting of non-brecciated andesitesandrhyolites. Thissecond dynamic movement produced locally, fissures extending below the horizon of breccia into the stratified rocks. These, however, are seldom productive below the eruptive zone. There are also metal deposits in connection with still older eruptions of andesite and diorite, such as Mineral Farin, Calliope, etc.

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In the Red Mountain district the ore deposits form a nected irregular chambers, trending downward, probably

channels of ancient hot mineral springs.

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water completely silicified the surrounding eruptive rock for some distance away from the ore chambers. So the ore bodies are distributed through a huge irregular column of quartz extending to an undetermined depth.

Large masses of brilliantly colored material are conspicuous in this region. They have been acted upon by mineral waters circulating through their crannies and fissures. Ore bodies are occasionally found in these, and such mines are locally known as cave mines.

The ores of the San Juan are mostly argentiferous gray copper, copper pyrites and galena associated with zincblende and iron pyrites in usually hard horn-quartz matrix. Some of the ore locally contains a high percentage of bismuth; others produce pyrargyrite and polybasite, rich silver minerals; others carry considerable gold, such as the recently discovered gold belt at Ouray. This belt occurs in Dakotah Cretaceous sandstone, which has been altered into a quartzite by the intrusion of dykes and sheets of eruptive diorite. One of these sheets spreads out in the quartzite. The ore occurs at the top of the quartzite, at its junction with a bed of shale. The gold, which is free and enclosed in brown oxide of iron, doubtless originated from the porphyry, and entered the joints and bedding planes of the quartzite, where they were opened by faulting. Above the shale the ore does not penetrate, the shale acting as an impervious resistance to uprising solutions. Ore bodies also occur in the Jurassic limestones below the quartzite, especially where they are penetrated by eruptive rocks.

In the eastern portion of the San Juan region some important gold deposits occur near Del Norte in the Little Annie or Bowen Mine, which appear to be a decomposed dyke of eruptive rock, containing free gold in brown iron, in the upper portion, and with depth iron pyrites also goldbearing.

Creede,

At the newly discovered camp of Creede, not very far from Del Norte, the fissure veins are very similar in character to those elsewhere in San Juan; they are quartz fissure veins traversing andesitic breccia and other volcanic rocks. The gangue matter in these veins is exceedingly rich in silver-bearing ore, so much so that the amethystine

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quartz composing the gangue or veinstone is quite in a minority to the ore, and the vein may be said to be nearly a mass of ore from wall to wall. The thick lavas of Creede rest doubtless with depth upon Carboniferous limestone or else on bare granite; the former is found outcropping at some distance from Creede, from beneath the lava overflow, and being penetrated by intrusive eruptive rocks shows signs here and there of productive ore deposits similar probably to those at Leadville. Creede is an encouraging example to a prospector, that all productive veins in Colorado have not been discovered yet, even in districts that have been pretty well tramped over. Creede had doubtless often been more or less walked over by prospectors for years before the great discovery was made, and in a year's time we may hear of several more similar discoveries in the great San Juan.

Rosita And Silver Cliff.

The next important and peculiar igneous district carrying fissure veins is that of Rosita and Silver Cliff in the Wet Mountain Valley near the edge of the prairie country in southeastern Colorado. Here a local eruption of considerable power and magnitude and of comparatively recent date has occurred. These eruptions, consisting of andesitic, rhyolitic and trachytic material have built up cones and rounded hills largely of fragmental material such as consolidated tuffs, ashes, and breccia, all of which, as at Cripple Creek, rest on granitic basement rock. From the fragmentary character of the rocks it is evident that most of the eruptions were explosive, alternating, however, with quieter flows; in some cases the dykes can be seen, where some of the lava came, at others the "necks "or throats of the volcanoes themselves filled up with volcanic boulders; of such is the celebrated Bassick Mine. 'The mine is in the throat of an old crater cf andesite, filled with boulders of granite and andesite bedded in gravel and sand. The ore of the Bassick appears as concentric zones or shells around these boulders, as a replacement of the gravelly matrix. The entire mass has been permeated by heated waters which have decomposed the rocky fragments, depositing opaline quartz and kaolin in abundance.

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The concentric shells around the boulders carry alternately several minerals, such as galena, antimony, zincblende, copper and iron pyrites, all more or less goldbearing. The ore deposition in this region seems to have taken place at the close of the eruptive period, when the i eruptions were dying out into hot springs, fumaroles, etc., and producing great decomposition of the lava rocks. The district was not thought much of, until Mr. Bassick made his discovery in the unpromising-looking throat of the old volcano, containing a formation quite anomalous, and which the regular prospector, accustomed to true, orthodox lt fissure veins, would have passed by as very unlikely. So ' it may happen to future prospectors, that some very unlikely formations may turn out great riches; hence it is well to keep a sharp lookout for everything examinable.

A STUDY OF MODERN LIVING VOLCANOES TO UNDERSTAND i THE CRIPPLE CREEK VOLCANO, ir

t

By far the most typical, instructive and important gold camp in Colorado and the West is that of Cripple Creek.

Plate: Lxxii.

Stromboli Volcano.

To understand the geology of the Cripple Creek region and gold-bearing volcanic regions and rocks and their relations i to the ore-deposits, a knowledge of the phenomena attend- a ing modern volcanic eruptions is necessary. Let us take that of the living volcano of Strom*0li, described by Professor Judd, as throwing some light on the phenomena that

natin siemens

may have occurred many thousands of years ago in the now extinct volcano of the Cripple Creek district.

From a point on the sides of the mountain of Stromboli, masses of vapor issue and unite to form a cloud over the mountain. his cloud is made up of globular masses, each of which is the product of a distinct outburst of the volcanic forces. At night a glow of red light appears on the cloud, increasing gradually in intensity, and as gradually fading away.

After an interval this is repeated and continues till the light of dawn causes it to be no longer visible. When we land on the island we find it built up of the " ejecta" from the volcano like a gigantic iron furnace with its heaps of cinders and masses of slag. The irregular shape and surface of the land is due to erosion removing the loose materials at some points, and leaving the hard slaggy masses standing up prominently as dykes and hard portions of lava flows, as Pisgah, Rhyolite Mt. and others at Cripple Creek do, above the eroded and

Pirate LXXIII. more fragmentary Map of Island of Stromboli. Lt s and breccias.

is great heap of cinders and slags rises 6,000 feet above the sea bottom with a base four miles in diameter; 2,000 feet above sea level is a circular depression, tie crater of the active volcano.

Looking down into the crater an outburst takes places. Before the outburst, many light curling wreaths of vapor ascend from fissures on the sides and bottom of the crater. Possibly this is the origin of some of the dyke-filled fissures of Cripple Creek. Suddenly a sound is heard like a locomotive blowing off itssteam. A great volume of watery vapor is thrown up into the atmosphere, and with it a number of dark fragments are hurled 500 feet above the crater, some

er ce

nt SE I

falling on the mountain, others back into the crater with a loud rattling noise. Those rolling down the mountain are

PLaTE LXXIV.

Stromboli Crater.

still hot and semi-molten. This is a clue to the origin of the fragmentary materials composing the tuffs and breccias at Cripple Creek. The black slaggy bottom of the crater is, as we have said, traversed by many fissures emitting jets of vapor. Some of these are quite large and vary in size and number and position at different periods. From some, only steam is emitted in loud snorting puffs. In others molten material is seen welling up and flowing outside the crater. Such fissures when all eruption has ceased would Pirate LXXV. be found, as at Crip-

Dykes Cutting Beds of Scoria and Tuff in the ple Creek, sealed up

Wall of a Crater. A A P

with solid lava with

a lava flow on their tops. From this liquid mass, steam escapes in considerable quantities. Within the walls of the fissures, a viscid semi-liquid lava heaves up and

down and churns around till at last a gigantic bubble or blister is formed, which bursts violently and a great rush of steam takes place carrying fragments of the scum-like surface of the liquid high intotheair. At night the fissures glow with ruddy light. The liquid matter is white hot and the scum on it a dull red. Every time a bubble bursts fresh glowing surface is exposed. It is the reflection of this upon the clouds of steam above the mountain that causes the fitful glows of light we mentioned.

The phenomena show there are cracks communicating

with the earth's interior highly heated matter beneath the surface, together with great quantities of imprisoned water, which escaping as steam give rise to all the active phenomena, What is popularly supposed to be flame in an eruption is the reflection on the cloud of steam and dust, from glowing masses in the mouth of the crater. Sulphur is not, as commonly supposed, erupted from a volcano, but is formed by the union of sulphurous acid and sulphureted hydrogen issuing from volcanic vents.

A volcano is a steam vent, like a geyser, which may be called a water volcano.

Origin Of Fissures,

Some light is thrown on the possible origin of some of the Cripple Creek dykes and fissures by the eruption of Vesuvius in 1872. The bottom of the crater was entirely broken up and the sides of the mountain rent by fissures in all directions, So numerous were these fissures that liquid matter appeared to be oozing from every part of its surface and the mountain to be " sweating fire." One fissure was enormous, extending from the summit to far beyond the base of the cone. This, filled with a dyke of lava, is visible to-day. From both crater and fissures enormous volumes of steam rushed out with a prodigious roar. This roaring was from explosion of bubbles one after another, and the vapor cloud above Vesuvius, as at Stromboli, was made up of globular masses of steam ejected at successive explosions. Each explosion carried upward quantities of fragments which fell back on the mountain. All along the course of the stream of lava, volumes of steam were throwa off.

Origin Of Tuffs,

The discharge of such large quantities of steam causes the atmosphere to be saturated with watery ap which, condensing, falls in excessive rain storms. pro

Plan

ucing mud

@

PLatE LXXVI,

Plan and Cross-Section of the Roots ofaCrater. Black=Dykes Filling Fissures, z

streams formed by rain water Sweeping along the loose volcanic dust and debris. In some such way, doubtless, the Cripple Creek tuffs and breccias were formed,

Gases And Materials Ejected From Volcanoes.

The most abundant of the substances ejected from volcanoes is steam, and with it many volatile materials, such

ak a te ee ee

as hydrochloric acid and carbonic acid, also hydrogen, nitrogen and ammonia, and at Cripple Creek fluorine gas.

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Microscopic Structure of Some Crystals Showing Microlitesand Crystallites,

Plate Lxxvii,

These different gases at Cripple Creek had much to do with the formation of ore deposits. Volatile metals, such

as arsenic, antimony and cinnabar are erupted; these substances, issuing from volcanic vents at high temperature, react upon one another forming new compounds, such as sulphur. Hydrochloric acid unites with the iron in the rocks to form yellow ferric chloride, common at Cripple Creek, and looking like a greenish yellow sulphur. Acid gases change lime, alkaline and iron elements into sulphates, chlorides, carbonates and borates, which, when removed by rain, leave a white substance like chalk, composed of pure silica. Beds of such material occur not far from Cripple Creek and powdered silica in some of the mines.

The lips of fissures from which steam and gases issue are coated with yellow and red incrustations of sulphide and oxide of iron, such as are common in many prospect holes at Cripple Creek.

Solid materials are ejected in vast quantities; fragments of the rock masses through which the fissure is rent are carried upwards by the steam blast, together with other matter far beneath the surface in a semi-fluid condition. Hence it is that at Cripple Creek we occasionally find fragments of red granite imbedded in the volcanic breccia torn from the throat of the volcano in its passage through the underlying granite of the region.

Mineral And Chemical Elements Of Lavas,

Eight chemical elements make up the mass of lavas, oxygen, silicon, aluminum, magnesium, calcium, iron, sodium and potassium. Oxygen makes up the larger proportion, so that lavas are mostly oxides. Next is silicon and aluminum, giving the quartz and feldspar and silicate element.

Lavas are of two kinds, acidic and basic. Acid lavas contain eighty per cent. silica, basic forty-five per cent. The former are rich in potash and soda, the latter in lime and iron; the former are commonly light in color and weight, the latter dark andheavy. Rhyolite is an example of an acidic lava, basalt of a basic one. The andesites and phonolites of Cripple Creek are intermediate. The minerals composing these lavas are principally quartz and feldspar, together with the dark minerals, mica, augite, hornblende, olivine and magnetite.

Crystals And Microscopy Of Lava,

! Many lavas are of a glassy nature, others contain many

: crystals, some of large size.

Microscopic sections of lavas show them to be made up of a ground mass of a glassy character, with distinct crystals set in it like plums in a pudding.

In others, the crystals are so thick that the glassy base

4 can scarcely be seen.

Through the midst of the glass, cloudy matter is observed; a higher power shows this " nebula" to be composed of minute particles called crystallites, the embryonic forms of crystals. Sometimes we can see an attempt of these par-

Plate Lxxviii.

Minute Cavities Containing Liquids in the Crystals of Rock.

Al ticles to aggregate into a geometrical form, sketching out

the outline of the large crystal they intended to form, but

wee prevented from finishing, by the cooling of the glassy magma. These crystallites assume forms like ferns, hairs, spiders, etc.

1 ty In subterranean regions the conditions were particularly favorable for the development of crystals. The lavas cooled with extreme slowness, under enormous pressure, allowing plenty of time for the crystals to form.

Those lavas containing most soda and potash (acid lavas) if assume a glassy condition, and these have often cooled near the surface rapidly, the more crystalline varieties

slowly at great depth. Obsidian and rhyolites are glassy types, granite and some porphyries with large crystals are of the latter class, whilst andesite and phorolite may be intermediate. The latter, however, at Cripple Creek, may have cooled quickly near the surface, and the crystals are for the most part small.

Besides the natural imprisoned water, crystals in lavas are found microscopically to contain globules, sometimes filled with gas, salt, and water, which may add to the materials for the production of steam.

Eruptions Of Dust.

Steam escapes from lava so violently that the froth or scum, called scoria, is broken up and scattered in all directions. This scoria like pumice is full of little holes like a sponge, due to escape of the steam in it. Such spongy scoria is found scattered over the hills of Cripple Creek. During violent eruptions a continuous upward discharge of these fragments is maintained; the cindery masses hurtling one another in the air, fall back into the vent, or are scattered over the mountain. Being often shot up again and again from the vent, they are reduced to the finest impalpable dust. They fill the atmosphere to such an extent as to bring on an " Egyptian darkness." This dust, mingling with descending rain, forms destructive mud flows, and sets or consolidates into the tufas or tuffsso abundant at Cripple Creek. When larger angular fragments are caught up and consolidated with these, the rock so formed is a breccia, as already illustrated.

Volcanic craters, after having been formed, are liable to be disturbed by later eruptions. Thus the crater of Vesuvius was reduced 400 feet by a later eruption, the old crater blown up and a much vaster crater opened.

Cripple Creek also witnessed its second disturbance, after the andesitic eruption had ceased, by one of phonolite lava.

Fluidity And Other Properties Of Lavas,

Some lavas, such as basalt, are reduced to such a state of fluidity that their streams run like water to great distances. Others are of a more viscid, mortar-like consistence, especially

the acid lavas, such as those of Cripple Creek. These are apt to flow but a short distance from their source, and to build up big domes and thick masses; of such a nature seems the structure of Nipple Mountain, south of Cripple Creek.

The peculiar columnar structure often observed in basaltic lava sheets, and in a rough way developed in the phonolite of the cliff above Victor mine, is due to cooling and contraction somewhat in the same way as mud cracks are formed ina drying up pond. A biock of lava isolated by these cracks assumes a polygonal form like the basaltic columns of the Giants' Causeway.

During the cooling down of lava and the escape of steam and gases, deposits of sulphur, specular iron and (at Cripple Creek) fluorspar, are deposited. Specular or micaceous iron is not uncommon at Cripple Creek. Rock masses are completely disguised by these incrustations.

Stratification Of Tuffs,

Tuffs and breccias are often found stratified. The fragmentary materials in falling through the air are sorted, the finer particles being carried farther from the vent than the larger ones. Craters built up of tuffs and breccias fallen in the condition of a muddy paste, show very fine stratification.

Large cones are built up of uniformly spread layers of more or less finely divided material disposed in parallel succession. At Cripple Creek the bedding is indistinct, and often difficult to trace, the dip of stratification being still more compressed by the cross fracturing of the rocks; hence it is hard to tell whether the lines represent cross fracture cleavage, or bedding planes. In most volcanoes the stratified tuffs are cut and crossed, as at Cripple Creek, by numerous dykes running in various directions, cracks filled by lava from below. .

Movements, too, have taken place subsequent to the accumulation and consolidation of the whole material as shown in Plate LX XIX, whereby the inasses are faulted and fresh fissures opened in them. Faults are found in some of the mines at Cripple Creek, faulting not only the lavas, but the veins also. Cliff sections of volcanoes show alternate

beds of solid lava, scoria and tuff, representing different eruptions or flows.

There seems an order and succession in the eruption of the different varieties of lava. During the earlier periods rhyolites, andesites and phonolites are erupted, and later basalts. This appears to be the case in the volcanic region west of Cripple Creek around Mt. MacIntyre, Thirty-Nine Mile Mt., and Black Mt. The prevalence of basalt capping the other lavas in that region, together with the greater

TT Tae Os

see

a

PuaTE LXXIX.

Cliff Section, Composed of Alternate Beds of Lava and Scoria, ut by Lava Dykes, and Fau!ted.

freshness of the rocks, imply that its eruptions were somewhat later than those of Cripple Creek, where basalt is not found, and where the rocks are much decomposed.

Volcanic eruptions shift their centers from time to time, making new cones along a line of fissure (for volcanoes are built upon lines of fissure). See Plate LXXX. Extinct craters are frequently filled by beautiful deep lakes. Cones rise within cones, and within great crater rings. At each successive great eruption, the old cone is blown away, and a new one formed.

Hot springs contain large quantities of silica or quartz in solution. The solution of silica is effected at the moment of its separation from combination with the alkali during the decomposition of volcanic rocks, and is favored by the presence of alkaline carbonates in the water, high temperature

, and the pressure under which it exists in subterranean regions. When the water reaches the surface and is relieved from pressure and begins to cool, silica is deposited. So are the basins of geysers formed, and so the opal and hydrated quartz we find in many of the Cripple Creek veins, and in resilicated rocks.

Hot and cold springs rising in volcanic regions are charged with carbonic acid, and passing through calcareous rocks dissolve large quantities of carbonate of lime, and redeposit it in a crystalline form known as "travertine." Near the base of Mt. MacIntyre, west of Cripple Creek, a prospect is opened on a fissure filled with this substance.

Nearly all eruptions take place along lines of fissures (See Plate LXXX). Probably all volcanoes are located upon fissures of some kind, and even the general distribution of

Plate Lxxx.

Showing Craters Found Along a Line of Fissure in the Eruption of Etna.

volcanoes over the earth's surface has been attributed to lines of fissures, as if the earth had been cracked like a glass globe. We have plenty of opportunities of seeing ancient fissures filled with lava in the numerous dykes at Cripple Creek, and in the greater volcanic region west of it; but so far no distinct volcanic craters have been found. Nevertheless it is probable that craters existed along these fissures, long since removed by erosion, or buried deep under flows and surface matter. We not unfrequently find at Cripple Creek that fissures did not all succeed in breaking through to the surface, for at some depths in the mines the apices of buried dykes are found and fissures filled by vein matter, whose outcrops do not appear at the surface. A single vein is followed from the surface, and with depth

TATA TERE ee reser pees

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Set Ts

two or more veins are often encountered, together with various small fissures.

Earthquakes doubtless accompanied the eruptions, and developed many smaller fissures, and further shattered the rocks, Added to this at Cripple Creek, there was the second eruption of phonolite, after the andesite had ceased. This second eruption doubtless added new fissures in the efforts of imprisoned vapors to ferce for themselves channels to the surface.

Gase* And Solfataric Action,

The several stages in the decline of each volcanic outburst are marked by the appearance at the vent of certain acid gases. As the temperature at the vent declines, the nature of the volatile substances emitted undergoes a regular series of changes.

In fumaroles, sulphurous acid and hydrochloric acid abound, with sulphureted hydrogen and carbonic acid in much smaller proportions. Around these fumaroles, deposits of sulphide of arsenic, chloride of iron and of ammonia, boracic acid, and sulphur take place. Arsenical pyrites are a common associate for the ores near the surface at Cripple Creek, and many rocks are permeated with iron pyrites.

Where volcanic vent sinks into extinction, hydrochloric and sulphurous acids are first evolved, and later sulphureted hydrogen and carbonic acid springs. Such springs are common in the volcanic districts of Colorado to-day, but we have long passed the stage of the stronger acids, which could only be expected in the pit of an active modern volcano like Kilauea. We may, however, expect to find traces left of these gases, in the rocks of Cripple Creek, such as a bleaching and decoloration of the rocks, leaching and precipitation of iron, forming those varied patterns of oxidation so common at every prospect hole; also deposits of various sulphates and chlorides, rocks deprived of iron and alkalies reduced to powdery siliceous masses.

One action of subterranean springs is the transportation of material in a state of solution and redepositing of it elsewhere, especially in lines of relief of pressure, such as

fissures, shattered rocks, ans| decomposed rocks and zones in the rocks.

At Steamboat Springs, Nevada, metallic gold, cinnabar and other minerals have been found coating the sides of fissures from which living hot springs issue at the surface. In great volcanic foci the transfer of various sulphides, oxides and salts, which fill veins, has been effected either by solution or sublimation, or the action of powerful currents. This applies to the veins and ore deposits in qués- tion.

As the igneous activity of a district declines, the temperature of the issuing gases and waters diminishes, till at last the volcanic forces appear to have wholly abandoned the region and been transferred to another. This may have been the case with Cripple Creek and the volcanic region west of it, of apparently later date. The history of a volcanic disturbance is as follows:

First. The area is troubled by subterranean shocks and earthquakes.

Second. The origination of fissures is indicated by the appearance on the surface of hot and carbonic acid springs and other gases.

Third. With increased subterranean activity the temperature of the springs and gases increases.

Fourth. visible rent is formed at the surface.

Fifth. From this fissure gas and imprisoned vapor escapes so violently as to disperse the lava in clouds of scoria or dust, or to cause it to well out in flows.

Sixth. Volcanic action concentrates at one or several points, and the ejected material accumulates from volcanic cones.

Sometimes the volcanic activity dies out entirely, leaving cones thrown up along the line of fissure. At others, some such center becomes for a long time the habitual vent for the volcanic forces of the district, and a large cone is built up.

When the height and thickness of the cone have grown great, the succeeding eruption rends the sides of the cone, producing fissures, quickly filled by lava, forming radiating dykes and surmounted by parasitic cones. The dykes of Cripple Creek may in cases represent such occurrences.

When volcanic energies can no longer raise material to

the summit of the crater, nor rend the sides, they find relief by making new fissures and small cones in the country outside the main volcani. crater. The numerous phonolitic dykes in the granitic region outside of the main center at Cripple Creek may have so originated. At last volcanic energy diminishes, eruptions of lava cease, fissures are sealed up with solid lava, volcanic cones crumble away.

But still the existence of heated mater at no great depth is indicated by outbursts of gases and vapor, formation of geysers, mud volcanoes and hot springs. As the underlying rocks cool down, the issuing jets of gas and vapor lose their high temperature, diminish in quantity, geysers and mud volcanoes become extinct, hot springs disappear, and all is quiet.

It was in the latter or hot spring stage, that the ores were at Cripple Creek leached from the volcanic rocks, probably from great depths as well possibly as from the sides, and concentrated and dencsited in the fissures, shattered zones, and decomposed rocks. The last stage is as we find things to-day.

GENERAL SUMMARY OF PROBABLE VOLCANIC EVENTS THAT OCCURRED AT CRIPPLE CREEK,

At Cripple Creek there was a volcanic eruption in Tertiary times due probably to some mountain elevation going on in the region of Pike's Peak or generally in the mountains.

We may assume that preluding the eruption the area was troubled by earthquakes. Various kinds of acid and hot springs appeared above the surface, indicating the fissuring of the ground that followed.

At the bottom of these fractures, which may have been numerous, molten rock appeared, giving off imprisoned vapor from bursting blisters of lava. These shoots of steam formed into a cloud overshadowing the area, and carried upwards quantities of scoria and fragments which fell back around the orifice, forming a crater cone, or craters. These fragments being repeatedly shot up, and falling back into the crater, were comminuted into fine dust, and fell, together with larger angular fragments, over the surface.

The atmosphere charged with condensing steam gave

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rise to heavy rainfalls. The water descending the ravines caught up the volcanic dust and fragments, forming mudflows, the material rapidly setting into the rocks we call tuffs and breccias.

As the first eruption at Cripple Creek was of andesite, these are called andesitic tuffs and breccias, and constitute the principal mineralized rock of the mining area.

These tuffs are sometimes stratified by the materials being sorted in the air by the water.

After this first eruption ceased, there may have been a rest for atime, the lavas may have cooled and consolidated, and the region been covered by various acid and hot springs issuing from fissures caused by the late eruption.

Then the district was a second time disturbed, this time by an eruption of phonolite, ascending through numerous rents and fissures, not only in the overlying andesite, but also in the granitic region outside of the first volcanic "focus," probably finding the old seat of action too much choked by eruptive matter.

This second eruption added many new fissures to the already shattered rocks, and gave many opportunities for the deposition of metallic and vein material deposited through the medium of gaseous and hot spring and solfataric action which followed upon the cessation of the phonolite eruption.

After the eruptions at Cripple Creek ceased, the volcanic forces seem to have transferred their field of action to the area west of Cripple Creek in the Four-mile district. The rest is the history of to-day. ,

Cripple Creek As A Prospecting Field.

A visitor standing on top of one of the hills like Mt. Pisgah, overlooking Cripple Creek, and glancing at the various mines and multitudinous prospect holes speckling the hills, is struck with the compactness of the mining district within the limited area of 18 square miles. In this small area all the principal mines are located, and one can ride <round the entire camp in an hour or two. Outside of this area, there are as yet no mines of importance, though prospect holes may be found for a circuit of many miles.

Andesitic And Granite Areas,

He will observe that the principal mines are located on the round smooth hills, on their tops, slopes, and on the gulches, where the vegetation is mostly grass and quaking aspen. These too are within a sort of natural rampart of more rugged hills wooded with pine. In these outlying hills, only a few scattered prospects are visible. The reason for this is to be found in the geology of the region, and the differences between the areas occupied by andesitic breccia and granite. The rounded grassy aspen-covered hills representing the andesitic breccia carry most of the ore bodies, and the principal mines are restricted to them. The more rugged hills covered with fir trees, represent the granite area, and in them for the most part are few mines of importance, though many likely prospects are opened upon dykes of phonolite, which, so far as known, does not as a rule seem to be so productive a rock as the andesite.

There are intermediate areas, such as that of Battle Mt., characterized by the presence of both andesitic breccia, phonolite dykes, and granite, in which are some of the richest mines of the district, such as the Independence, Portland, Annie Lee, and others.

It will appear how important and useful a geological survey is of such a region, a fact not always recognized by practical miners. If the ore bodies are mainly associated with the particular rock called andesitic breccia, it is well for them to be able to recognize that rock, and ascertain the limits of its area.

Signs That Lead To Prospecting.

The next thing that strikes the observer is the prodigious amount of prospecting holes and prospecting trenches, the latter being particularly common. He may ask what was there in the general appearance and character of this district that led the "eagle-eyed" prospector to suspect the existence of ore bodies in it, or that it was "a kind'er likely looking place"? Again, how is it that it was so long overlooked by the " eagle-eyed," especially when so easily accessible?

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On general principles, in past years, miners in Colorado, after the Leadville and Aspen excitement, were more on the lookout for silver than gold; they looked therefore for rocks like those of Leadville, with contacts between porphyry and limestone, and every limestone ledge in the country was ransacked. Silver was rarely found in volcanic lava rocks, except perhaps in the great San Juan region, and miners thought as little about prospecting unpromising looking hills of lava, as they would the basaltic caps of the table mountains on the plains. Again, gold leads do not show their ore on the surface like some silverlead veins. There is nothing perhaps but a little seam of rust that might occur almost anywhere, and in any kind of rock. Hence lava districts of somewhat recent origin were overlooked, rather than looked over. The discovery of the gold-bearing properties of the Cripple Creek lavas, together with the increased thirst for gold, turned the tables, and now throughout Colorado every lava formation is being prospected with as much zeal and indiscriminateness as were the limestones in the Leadville days, The prospector now needs to know volcanic lavas at sight, to distinguish varieties, and to know all he possibly can about their origin, varieties and mode of occurrence. Hence the importance we gave to the subject in the preceding remarks on volcarses. prospector now would at a glance consider the area about Cripple Creek as worth looking over; and the geologist would consider it a very likely

lace, not merely from the presence of the lavas, but mainly rom the great decomposition of the rocks, and the evidence of the presence of past solfataric action.

Difficulties In Prospecting,

But the "eagle-eyed" one did not entirely overlook this district in the past, for some years ago he was sufficiently prepossessed with the appearance of things to drive a couple of short tunnels in Arequa gulch, and narrowly escaped becoming a millionaire. What troubled the prospector was, that though he found the hills covered with an extraordinary amount of " float," he could not trace this float to any ledge or rocks "in place." For the most part the hills were grassed over,or covered with vegetation; and through

the turf were very few outcroppings of a likely kind, so far as he could see. There were no prominent quartz veins, or zones deeply impregnated with iron, hence he gave up the region, mentally wondering where on earth all this ric float could have come from, perhaps solacing his mind by one of his igneous, brimstony theories that it had been scattered over the country from a distant volcano, or washed there by flood or glaciers from some unknown distant region. The former theory after all was not far from the truth but the absence of all rounding and smoothing of the fragments of float precludes the latter hypothesis. Evidences of former glaciation are veinaehalty absent from the vicinity.

The Region Impregnated With Ore,

To those who have studied Cripple Creek of to-day, the source of this " float' is no mystery. Little, if any of it, has been broken off from orthodox quartz fissure veins, or even extracted from well-defined ore zones. The fact is, that the whole andesitic area is more or less impregnated with the precious metals, and the float on the surface is little more than the surface debris of the general underlying rock. There is scarcely a stone that you may kick with your foot over the entire area, but ..hat will show some trace of gold. Onone hill an experienced mining superintendent told me that, for an experiment, he went around with a wagon and picked up the " float" almost at hap-hazard, and it averaged 22 dollars in gold. That such a "floaty" region should receive attention some day is not to be wondered at, and we believe Colorado Springs men were amongst the first to give it serious attention by opening holes and prospecting trenches almost at random, resulting in important discoveries. Asa rule even after this, the best mines were discovered by mere chance and guess work, or by plodding but blind prospecting, something like the Leadville prospector who in early days had all Leadville before him to prospect, but did not know where to begin, till sitting down under a tree eating his lunch he saw a squirrel scratching in the ground; he accepted the happy omen and "went down," so the story goes, and of course

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"struck itrich;" so we understand the Pharmacist and many other now noted mines were discovered at Cripple Creek.

Mode Of Prospecting,

This absence of surface outcrops or visible leads, when the " rush' came, led to indiscriminate and abundant prospecting which has been kept up till the present time, hence the extraordinary freckling of the hills with prospect holes and trenches.

Sometimes they would select any piece of land they thought, for some reason or other or without any reason at all, likely, and go to work to punch holes and dig trenches all over it to find something. In this way they frequently came across enough signs to warrant putting down a prospect hole, and holding the claim, and then went on "to pastures new."

Character Of Float And Other Surface Signs,

As we have said, the whole region is covered with float. This float is usually a somewhat porous piece of lava, or andesitic breccia, or tuff, stained with yellow, brown, or red oxide of iron, sometimes in patterns or concentric rings. It is often found to be honeycombed when broken with a hammer, There is no visible ore, but an assay will most likely show traces of more or less gold. Again, a species of red porphyritic granite has been desilicated and robbed of many of its crystal constituents, and left as a porous skeleton of a rock by the action of gases and springs. The pores in this are often occupied by oxide of iron, or even by crystals of fluorspar. This is a likely kind of float. Honeycombed rusty rock with quartz crystals is a likely float, both of these representing the action of mineral hot springs. At rare intervals we may see a little of this oxidized rusty rock in place protruding from under the grass, and if so, there is sure to be a prospect hole alongside of it.

Bold outcrops of lava rock are comparatively scarce, and when they do appear, asin the cliff above Victor mine, Mt. Pisgah, Bahr, and Rhyolite peaks, the rock is apt to be so hard as to preclude the probability of much ore deposits in it.

Pieces of rock or float stained a violet purple color by fluorine are considered a good sign of an ore body not far off, this fluorspar being found characteristic of some of the richest veins in the camp; and fluorine gas was doubtless

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connected with the deposits of ore matter, especially of the tellurium, the present matrix of the gold in the deeper parts of the mines.

Pyrites is not usually found on the surface till the rock is broken open, and tellurium in little silver scales and spots, not till considerable depth is attained. But free gold may be found in surface float, and from the grass roots down, and in the early development of a mine, in the oxidized upper portions, associated with iron oxide and black manganese or " psilomelane."

Mi ceous or specular iron, is seen in some prospect holes; and localities marked by evidences of past hot spring action, such as the appearance of botryoidal chalcedony or opal, should be prospected. A common and curious marking in some of the bleached volcanic lavas is that of an imitation of trees, ferns and mosses, popularly called " photographic rock," scientifically " dendrite" or tree rock.

This remarkable imitation of nature is due to crystallization of solutions of manganese, a. .uay be compared to fern-like appearances on a frosty window-pane in winter, which are certainly not of organic origin, or in anyway connected with the processes of photography. These dendritic markings may or may not be considered as signs of ore. Similiar markings are very common in the porphyries of Leadville overlying the silver deposits.

Surface Prospecting Of A Mine,

In some of the surface discoveries of mines, when a considerable area, covered by a blow-out of iron oxide associated or not with purple fluorspar, has been found to run well in free gold, the ground is prospected and developed to the depth of a few feet, and over a certain amea, with plows and scrapers, the material so obtained being sent wholesale to the stamp-mill and often giving rich returns. The object of this work is not merely to get all the values out of this rich float, but im hopes of uncovering the vein or veins of whichit is the oxidized cap or blossom. This was the way in which the Deerhorn mine was opened up, and its veins discovered on Summit Hill. The ground on the top of the hill is observed to have been " gophered" in all directions like the catacombs to a depth of about ao feet, and over an area of square acre or so. This was done partly to gather up and collect the rich float which

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was found scattered over the hill and partly to discover the leads in place. This rich float was stained with purple fluorine, and upwards of 25,000 dollars' worth of gold was obtained from i this, the material being dug up by plows and scrapers, before the subsequently discovered veins were found or worked. In the case of the Anaconda mine on Gold Hill, the out- j crop of a dyke of andesite was discovered on the hillside ] covered with an oxidized crust carrying gold. The owners developed this by an open quarry, about a hundred feet in length and 4o to 50 feet deep, from which they extracted the bonanza which made this mine at its outset so celebrated, and later proceeded to uncover the dyke on the surface, to a depth of about 20 feet along the entire length of ] their claims, but nothing comparable with the bonanzas . the first quarry has been found since in extension or H

Richness With Depth, Etc.

PR Side

Many of the mines shipped their best ore from the grass roots and upper oxidized portions of the veins, which con- i tained free gold and were free milling, With depth some of these mines have not done nearly as well, especially when they reached the unoxidized zoue, ..way from surface influences, and the ore was found wrapped up in tellurium + or iron pyrites. 1

The palmiest days of many a gold camp are its earliest , days. ya

Suggestions To Prospectors. A

In the more productive area the prospector will do well i to keep to the andesitic breccia, and follow the signs we i have mentioned. Outside of this area his course may be a 4 little different, as then he is in the granite district, and looks

i out for the appearance of dykes of phonolite, rarely more

: than a few feet, though sometimes many yards, in width, and

i easily distinguished from the red granite by their light gray or white color. These dikes do not often appear outcropping in the granite cliffs, but are more commonly to be found buried beneath the debris and grass of the slopes.

On these he may find no indication and trust to hap-hazard trenching; or a few stray pieces may lead him to the spot.

The more rusty, oxidized and decomposed the phonolite, the more likely it is to carry gold; at times he mav find ore and free gold in the dyke itself, but more often at its contact, on one or both sides, with the granite. There he is likely to find a crevice filled with clay or iron-oxide, carrying seams and cavities lined with quartz crystals or stains of purple fluorspar.

Sometimes he may find the coarse granite, as in the case

Plate Lxxxii.

A Section Moose Mine Vein, Raven Hill. 1. Country Rock Breccia. 2. Yellow Jasper, with Cavities of Quartz Crystals. 3. Blue Gray Jasper, with Seams of Quartz and Iron containing Gold.

of the Independence mine on Battle Mt., just at the contact with the dyke of lava, to be very rotten, much honeycombed and robbed of many constituent minerals, and these, by replacement with metals, may yield him the richest ore. Again, the dyke between walls may be reduced to a blue or yellow jaspery clay, with a vertical lamination or cleavage, the lines of cleavage filled with quartz and iron oxide (See Plate LXXXII); in such lines he is apt to find the richest ore.

After opening a prospect, the ore signs, consisting of stains of oxide of iron and manganese, instead of pursuing an even or regular course are apt to scatter amongst the infinite number of crevices shattering the rocks, no one

little lead being of sufficient richness to follow with profit, and the whole body bet.veen walls scarcely paying to work.

The ore signs often follow a very uneven course, now lying upon a fairly defined wall, then running for a distance into one wall or other, or again following the main course of the creviced lava breccia between walls, now in pockets and crevices, again scattered, or again impregnating the porous and decomposed rock. There are very few true, well-defined veins in the camp; the ore rather impregnates certain ill-defined, shattered zones of rocks between certain ill-defined boundaries called walls. At others the ore occupies narrow cleavage planes in the rock, of which there may be two or three in a mine, some of them productive, others very little so. Ore bodies in the harder or more compact rocks, such as the Buena Vista and Victor mines, are apt to have something more like defined veins and defined walls. In some cases surface signs have been poor, and with depth have done well; the exact opposite has often been the case. Some mines have been good from bottom to top, but we have to be careful here, as in most gold camps, of the old fallacy of " richness with depth." There is little more criterion for this than in other camps, and many a once famous mine is looking vainly with depth for its lost bonanza, though in other respects doing fairly well,

As regards the granite itself, we have heard of few ordinary quartz fissure veins unaccompanied by lava intrusions proving productive.

The fine grained, red, eruptive granite on Barnard Creek, north of Cripple Creek, has shown a promising ore body in a lava dyke in the granite, which, singularly enough, produces a fine grained galena, rich in gold. Galena is quite aware ore in Cripple Greek. Green carbonate of copper stains appear at times in the schists and gneisses, but none so far productive.

The railroad from Canyon City to Cripple Creek did some good prospecting work in the granite area, its cuttings exposing quite a number of phonolite and other dykes, together with some granitic veins.

Outside of Cripple Creek, in the great volcanic area to the north, between Cripple Creek, and South Park, is a fair prospecting field. The rocks are mainly granites,

rhyolites, trachytes, andesites and basalt, the products, as at Cripple Creek, of a series of volcanic eruptions, of which the latest appears to have been basalt, which commonly caps the other and lighter colored lavas.

The rocks in this region are for the most part less decomposed than those at Cripple Creek, which is not so favorable a sign. Here the prospector should look out for all signs of decomposition, such as we observed at Freshwater district, a not unlikely spot. The very hard, massive rocks are not likely to be productive, such as the hard black basalts. The lighter colored and more decomposable lavas offer a better chance.

Centers of eruption, such as relics of old craters and dykes from which these different lavas issued, should be sought for and prospected. Balfour, a small mining camp at the north of this area, is established among granite and eruptive rocks, which have been found to be mineralized by pyrites. The granites here have several fissure veins and dykes in them, showing considerable disturbance to have taken place in that neighborhood. The low hills in which the prospect holes are located are capped with basalt, apparently resting on volcanic tuffs and other lavas. So far, nothing very productive has been found, though here, as elsewhere, much is hoped for with depth. Singularly enough, in one of these veins in lava, we noticed a tarry substance or inspissated bitumen in the cavities of the rock, an unusual occurrence in fissure veins or in volcanic rock.

Chapter Xii. Ore Deposits In Sedimentary Rocks.

Blanket Ore Deposits, Contact Deposits.

This great second class of ore deposits, occurring principally in Paleozoic limestones at contact more or less with intrusive sheets of porphyry, is mainly represented in Colorado by the Leadville and South Park mining district, the Kokomo and Red Cliff districts, and the Aspen and Gunnison districts, though locally here and there, wherever

Paleozoic strata accompanied by igneous rock may be exposed, silver mines may be found. We will begin with Leadville and South Park as primarily instructive and typical. SUUTH PARK ORE DEPOSITS.

The basin plain of South Park is underlaid by sedimentary rocks from the Cambrian below, to the Upper Cretaceous on top. These strata slope up to the crest of the

Mosquito range on the west, where they become violently folded and faulted and eroded.

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Contact Ore My YY] : he LINE: pent Tes WN YY Yj y, "Contact Depos e SZ st ae. Tp lass Pondery Mine

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PLaTE LXXXIII. Section of Leadville Cliff.

The mineral developments are on the slopes of this range on both sides of it.

The order of succession of strata forming the structure and cliffs of the range and resting on the granite, is as follows, beginning with the lowest:

Feet thick. Cambrian quartzite 60. cesee eee en eee e renee ene nete ener steeeeees 200

Silurian drab limestone (dolomite) . .ceeeeee creceeeveevoue 200 Lower Carboniferous blue limestone... 05 ceeeeeeeeresees 200 Middle Carboniferous sandstones and quartzite (Weber grits). .2,000 Upper Carboniferous limestones, reddish SandstoneS eeeees 1,000

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These formations have been traversed by eruptive quartzporphyry and porphyrite dykes and intrusive sheets. "The dykes occur principally in the Archean, but the intrusive sheets are many and are spread out between the quartzites and limestones of the Cambrain, Silurian and Carboniferous.

The connection between the eruptive masses and deposition of ore is very marked. The ore bodies are a concentration of the metallic minerals originally disseminated through the mass of these eruptive porphyries and deposited along their plane of contact with the sedimentary beds, and by metasomatic substitution extending more or less into the mass of the latter.

On mountains Lincoln and Bross, in the principal mines, the ores are mainly argentiferous, yielding galena and its products of decomposition, viz., carbonate of lead (cerussite) and sulphate of lead (anglesite) with chloride of silver. Barite (heavy spar) is a common gangue or vein rock especially in the richest parts of the mine. Iron pyrites decomposed and passing into a hydrated oxide of iron, together with a black oxide of manganese, give to the ore its rusty and black color.

The deposits occur in irregular bodies or pockets often of great size, in the blue limestone, near its upper surface, but not always easy to find or follow. This limestone was originally covered by a sheet of quartz-porphyry which has been locally removed from the ore deposits, but exists in the peak. This porphyry, generally recognized by its large feldspar crystals, is called Mt. Lincoln porphyry and is quite common and characteristic of Western Colorado. In the Dolly Varden mine the ore occurs in the limestone at contact with a vertical dyke of white quarts-porphyry.

In the Fanny Barrett mine, 0n Loveland Hill, rich deposits of galera and anglesite occur in a vertical fissure (probably a gash vein) crossing the hill from side to side and traversing the Paleozoic strata at right angles to their dip, but probably not entering into the underlying granite. This mine was discovered by noticing little pieces of iron following a general line across the hill.

In Buckskin Gulch the Phillips mine is an immense mass of gold-bearing iron pyrites, deposited, in beds of Cambrian quartzite near a dyke of quarts-porphyry. This mine was discovered by its rusty outcrop being exposed along

the edge of the stream. At first this crust of iron oxide was loose enough to be panned for gold with good success by the old-timers, and afterward milled. But when the hard pre set in, the ore was found to be too low grade to pay or roasting and smelting, and for many years lay idle.

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The Criterion in the cliff above this consists of large caves in Cambrian quartzite, still partly occupied by oxidized goldbearing iron ore, and galena-bearing silver close to a pore pavrite dyke.

The London mine in Mosquito gulch is peculiar and instructive as being involved in the great London fault. There are two strong veins or deposits of pyrites carrying both gold and silver; the gangue of one is quartz, the other calcite. They occur in the limestone in connection with an intrusive bed of white porphyry. These deposits stand in a vertical position, the beds containing them having been turned up abruptly against the great London fault, by whose movement the Archean granite rocks forming the eastern half of London Mt. are brought up into juxtaposition with the Silurian and Carboniferous beds at its western point.

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The London Mine Fault.

Going south along the Mosquito range the intrusive sorphyries diminish in extent and with them also the mineral deposits.

The Sacramento mine is a good example of a " pocket" mine. Rich bodies of galena and rich decomposed ores have been found at uncertain intervals in a series of pockets or cavities. Some of these pockets or cavities are empty, and lined with modern stalactites, others contain loose sand, with pebbles of rich ore, others are quite full of rich ore deposits. These deposits are difficult to follow with

any degree of certainty, and much of the profits made in the rich pockets have been used up in blindly " gophering " after other pockets. From some of these chambers open fissures or joint planes ascend to the surface, The limestone was originally capped by a porphyry which has since been eroded off. This porphyry doubtless supplied the ore.

Leadville District.

The western boundary of this district is the Sawatch range of Archean granite. The slope of the Mosquito range in the east and the hills on the north, forming the watershed between the Grand and Arkansas rivers, have a basis of Archean granite and gneiss more or less covered by patches and remnants of the Paleozoic formations, é@.¢., Cambrian, Silurian and Carboniferous, which have escaped erosion.

Their lower position relative to corresponding beds on the eastern or South Park side of the Mosquito range is due in part to faulting, and in part to folding of the beds.

Within these Paleozoic formations, these beds of quartzite and limestone, ¢here ts an enormous development of eruptive rocks, principally quartz-porphyries partially occurring as dykes but generally as immense intrusive sheets following the bedding plane of the sedimentary rocks.

Glaciers have been at work also in this neighborhood. A huge "mer de glace" occupied the great valley of the Arkansas to whose bulk numerous side glaciers contributed ; these glaciers have carved and sculptured the mountains. In the flood period following the first glacial epoch a lake was formed occupying the head of the Arkansas Valley. The stratified gravel and sand beds which were deposited at the bottom of this lake now form terraces bordering the valley of the Arkansas River. These beds, known as "wash" or placer grounds, yield gold and are open to further development. Leadville is the center of the mining district, the ores are argentiferous galena and zincblende. They are smelting ores. Their value is increased by their having been oxidized, the lead occurring as carbonate, the silver as chloride in a clayey, or else silicious, mass of hydrated oxides of iron and manganese.

The ore is principally confined to the horizon of the

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"blue" or Lower Carboniferous limestone, covered by an intrusive sheet of " white Leadville quartz-porphyry." The ore bodies occur not only at the immediate contact of these rocks, but extend down in irregular pockets and chambers into the mass of the limestone, sometimes to a depth of 100 feet. Sometimes the ore completely replaces the limestone between two sheets of porphyry, as in the " Col. Sellers mine," Chrysolite, Little Pittsburg, and on Fryer Hill. A few ore bodies occur, carrying more gold than silver, found at other horizons, usually as "gash" veins running across the stratification or along bedding planes. Such are the Colorado Prince in quartzite, the Tiger and Ontario in the Weber grits of the Middle Carboniferous,

The " Printer Boy," one of the oldest mines, has produced a good deal of gold, found as free gold associated with carbonate of lead and galena, passing down, as is usual in gold mines, into unaltered auriferous iron and copper pyrites, which occur in a body of quartz-porphyry along a vertical cross-joint or fault plane in the porphyry. The gangue is a white clay resulting from decomposition of the quartz-porphyry, and though the clay ore is rich, it shows no minerals to the eye.

The Paleozoic formations, together with the intrusive porphyry sheets sandwiched in between them, have been compressed into gentle folds, and where the fold was at its greatest tension, a series of parallel faults have occurred having a general north and south direction; their uplifted side is generally to the east.

The prevailing eruptive rock is the "white Leadville porphyry," occurring generally above the blue limestone but also in places below it and at other horizons.

There are also other intrusive sheets of different varieties of quartz-porphyry. The ground is generally buried beneath a hundred feet of glacial moraine material, locally called " wash."

The general geology of the South Park and Leadville region has been so elaborately traced by the labors of the U. S. Geological Survey that we cannot do better than give an abstract of their report in this connection:

Mosquito Range,

A study of this range is necessary to the understanding of the Leadville ore deposits, which occur on its western side. It comprises a length of 19 miles along the crest of the range, and in width including its foothills bordering the Arkansas Valley on the west, and South Park on the east, a slope, in one case of 7% miles, and in the other of — g miles. All of it is about 10,000 feet above the sea evel,

The range has a sharp single crest trending north and south., To the west this crest presents abrupt cliffs descending precipitously into great glacial amphitheatres at the head of the streams flowing from the range. Mts. Bross, Cameron and Lincoln constitute an independent uplift. The abrupt slope west of the crest is due to a great fault extending along its foot, by which the western continuation of the sedimentary beds, which slope up the eastern spurs and cap the crest, are found at a very much lower elevation on the western spurs. The jagged step-like outline of the western spurs is due to a series of minor parallel faults and folds.

The secondary uplift of Sheep Mountain on the eastern slope is due to a second great fold and fault.

The elevation of Mount Lincoln is the result of the combination of forces which have uplifted the Mosquito range and those which built up the transverse ridge separating the Middle from the South Park.

The range has been sculptured by glaciers into canyons, and the Arkansas valley is covered with horizontal terraces representing the distribution of material by waters, on the melting of the glaciers.

In the seas of the Paleozoic and Mesozoic eras which surrounded the Sawatch islands, some 10,000 to 12,000 feet of sandstone, conglomerates, dolomitic limestones and shales were deposited. Towards the close of the Cretaceous, eruptions occurred by which enormous masses of eruptive rock were intruded through the Archean floor into the overlying sedimentary beds, crossing some of the beds, and then spreading out in immense intrusive sheets along the planes of division between the different strata.

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The 'intrusive force must have been very great, since comparatively thin sheets of molten rock were forced continuously for distances of many miles between the sedimentary beds.

That the eruptions were intermittent and continued for a long time is shown by the great variety of eruptive rocks found. That this eruptive activity preceded the great movement at the close of the Cretaceous, which uplifted the Mosquito range as well as the other Rocky Mountain ranges, is proved by the folding and faulting of the porphyry eruptions themselves.

In the period intervening between the close of the Cretaceous and the deposition of the Tertiary strata, during which the waters of the ocean gradually receded from the Rocky Mountain region, the pent-up forces of contraction in the earth's crust, which had been long accumulating, found expression in dynamic movements of the rocky strata, pushing together from the east and the west the more recent stratified rocks against the relatively rigid masses of the Archean land, and thus folding and crumpling the beds in the vicinity of the shore lines.

The crystall'ue and already contorted beds of the Archean doubtless received fresh crumpies in this movement.

A minor force also acted north and south, producing gentle lateral folds along the foothills at right angles to the trend of the range. These movements were not paroxysmal or sudden and violent, but protracted for an enormous lapse of time, and appear to be continued in diminished force up to the present day.

Mineral Deposition,

It was during the period intervening between the intrusion of the eruptive rocks and the dynamic movements which uplifted the Mosquito range, that the original de- - positions of metallic minerals occurred in the Leadville region in the torm of metallic sulphides, though now they are found largely oxidized and in other combinations. They were derived from the eruptive rocks themselves and are therefore of later formation thanthey. Their having been folded and faulted with them shows that they must have been formed before the great Cretaceous uplift, and therefore they are older than the Mosquito range itself.

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No.1. Ideal Section, s*oning Paleosoic and Mesozoic Strata, with Intrusion: of Eruptive Islands, prior to the great Mountain

§ uerce Staves Pecos

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laweter eft (A el meas coal ae Range 7OSe207> Pasteasore 2

No. 2. Ideal Section, showing result of the great Post-Cretaceous t

No. 3. Average Section of Leadville District, Mosquito Range and South Parkas i PLaTE

Sections to Illustrate the Gradual Geological Development of the

Intrusions of Eruptive Rock, beneath the Mesozoic Sec, between Sawat, Front Range Y Mevation b ene of Cretaceous. anne tk

teréat Mountain

ange ZJouth Park Basin Cotorade front Range Upisyt t great Post-Cretaceous Uplift and the folding "p of the Mosquito Range.

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Archacan Granite Gnesse

ngeand South Park as tt ts Today, showing result of Faulting and subsequent Erosion. PLaTtE LXXXVI.

ical Development of the Leadville and South Park Region, Colorado.

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The deposits were formed by the action of percolating waters taking up certain ore materials in their passage through neighboring rocks, and depositing them in more concentrated form in their present position. This may have taken place while the sedimentary beds were still covered by the waters of the ocean, and the waters therefore may have been derived from it, or the area of the Mosquito range may have already emerged from the ocean and the waters have been estuarine. The uplift of the Mosquito range consisted of a series of folds fractured by faults. The crest is formed by the Mosquito fault, another parallel fracture is the London fault. The greatest movement is towards the center or Leadville region, dying out at either end north and south; the greatest displacement is 10,000 feet. Whatever cliffs may have originally been formed by this faulting have been planed down by glacial erosion.

Origin Of Leadville Ore Deposits,

The ores are deposited for the most part in the blue limestone of the Lower Carboniferous. As the ores were deposited by water solutions, the soluble limestone beds would be more easily acted upon by solutions than the sandstones and shales composing the other rocks of the neighborhood, which are less susceptible to percolating water. The Paleozoic formations in America are the principal repositories for lead and silver ores, not by reason of their geological age, so much as by their containing such a quantity of soluble limestone and being physically as well as chemically favorable for the reception of mineral solutions.

The physical structural conditions of Leadville are particularly favorable to the concentration of percolating waters in the blue limestone. Great intrusive sheets of porphyry follow the linsestone persistently, principally on its upper surface. This porphyry is very porous, and full of cracks and joints, affording ready channels for water from above, and also channels for ascending water from below, along the walls of the fissures, through which it iserupted. Such waters passing through a medium of different composition would be ready for a chemical interchange with the limestone.

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Composition Of Ores.

The ores were deposited originally as sulphides. This is shown by the fact that the oxidized ores near the surface pass down with depth into sulphides. In Ten-Mile district these oxidized ores are seen to result from the alteration of a mixture of galena, pyrite, and zinc-blende. There is very little gold in the average Leadville ores; what little there is comes from the Florence mine (native gold), and from others where it is associated with pyrites. It is usually associated with porphyry rocks, and a porphyry commonly called pyritiferous porphyry shows gold to exist diffused through the pyrites disseminated through its mass.

Silver occurs as chloride, a secondary condition, its original condition probably being sulphide.

Lead occurs as carbonate and sulphate and, deep in the mines, as sulphide. Specimens are common of galena nodules surrounded by a thin coat of sulphate, and that again by a coat of carbonate, showing the order of transition from sulphide to sulphate and thence to carbonate.

In the iron mine native sulphur occurs as an alteration product of galena.

Iron and manganese constitute rather a gangue material than an ore. They are hydrated oxides and protoxides. The iron was originally deposited as sulphide or pyrites, but has been wholly transformed by oxidation.

Zinc is not common, but occurs as calamine (zinc silicate) in needle-like hairs and white crystals in cavities in the mines. Its original form was zinc-blende (zine sulphide), as shown in the Ten-Mile district.

The earthy niinerals, alumina, lime, silica and magnesia, are in fair proportions, as might be expected from ores which are a replacement of limestone in close connection with porphyry. The alkaline element among the ores might also be traced to the influence of the latter rock.

The agents of alteration were surface waters, which contain everywhere carbonic acid. oxygen, organic matter, chloride of sodium (common salt}, and phosphoric acid. The rocks through which these waters passed, such as porphyries and limestoaes, were found to contain phosphoric acid and chlorine, while organic matter exists in the blue

limestones; and in the overlying shales and sandstones are many carbonaceous beds and even beds of coal. Water passing through these rocks would take up all these elements and be ready for chemical reactions.

Galena (lead sulphide) is much richer in silver than its alteration product, carbonate of lead, orcerussite. On Carbonate Hill the carbonate averages 4o oz. silver, the galena is 145 oz. to the ton. But galena is harder of treatment.

Silver is found at times disseminated through vein matter and country rock, without the presence of lead, proving that during alteration, silver was removed farther from its original condition and more widely disseminated than lead.

Outcrop deposits have proved in many cases richer than those at depth. The deposits near the surface have been the refined, concentrated remains of larger bodes gradually removed by erosion, as the alteration by surface waters went on. The baser and more soluble metals have thus been removed in solutions, leaving behind the more valuable and perhaps less soluble metals in new and richer secondary combinations.

" Kaolin" or " Chinese talc," which occurs both along the line of contact and between the porphyry and limestone and also in the heart of the ore deposit, is a decomposition product from porphyry. It consists principally of hydrated silicate of alumina derived from the feldspars of the porphyries, perhaps at the time when acted upon by sulphurous waters, which brought in the original ore deposits.

Calcite occurs incrusting recent crevices and lining recent cavities.

Barite is common, generally associated with chloride of silver and manganese, and is /ocally recognized asa sign of rich ore.

Mode Of Formation Of Leadville Ore Deposits.

The ores were deposited from water solutions by a metasomatic interchange, #.e., substance exchanged for substance with the limestone; and lastly or originally as sulphides.

Mineral matter is carried from one place to another within the earth's crust by heat and water, or these combined. Metasomatic interchange of metal for limestone and the removal of dolomite could only have been produced by

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water. The ores were wot deposited i. pre-existing cavities, but are a replacement of the country rock, /.¢., dolomitic limestone.

The ores grade off gradually into the material of the limestone, with a definite limit, as would not have been the case if the limestone had been previously caverned. The only limiting outline to the ore bodies is that formed by the contact porphyry.

Fragments of unaltered limestone are found entirely enclosed within the ore bodies, and ore bodies often occupy the entire space for long distances between two horizontal sheets of porphyry, which space further on is occupied by the limestone. This is well seen in Colonel Seller's mine. Examination of ores and veinstone shows lime and magnesia not in the crystalline condition they would have, had they been brought into a pre-existing cavity and deposited, but in the same granular condition in which they exist in the country rock.

The deposits in rocks other than limestone consist of metallic materials and of altered portions of the country rock, in which the structure of the latter can sometimes be still traced, and are not the regular layers of matter foreign to the country rock, which results from the filling of a preexisting fissure or cavity by materials brought in from a distance and deposited along the walls.

In the Ten-Mile district the arrangement of the particles of the original rock is frequently seen to be preserved in the metallic minerals, which maintain a certain parallelism with the original bedding planes in the lines defined by minute changes in these minerals.

The common characteristic of caves which have been dissolved out of limestone is, that their wails are coated with a layer of clay which has been left undissolved by the percolating waters, and these walls have a peculiar surface of little cup-shaped irregularities from which also stalactites frequently hang. There is also an accumulation at the bottom of the cave of fragments of limestone, fallen from the sides of the roof. None of these characteristics are found associated with the ore replacements.

Also, when mineral matter is deposited in " pre-existing cavities" it takes the form of regular layers parallel with the walls of the cavity, as is beautifully shown in geodes

lined with a succession of zeolites or with layers of chalcedony, opal and quartz.

No such successive arrangement in layers is found in the Leadville ore bodies.

Again, could such large, open cavities have existed for long distances without support between the layers of porphyry? Why did not these porphyry sheets close together? And further, how could such extensive cavities have been formed and kept open under a pressure of 10,000 feet of rock, which the geology of the region shows to have existed above the deposits at the time they were being formed? Such cavities as we do find in the region are all of very recent origin, cutting through both limestone and ore bodies, and have been hollowed out by surface waters more recent even than those which produced the secondary alterations in the ore bodies.

The ore deposits of Ten-Mile district about Kokomo, not far north from Leadville, are very similar in character to those of Leadville. They occur, however, in a somewhat higher division of the Carboniferous, and the ores as a rule are not so decomposed and oxidized, and the transition from the original sulphide character of the deposits to the oxidized condition is more easily show"

Red Cliff Gold

At Red Cliff, still further north of Leadville, in the valley of the Eagle, the same geologic series are found, penetrated, as at Leadville and Kokomo, by eruptive sheets. In the limestones at contact with the porphyries, much the same classes of ore deposits occur, but the peculiar and instructive feature of tile camp is the rich deposits of gold in chambers and cavities in the hard and usually unproductive Cambrian quartzites resting on the granite.

The gold in these chambers often occurs as nuggets. The quartzites dip about 10° N. E., and between their bedding planes lies the ore. The so-called contact or bedding plane between one stratum of quartzite and another is clearly defined. At this line there isa filling so to speak of " brecciated," broken up quartzite fragments cemented by iron rust and at times by iron pyrites, The thickness of this breccia varies between four and six feet, Ore chimneys on this breccia occur at intervals,

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Their presence is indicated on the outcrop by seams of rusty clay, which lies on top of the ore body and follows it along the roof of the deposit for 100 to 200 feet, then thins out gradually and coapipeets entirely; at the point of its disappearance, unaltered iron pyrites set in.

These ore chimneys are about 4 feet in width, their thickness is limited to the space between the floor and roof. The quartzite roof is always smooth, but the lower quartzite floor is rough and corrugated and shows chemical action on it attendant on deposition of ore. The floor at times is impregnated with ore, which does not, however, extend any great distance into it. Though the ore chimneys are from 4 to 6 feet wide the pay ore is only a few inches, swelling form floor to roof. The pay ore in the oxidized rusty portion yields 7 ounces gold and 50 ounces silver.

In mining, the floor is followed as a guide. Individual ore chimneys are connected laterally by ore chutes like a network, These ore chimneys divide and separate, the branches reuniting or again splitting up. The whole ramification comes together again at intervals in one main chimney. The rock filling the space where the divergence has taken place is the same as the breccia filling, only more compact and impregnated with pyrite. These fillings are left standing as pillars after the ore is mined.

To sum up, the characteristics of these deposits are:

first. The outcrop of the ore chimney indicated by what is locally called a " joint-clay."

Second. A zone of oxidation for 200 feet, which gradually merges, as the natural water level is approached, through a zone of mixed oxides and sulphides to the zone of unaffected sulphides.

Third. The "joint-clay" gradually disappears as the sulphides are approached. The ore on analysis shows sesquioside and sesquisulphate of iron, silica and alumina, and sulphate of barium.

In the Ground Hog mine the ore chimneys are 600 feet apart, but are probably connected. They abound in nuggets; the latter are sometimes twisted like bent horns; in other chutes they are lumpy, composed of crystalline gold particles cemented together by sesquisulphate of iron and horn silver.

Nuggets are found in troughs in the quartzite floor imbedded

in clay associated with rich silver or horn silver ore. With the nuggets are lumps of sesquisulphate of iron carrying much gold. This proves, according to Mr. Guiterman, that the secondary deposition of gold in crystals was through the medium of persulphate of iron derived from slow . xidation of iron pyrites, and is an admirable confirmation of the theory as stated by Prof. Le Conte in his geology.

Aspen Ore Deposits,

. The Aspen mining region is geologically related to that

of Leadville; each is on the shore line of the old Archean island of the Sawatch, one on the east, the other on the west, opposite one another, but about 50 miles apart.

The ore deposits occur in the same general horizon, viz., the Lower Carboniferous.

Both regions show intense disturbance, both by volcanic intrusions of igneous rock, folding, and faulting. The process of ore deposition in both regions has been an actual replacement of the country rock by vein material.

At Aspen the ore is not found in actual contact with the overlying eruptive igneous rock, but at some depth down in the limestone, at a zone where the " blue limestone" becomes dolomized, or, as Aspen miners say, "passes from blue lime into short lime."

The mines of Aspen are situated in Paleozoic strata reclining upon the slope of a narrow ridged mountain, forming a granite spur " ex echelon" with the Sawatch range.

The strip of ountry in the vicinity of Aspen constitutes the dividing li... between the two distinct uplifts of the Sawatch range on the east, and the Elk mountains on the west, and has been successively affected by each upheaval.

The Sawatch upheaval was a gradual elevation of this mountain mass resulting from a gradual subsidence of the adjoining sea bottoms, which caused the sedimentary beds deposited in those sea bottoms to slope up at varying angles all along the ancient shore line toward the central mass of the Archean island.

The Elk Mountain range, which extends to the west and south of this region, was upheaved later than the Sawatch, with greater violence and eruptive energy, and the up-

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heaval was accompanied by enormous intrusions of eruptive rock which were forced into the sedimentary strata already shattered by the forces of upheaval, in great " laccolites," or solid masses, and spread out through them in every direction in the form of dykes and intrusive sheets. The surface exposures of these igneous bodies cover areas of twenty-five to thirty square miles, and their extension below the surface is doubtless very much greater.

The intrusion of such enormous masses of foreign matter must not only have greatly disturbed the beds within the region of upheaval, but also have so expanded the volume of the earth's crust in this area as to cause a severe lateral pressure in the adjoining region. That adjoining region was Aspen and its neighborhood.

It would be just in the strip of sedimentary beds along the Aspen Mountain ridge, which is backed by a projecting point of the unyielding Sawatch Archean, that this compression would be most severely felt, the Sawatch granite mass acting as a point of resistance against the intense lateral compression caused by the younger Elk Mountain uplift.

The sedimentary beds resting against the Archean correspond generally, with slight differences, to those in the South Park and Leadville region in a similar position.

The latter were deposited in a partially enclosed bay, now constituting the South Park basin, the former on the west side of the Archean

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island in a wider and deeper sea, and on this western slope the beds are generally much thicker than those of corresponding geological horizons on the east.

Stratigraphy Of Aspen.

1. The horizons represented are the Upper Cambrian quartzites, 200 feet, resting on the Archzan granite.

2. Silurian silicious limestones and quartzites, 340 feet.

3. Darker limestones, rusty brown and dolomitic at base, blue compact and pure on top, 240feet. (These are Lower Carboniferous.)

4. Carboniferous clays and shales and thin bedded limestones, 425 feet. These belong to the Weber grits (Middle Carboniferous).

5. A series of variegated green and red sandstones, clays and shales, some limestones and red sandstones of the Upper Carboniferous. ;

6. Heavy bedded red sandstones (Triassic).

Above these again are several thousand feet of Cretaceous strata, up to the base of the Laramie coal beds. (The Cretaceous, however, and the Jurassic do not rest immediately upon the granite).

Diorite.—On Aspen Mountain is a bed of " white porphyry" (diorite) in the black shales, 60 to 100 feet above the top of the blue limestone. It is 260 feet thick on the slope back of town, but thickens considerably to the south, and is traceable to Ashcroft. It appears to extend also across the valley of Roaring Fork to Smuggler Mountain. Small intrusive sheets also occur in the lower quartzites near the point of Aspen Mountain and on the east face of Richmond Hill.

As affected by the Sawatch upheaval, these beds wrap around the Archean mass, resting against or dipping away from it at varying angles.

The quartzites and limestones cross the valley of Roaring Fork from Smuggler Mountain to Aspen Mountain, striking northeast and southwest, dipping northwest. The angle of dip is about 45°, varying from a minimum of 30° toa maximum of 60° in " flats" and " steeps."

The Ore Bodies.

The Lower Carboniferous "blue limestone" is compact, homogeneous and composed of pure carbonate oflime. The "brown" or "short" dolomitic limestone is of a dark gray color, finely crystalline, finely granulated and traversed in every direction by a network of minute veinlets containing iron salts, wiiich, when oxidized, color the surface a rusty brown. The oxidation along these minute veins makes the rock break easiiv into dice-shaped fragments giving the a a"crackiy" structure, hence its local name of short ime.

Ore Distribution.—The outlines of the ore bodies cannot be detected by the eye, owing to the gradual transition from ore co country rock.

The ove is not confined to the brown dolomite below the so-caiied contact, but several ore bodies extend 20 or 30 feet above this contact into the blue limestone and in some cases follow the lines of cross-fracture entirely across the blue limestone.

The ore is not confined, either, to a definite plane or contact between two dissimilar beds of limestone and dcoiomite from which its solutions have eaten into the underlying dolomite, for in the first place there is not one single contact, but many; and if this so-called contact constitutes an essential condition of ore deposition, there is no reason why it should be confined to the one and not found in the others where the rocks have the same composition. Again, ore-bearing solutions would not be likely to eat upwards for any great distance from the contact plane if they entered the beds along this plane.

This so-called contact plane is well defined on Spar Ridge and continues down with the dip in the underground working, but ore bodies occur above and below it.

The rock thus mineralized is dolomite in most cases, but it is none the less above the true bedding plane called the contact.

In other parts there has been fracturing across the beds as shown by a vertical breccia of limestone fragments with a cement of iron oxide and manganese.

Over the ore bodies are lines of open cavities following

the lines of cross-fracture, through which the ore solutions passed which deposited the ore bodies. These caves are now being hollowed out by water descending from the surface dissolving the limestone in the roof and flowing off along the floor, depositing a mud of silica, alumina, lime, magnesia and iron oxide.

Hence this contact is not necessarily the only ore channel of the district, and other channels may be sought for.

Portions of the ore bodies have been formed by solutions percolating through cross-fractures and spreading out between the parallel bedding planes.

This would happen if these solutions derived their metals from the overlying porphycy, for it is separated from the limestone by argillaceous shales which would be impervious unless fractured across the bedding. The analysis of the lime mud at bottom of the cave shows by its preponderance of alkalies, which do not exist in the composition of either brown or blue limestone, that the waters dissolving it came from the porphyry. The waters brought both alkalies and silica from the porphyry, and probably the iron and baryta.

Dolomitization.

This is a secondary process upon the blue limestone by magnesian waters, which is proved by irregular tongues of dolomite extending up, into and across the blue limestone. The lenticular bodies in the Durant cliff point to the same fact. The crackly structure of the brown lime results from the replacement of a molecule of lime by a molecule of magnesia, involving also a contraction in volume of the rock itself, which would cause it to separate in angular fragments, the intersections filled by material more soluble than the rock itself. ;

The magnesian waters may have been connected with those which brought in the vein materials.

In the ore bodies the partially mineralized rock on the borders of the ore is changed to dolomite, hence dolomitization either preceded or accompanied ore deposition.

Mr. Emmons suggests as probabilities only, that the porphyry intrusion preceded the faulting;

That the ore deposit followed the intrusion of porphyry and also the principal faulting movements;

That small movements have taken place in recent times both in the strata and contained ore bodies since the oxidation of the latter; that at the time of the great faulting, the beds may not have attained entirely their present position.

In the vicinity of Aspen Mountain ore bodies, the strata appear to have been synclinally folded and faulted between the main Archean area on the east, and a mass of granite at the western extremity of the mountain, thus producing a second series of oppositely inclined beds, also containing a few ore bodies. Intrusions of altered eruptive diorite occupy a prominent position in the intervening trough and may have seriously faulted or dislocated the strata in the depths. The bulk of the Aspen ores are largely oxidation products of argentiferous minerals with true silver minerals, associated with calcspar and baryta; it is a "dry ore" requiring to be mixed with silicious lead ores before it can be treated. Such rich ores as polybasite and brittle silver occur also.

A great deal of the ore consists of fine grained steel galena, very rich in silver.

Aspen As A Prospecting Ground.

Aspen again is an example of a region that had often been skimmed over by the prospector and abandoned before the final thorough prospecting revealed its great riches. Years ago some prospectors found signs of " float" and "blossom" cropping out under the blue limestone of Spar Ridge. They even went so far as to sink an incline of a hundred feet or more, but though they found ore, its character was so low grade, that the mine was for a long time shut down and practically abandoned. Then an enterprising individual conceived the idea of boring down on the sloping back of the limestone in the adjoining Vallejo gulch, to tap the ore body, already discovered along the outcropping, on the underside of the limestone. At about 50 feet deep the limestone was pierced, and an enormously large and rich ore body was discovered. Itamediately the original locators began again with all speed to push on their incline, and then originated the celebrated " apex and side line" lawsuit. The original locators had the apex on the outcrop. They therefore claimed the'whole mountain,

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and tried to drive out the side line men. Finally a compromise was effected, but that boring down on the back of the limestone and its discoveries led immediately to an army of prospectors examining the mountain, and it was astonishing how many ore deposits were discovered in a region that was supposed to have been prospected and given up as no good. Of course Aspen is an example of "richness with depth," A dangerous precedent and encouragement to that often ruinous policy of running long cross-cut tunnels to cut an ore body at depth, which has only proved indifferently good near the surface, on the fallacy we have before alluded to, of the improbable probability of " richness increasing with depth."

An Example Of Prospecting.

Now supposing our prospector was the first man to enter that region years ago. What signs were there to lead him to think it was a good prospecting ground? Supposing him to be fairly versed in geology, he would have noticed, as he came down over the Sawatch range, that the Paleozoic strata he had. observed as ore-bearing at Leadville, out-cropped also on this western side, together with the "blue limestone;' secondly, he would have noticed the presence of large masses of eruptive rock constituting the Elk range; thirdly, he would observe the region was much disturbed, that the strata were intensely folded, and intensely faulted. All these signs he would have considered likely. Then after following up the various creeks, he would select such spots as where he saw the massive blue limestone outcropping. He would readily find this bed from its relation to the granite and Cambrian quartzite below. He would look for places where porphyry was intruded into the limestone or where great masses of it lay above or in vicinity of the limestone. This would probably have led him, on nearing Aspen Mountain, to give that mountain more than a passing look. He would notice that the strata on Aspen Mountain were very much disturbed and faulted, that a spur of granite, quite out of place, came right up through the middle of the mountain, that strata were pitching in various directions off from this, and moreover that in the lap of this

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fault-fold was avery thick bed of porphyry. He would observe the line of change from the blue uuatets to the dolomite, and at that line he would have prospected and found and followed up the " blossom" at the line, consisting of calcite and baryta running in a rusty line, like the outcrop of a coal seam, all up the side of Spar Gulch, and so he would have discovered the great Aspen ore-deposits, and by following up the indications along the outcrop and locating claim after claim as along an outcropping coal seam, he could have secured practically the whole " apex" of the hill, and become master of the mountain and all it contained; but had he known then the litigation of " side

line and apex" that was to arise, he should have gone further, and located claims covering the side line, on the back of the sloping limestone ridge, leading down into Vallejo gulch. But again he might, like the original first discoverers, have become disheartened with his find on testing the outcropping ore by assay or mill-run, and finding it so low grade near the surface. On general principles in this respect he would have been right.

Now having thoroughly explored the little Aspen Mountain, he would observe that much the same formations crossed the creek and entered into Smuggler Mountain, though much obscured by heavy glacial drift. Here he might have located fresh claims on this hill, and become the owner of the celebrated Smuggler, Regent and other mines with their untold wealth. Thence he might have continued his successful trip, and followed the same socalled " contact" outcrop for mileson to Ashcroft. It must be remembered here, however, that in locating all these claims, whilst the prospector may drive his location stake at every 1,500 feet, he is required, within sixty days after location, to dig a ten-foot hole in each location. As this may be a little difficult for him to do he generally enlists others in his enterprise, to assist him, and enters some of the claims in their names, to prevent the discoveries being jumped by a horde of prospectors who press in as soon as anything is found. Good advice to a prospector, is to keep very still and "mum" about his discoveries until he has well secured them, and to be very careful how he " opens his head" to any one. Commonly a prospector who has "struck it," comes into town, fills up with whiskey, " blows

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it in," and then, " blows it off' all over town about his discovery, and is elated to find himself the hero of the hour. The result is, before daylight the following morning, a hundred men are chasing one another in the direction of his discovery, and before a day or more is over, the mountain is covered with locations as close as graves in a city churchyard, and in a week's time these locations are covered again by a second layer, as the saying is, "several feet deep." .

A boom follows. The offscourings of the country pour in with the saloon, dance hall and gambling hell element. A murder or two follows. Lynch lawtakesahand. Then a horde of real estate men come in, and lots are sold at fabulous prices, and the town is inflated with a population and everything else usually far above the capacity of the mines to support. A collapse follows, and a steady retreat of hollow-eyed, disappointed adventurers. In time the town and camp assume their lawful proportions and business settles down to its lawful regime.

Whilst all this has been going on, and amidst all the fuss and bustle and " hooraying" of real estate " boomers"

and so forth, some prospectors have been quietly trying to

follow up the first desirable indications into the neighboring region, resulting often in an extension of the ore-bearing region. Some of these locations are "bona fide" and valuable. Other "holes in the ground" are dug on the merest pretext of indications to catch the ignorant, adventurous tenderfoot capitalist purchasers, or "suckers." An investor going into the camp at such a time finds a fabulous price placed on every prospect, whether genuine or false. Asa prudent man, he either beats down such prices, or concludes he will visit the camp a little later, when the excitement and inflation has gone down, and when things are on more of a business footing, and something like. the real value of the camp has been found and proved. Of course in such a gambling speculation, by such prudence and delay he may lose a lucky chance, but he has preserved his prudence and escaped being wofully bitten.

Perhaps, in a month's time, the discoveries are found to be merely superficial, the boom utterly collapses, and the dreary sight is seen a little later, of a desolate village, with frame houses and log cabins, and possibly a mill or

two, for mills are sure to follow, lying in wreck and ruin, a home for the owis and the bats; or else the genuine discovery epaty t one or two mines and supports a handful of population legitimately. gain, a region like Aspen may disclose a limited number of very rich ore deposits, but sufficient to support and sustain a fair sized town. But the most important and most lasting discoveries of all are of areas producing an immense quantity of low rade ore such as Leadville. This gives an opportunity or a great number of mines and for the support of a large and permanent town.

Chapter Xiii.

Examining And Sampling Mining Properties, Prospects Or Mines.

A prospector may be, or become, a " mining expert" and be called upon to make examinations of mining properties,

whether prospects or developed mines, so a few suggestions may prove useful.

Mining properties of the precious metals are generally of two kinds, those containing ore deposits in place, such as fissure veins and blanket deposits and placers, the latter being gold-bearing. In both cases, and especially in the former, the character, position and other relations of properties are infinitely varied, so that no hard and fast rule can be given to suit ail cases; certain rules, however, will generally apply.

A mining engineer receives a letter from a company telling him to go to such and such country or region and examine and report on a certain property that has been offered them. Such a mandate is usually accompanied by a letter or report from the owner or parties offering the property, giving the owner's description of the same, or else the report of some expert on it. As a general rule such reports give the most favorable view, and in some cases must be taken "cum grano salis." To the mining engineer they give some sort of an ides as to what the

property may be like. As to its value, etc., that he proposes to find out for himself. The company sometimes asks him to examine with a view to verifying or modifying or contradicting such reports.

The region, the country, the character of the deposits, the local conditions, may in all probability be comparatively new or strange to him. Prior to starting he may make inquiries in mining circles if anything is known about the region or district. If there are any published mining or geolos;ical reports or maps, he will consult these. Finally be starts out with as little baggage as possible, usually 2 small hand-bag, containing a few necessaries; a tape line, geological pick, clinometer and compass and note or sketch book. J%is dress is generally a suit of corduroys, leather gaiters aud strong boots.

As he enters the region by rail or on horseback he notices the main geological features, whether the rocks are granitic, sedimentary, or eruptive. Finally, he reaches the camp, calls on the owner or superintendent, and rides up with him to visitthe mine. If he should "lay over" for the afternoon in the village, he may as indirectly as possible try to pick up any gossip there may be afloat relating to the property. He is at once impressed with the accessibility or inaccessibility of the property, and estimates the probable cost of bringing down the ore to the mill orto the railway track, and observes the proximity or absence of timber and water power. At last he reaches the mine, dines at the boarding house, and is then taken over the premises by the superintendent. His first attention is directed to the surface character of the property, its topography, whether rolling, smooth or precipitous, whether it is high above the valley or near down to it, whether the mine is high or low as regards the water level or drainage system of the neighborhood, whether the property is conveniently situated for worki:ig the mine and transporting the ore, etc.

Accessibility is an important matter. In some regions, such as in the San Juan district (Colorado) for example, mines and prospect holes are sometimes on the top or sides of mountains or precipices, thousands of feet above the valley below, located at spots one would think only an eagle could reach; prospect tunnels, too, are driven where

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there appears scarcely a foothold fora squirrel. No spot, however, seems too inaccessible for the prospector. Ata glance the engineer sees that in a property situated in such a region, accessibility is one of the first and often most formidable problems to be considered.

To some of these mines are long zigzag trails cut in the side of the mountain. The engineer calculates how much the owners of the donkey or " burro" train will charge to bring that ore down to the valley or mill. He argues that a mine at that almost inaccessible height ought to carry a. good deal of pretty high grade ore to pay even for transportation by the "burros," let alone the cost of freight afterwards to distant smelting works. On the other hand a mine whose workings open out within easy access of the valley or railway track, could afford to carry less valuable ore. Then there is timber and water power to be considered, the former for timbering the workings of the mine, the latter for running a stamp mill, or for supplying steam power to the engines of the mine. If there be no water power, and the vein carries free gold, the ore must be carried down to the nearest stamp mill. Ina young or " virgin" property or prospect, the engineer will look out for a convenient site for such a mill, under a developed property; if there be a mill on the premises, he will examine and report on its capacity and suitability for treating the ores. A mill site must, of course, be selected close to some water power. In some districts there is a superabundance of water, in others a serious lack of it, or the supply is meagre at certain seasons, or is frozen up in winter. Some mines are quite dry, but generally they will supply enough mine-water from their workings to afford steam power.

He observes the character and dip and direction of the veins if exposed on the surface, examines any prospect holes on them, and takes a few samples for assay. He will consider the nature of the ore deposits, whether they are in fissure veins in crystalline rocks, or blanket deposits in sedimentary rocks, or contacts at junction with eruptive porphyries. A great variety of local and minor details have to be noticed which can hardly be specified.

Having looked over the surface, he enters the tunnel or workings with the superintendent. As he passes aiong,

Amphitheater & Millsite

PLaTE XC.

Sunnyside Extension Gold Mine, San Juan.

Example of a Rough Hasty Field Sketch of a Mining Property.

pot, the He may suggest the aavisabilthe

latter is likely to call his attention to this or thar s

as especially good, and naturally he rather overlooks

poorer parts of the mine.

ity of taking samples from such favorable spots. The engineer, however, takes little heed, as, if he were to confine his attention to, and sample only, these choice portions, he would obtain an incorrect estimate of the average run: of the mine. Moreover in some cases it is well to be on the lookout, lest these points to which special attention is called by the miner be previously " salted" or " prt up" for the expert, and charged in various ways by rich ore.

Having traversed the workings and obtained a general idea of the position of the vein and ore bodies, and taking an inventory of the amount of development, length of drifts, shafts, etc. (the latter he can obtain from a map of the mine in the superintendent's office, a copy of which he will send to his company) he asks the superintendent to leave him and his assistant and vacate the mine, as he does not wish any one except his assistant to be with him whilst he is taking samples for assay.

Sampling.

Now begins his hard and most telling work, the time and labor depending very much upon the size and amount of development in the mine, or the degree of accuracy necessary. Taking a large strip of muslin, he cuts part of it up into small pieces about the size of a pocket handkerchief, these are to contain his samples for assay, when quartered. Then he takes the remainder of the muslin, or better still an ordinary candlebox, this to catch the mass of small fragments he detaches from the vein with his pick.

Now with a light pick or with a chisel and hammer he begins, either from the entrance or end of the tunnel, to detach small portions of the rock, cutting a rough groove across the vein. Sometimes the tunnel occupies the whole width of the vein, in which case he will have to make a circular groove clear around the tunnel, across the floor, roof and walls as shown in Plate XCIV; the fragments from his work drop into the candlebox cr onto the muslin.

According to the length of the workings or the need for great accuracy, he repeats this operation at intervals which may be every 5 feet, 10 fzet or 20 feet; at intervals of say 20 feet, he masses and mixes together all the samples, breaks them up as fine as he can ona shovel and divides

the result into four parts, throws away three parts and retains one. This he reduces to a fine powder and wraps u in the small muslin pieces, ties it up and seals with sealing wax, marking on it the number and other notes, such as 10 feet from entrance, etc., with an indelible pencil. This work he continues till he has reached the end of the tunnel, which if it be 100 ve long psi i

ive him from 20 feet mn : terval. five little Pirate XCI, sacks of powdered ore Natural ater 5 ge on # Blanket for assaying. As a ae check upon this work and for reference in case of any .accident to or any tampering with his samples in transit, will occasionally take a " grab" sample from his broken

Geological Section Showing Workings and Ore Bodies in Contact Blanket Ore Body, Shaded Portions are All Worked Out,

rock before quartering it. Here and there, too, he may take a chunk of some peculiar rock such as a porphyry or some peculiar streak in the gangue, these he will put in his coat pocket and keep on his person.

It is sometimes important in a vein to find out what rock

or portion of rock carries the most value. For instance, on one occasion we examined a vein said to carry gold clear across its entire width of some 50 feet. Now this socalled vein proved to be a decomposed dyke of porphyry impregnated with pyrites and free gold, and through the dyke ran a net-work of little narrow quartz veins or veinlets. On sampling, whilst we took samples clear across the whole width of the vein, we kept those fragments which came from the quartz veinlets apart from those which came from the porphyry gangue. The result was, we found the

orphyry, constituting of course the main element, to be

arren and the gold to be concentrated in the quartz veinlets constituting a minimum of the width.

So in a vein there will generally be parts richer than

Plano-Section of a Flat Ore Boddy.

others, " pay streaks" as they are called, which it is important to distinguish, also certain metallic minerals in the vein carrying greater values than others. Thus the pyrites, if undecomposed, may prove too poor to treat for gold, or ina silver mine, streaks of gray copper may be very rich, whilst bodies of coarse galena may be very poor. In a gold mine it is important for the engineer, if he can, to find out to what depth surface decomposition or oxidation has penetrated, because in this brown rusty matter will likely be most of the "free goid;" whilst when the unoxidized pyrites makes its appearance the ore is no longer free ore, but must be treated by some process other

than that of a stamp mill, and with the incoming of pyrite the palmy days of the gold mine may be at an end. Boies times, however, though the oxidized brown gossan may play out and succeed to white

quartz, the latter, if it be not too

hard, white and "hungry," may

still continue to carry free gold

init. Again in the veins, with

their descent into depths, greater

or less richness may occur or

different varieties of ore set in,

or absolutely barren quartz, so

if there be shafts or tunnels driven

on oe Ae a distinction hm;

should be noted with descent, as .

to values found at different lev- PrateE XCIV. els, also as to character and richness of the ore above and below water line; the latter corresponds to the average drainage level of the country.

Expert Taking Samples.

Fissure Vein Outcrop on Hillside Showing Surface Workings.

This completes his underground examination. Whilst in the mine he may make a rough sketch or two of the vein showing the general disposition of the ore bodies or any peculiarities. On emerging and carefully securing his samples beyond reach of their being tampered with, he selects

a convenient point, possibly on a neighboring hill facing the property, and takes a general sketch of the property in gee or water-colors (see Plates LKXXIX, XC, XCI and XCII), also makes a pencil sketch and ideal section of the hill, showing the position of the vein and its workings (see Plates XCV and XCVI), the amount of ore stoped out and the amount presumably in place intact; to estimate the latter is often a difficult and uncertain problem. He may make some sort of estimate as to the reasonableness

Hole.

Tumnels

Tunnel 2

PLaTE XCVI,

Cross Section of Vein Showing Workings. Dotted Portion is Ore Body, Shaded is Ore Worked Out.

or not of the price asked and give his estimate; he can form, however, no true estimate of the value of the ore bodies till he has had time to assay his samples, for these are the crucial test of the value of the property.

In writing up his report at his leisure, which will most likely be read at a general meeting of the company, he cannot be too clear, simple and explanatory in his account and its details, as it is to be remembered that the company is likely largely to be composed of men unacquainted with mining and mining terms; he must, therefore, not take it for granted that they know what "stopes," "adits" and "gouge," etc., are, but explain as he goes along, accompanying his remarks with rough sketches to make his meaning clear and put the members of the company as inuch on the ground as possible. We ourselves have found that it is not necessary generally to make elaborate notes

in the field or to write pages of reading matter then, provided we make many sketches and on them put down items such as length of workings, etc., etc. The sketch is generally the notes, and when the engineer returns home, his sketches will recall vividly all he has seen and from these he will write his report. Upon certain matters, however, such as involve numbers, he should be very accurate in writing notes and not trust to treacherous memory for them.

Description Of Plates.

In Plate LXX XIX we have an actual example of a rather inaccessible property in the San Juan, which with Plate XC shows the kind of sketches to accompany a report. In Plate LXXXIX with its section, it will be observed how very high up the mining holes and prospects are perched, in most cases over 1,000 feet above the valley, and again, before the ore can be brought over to the mill, a ravine of a hundred feet deep occupied by a boiling torrent has to be crossed. Some of the properties might be worked perhaps by a suspension tramway thrown across the gulch. In another case a trail has had to be cut in long zigzags of some miles before the bottom of that could be reached. Another disadvantageous feature in this property is the number of scattered veins, none of them very rich by itself; this involves a separate plant or workings for each. One good vein would be better than all these put together. There is fine water power on the property and plenty of timber.

In Plate XC there is one fine rich gold vein easily accessible and easily worked; below it lies a natural basin and abundant water which makes it an admirable location for the stamp mill. This Plate gives an idea of the rough kind of a sketch the expert makes on the ground, which he embellishes and elaborates on his return.

Plates XCI, XCII and XCIII show:

(XCI.) The surface appearance of a "flat" or contact blanket on the side of a hill, such as Leadville.

(XCII.) Cross-section showing the position of ore bodies, the portions worked out and portions probably left in reserve, also the workings of the mine and the geological section, together with a prominent fault.

(XCIII.) Is a somewhat ideal sketch of the probable relations of a flat ore body if the surface matter were removed, or rather if it were opened like a book.

Plate XCIV shows the expert taking samples ina tunnel driven in the vein; the vein in this instance, being a very large one, occupies the whole width of the tunnel; this is not generally the case, the vein and ore body are more commonly observed about the middle of the roof, 1.¢., if the vein is small,

Plate XCV shows the outside appearance of a fissure vein with three tunnels down in it, and Plate XCVI shows cross-section and profile showing the tunel and the ore bodies so far discovered in the quartz gangue and how much has been worked out.

CHAPTER XIV. PROSPECTING IN VARIOUS REGIONS. THE GREAT NORTHWESTERN PROSPECTING FIELD.

In former articles we have dwelt a good deal on prospecting in Colorado and the Rocky Mountains, considering that region as typical and comprehensive, and that if a prospector knew experimentally that region thoroughly, he would be pretty well posted 'or tackling other regions of the West.

The main and general features of geology and of ore deposits are very similar throughout the great West; the differences rather lie in exceptional cases. -

Let us take a general view of the great northwestern prospecting field as a whole before we take region by region. The features that most strike us are the comparative little settlement of those vast areas, the chance of their being comparatively new, and little tried and certainly not exhaustively prospected regions; the vast areas that for various physical reasons have not been prospected at all, and in some cases not even entered by white men. These

are alluring prospects for the daring young prospector who longs to enter some region in which he could say:

I am the first that ever burst Into this silent land.''

We do not like going over old well-beaten tracks. We do not like to meet a prospect hole every few hundred yards, or after following up " float" and other signs, at last to come to the ledge in expectation of great things and find Bill Smith's ubiquitous stake staring us in the face. Much of the Northwest is a kind of untracked region. From the various accounts th. reach us there is no lack of gold in th.se northern regions. The placer deposits are excep-

PLaTE XCVII. Alaskan Prospectors Breaking Camp at Foot of Chilkoot Pass.

tionally rich and large, as we might expect them to be in such tremendously glaciated areas; and the finds remind one of the halcyon days of early California. But there are great difficulties to be overcome, not met with in Colorado or the Rocky Mountain region generally, and requiring great hardship and lots of pluck. There are mighty glaciers to be encountered, networks of great and little rivers to be crossed, a very peculiar climate to deal with, plenty of mosquitoes, vast and almost impenetrable forests to be

traversed, while a thick underbrush and profuse vegetation cover up large area of unknown wealth, So, whilst the prospector of Colorado and Rocky Mountain experience may have found his pick and shovel and pan all that was hitherto necessary, in these new regions he must add to his outfit a canoe, a pair of snowshoes and a sleigh, and in place of the "burro," a pack of native sleigh-dogs, and, above all, he must carry a good axe, or even a long crosscut saw, as often he will have literally to hew and saw his way to fortune. Said a prospector just arrived from those regions: " Prospecting is hard ; the country is heavily timbered, with much underbrush and fallen timber. The prospector has to pack his tools on his back and cut his own trail through the wilderness; when he finds a favorable location he makes his central camp, and works from that. Game is not plentiful. In the veins they find sometimes a 'cap' rock rusty with oxidized iron, broken over and capping the veins. This cap is two to four feet deep. Then the rock passes down into hard unoxidized pyrites. Prospecting is hard and slow, for you have to blast from grass roots. Caps are poor. The best ore is found with depth. The veins in this region have not been much prospected, attention being confined mostly to placer and river deposits. Those veins I saw were rich and narrow, with free milling quartz doubtless down to a limited depth below the surface. There are few, if any, large mines between the Selkirk range and the Rockies. Veins may carry both gold and silver, but principally the former, and that mostly in arsenical pyrites. Galena and silver ores, however, occur locally. In Idaho, on the Snake River, placers are worked on bars at the surface line of low water. The gold is fine, light, and hard to save. At Spokane the river valley consists of barren wastes of sand. The sand breaks farther up between Idaho and Oregon. Banks are low, and long bars are worked which are washed up on bends and islands right down to the water line. The soil is alluvial in this part with no glacial matter. Various machines are used, and pumping plants are necessary, as there is no head or gravity line. In British Columbia gold can be found in nearly every stream. The Columbia River is thirty-five feet between high and low water mark six months of the year. Placers shift and change with every

flood season. The first gold worked in paying quantities is forty miles north of Revelstoke on small streams coming in from the East. Every stream running from the east side contains placer gold as far north as Goldstream, seventy-five miles, The country has been worked and prospected for the last seven or eight years. The altitude of the Columbia is 2,000 feet above sea level and the higher ranges about 8,000 feet. Glaciers extend down to a level of 4,000 feet, and are still working and grinding down gold, and the best pay has been found late

PLATE XCVIII. A Glacial Region Showing bipe cisciers Leading up to Amphitheatres

and U Shaped Canyons.

in the season of October at the foot of the glaciers. The side streams, as well as the Columbia, are raging torrents from June ist to September, but are worked about a month in spring, in April, and in the fall in September and October, and between the thawing out in April and the floods of May. In the fall they are worked in September, after the floods have run off and before the hard freezing of October. This high water is caused by melting snows, by warm weather. Rain, contrary to what might be supposed, lowers the water in the streams because it makes the water so cold on mountain tops that it checks the melting of snows, and the highest water is during clear, bright, hot weather. The snow rather than the rain is the cause

of rise or fall of the rivers. The gold is fairly coarse, and found, as commonly elsewhere, mostly at bed-rock and near the bed or channel of the present streams, also at the bottom of boulder and glacial debris to a yy ee of 20 to 80 feet. As an example of the richest of these placers, and the difficulty of getting it, as well as the enduring pluck of the prospectors, we may cite that of the Last Chance placer. The prospectors worked four years in an endeavor to dig down to bedrock, a depth of only 60 feet, but with a river of water to contend with, and only a few months in the spring and fall available for working. They were drowned out in summer and frozen up in winter. The prospectors made their own wooden wheels and pumps, packed everything over a rough trail 75 miles on mules, They had to make bridges across streams which were liable to be washed away again before another trip. For supplies they would make two or three trips in the summer season. The first season they drifted on bedrock, hoisting the dirt to the surface and washing it in a common sluice box. In one short season in this way they took out $7,000, the following year $10,000, and the next the same. On some of the streams they are hydraulicking, with an old-fashioned canvas hose with brass nozzle, like a fire-hose, with fifty feet head of water-power, stripping the surface for some twenty to thirty feet. Some are working on benches not in well-defined channels and with glacial drift full of immense boulders to contend with.

''In places they work up almost under the present glaciers. The main aim is te get down to bed-rock, often at considerable depth, getting a little pay gold as they go down. Prospectors go off in canoeing parties up the rivers, landing here and there and prospecting the bars along the river reaches. The first glacier I met with was near Revelstoke. 'These glaciers are narrow necks of ice leading up to big basins full of ice. One of these glaciers was 400 feet deep (Plate XCVIII.).

''The Kootenai country lies east of the Columbia, between the Canadian Pacific Railway and the boundary at the end of the Selkirk range. Galena and silver ores are principally found north of Spokane country. The region is steep and rugged like parts of the Colorado Mountains. It is a great region for snow-slides, another peril to the prospector

, but an agency by which rich veins are often uncovered and float distributed. These snow-slides cut lon

swathes through the thick timber and pile up a big bank of debris in the valley below. Several large mines are worked in this district rich in silver, from 300 to 500 ounces to the ton. There is a smelter at Pilot Bay, on the Kootenai Lake, and another at Trail Landing on the west side of the Columbia. Ores are hard, being arsenical pyrites, carrying gold and silver, one to three ounces gold and 10 per cent. copper and some silver. Bars of this ore occur in the granite, and the ore is ' frozen' on to the walls —that is, there is no parting selvage or gouge between the ore and the country rock. The War Eagle and O. K. are shipping between them 200 tons ys day, principally gold. The average is two ounces of gold or $s0 per ton. Bound-ary

Creek as well as Trail Creek report good prospects,and the mineral belt extends south into Washington, but is covered at present by Indian reservations, which precludes prospecting.

he Fraser and Cariboo districts lie west of this region. There are some expensive hydraulic plants in the Quesnal and Horsefly, with 50 miles of ditch on each plant; several

"

thousand feet of steel pipe and large siphons and storied reservoirs, preparing for next season. he gravel banks are 30 to 60 feet deep and average from 50 cents to $2 per cubic yard, so it is said. The company must have good assurance of the great richness of the gravels to warrant so expensive an outlay. The main obstacle outside of the shortness of the season is from immense glacial boulders. These, in all placer mining, are obstructions owing to the difficulty in handling them. They may have to be blasted or lifted out by derricks, and many an otherwise rich deposit has had to be abandoned owing to the insurmountable difficulties from a preponderance of these boulders. On the Fraser, Chinese and Indians wash bars every fall and spring at low water with rockers, sluices, etc., making a living. On the Middle Fraser dredges are at work, costing $75,000 per dredge, dredging up sand and grave! fifty feet below the water surface. In Horsefly country, worked since 1860 successfully, they put down a 'wing dam' or caisson to bed-rock, and clean up well, In parts of Alaska they work the gold gravel out in frozen blocks and pound

it up in the spring, and work 'drift mining' in this way all the winter. The gravel beds never thaw out in Alaska. Throughout British Columbia transportation is by horse, but they use canoes where they have !akes or can go down stream. The streams are too swift to ascend in that way. Leaving the travelled trail, you have to carry things on your back. Trails have to be made, and prospectors carry big cross-cut saws as part of their outfit and saw through the timber and fallen logs." Such is my friend, Mr. L. T. Preston's, comprehensive account of prospecting over this region from his own personal experience of several months. Of course he did not go everywhere and see everything, but the general sketch will give us the best possible idea of what is before the prospector in the great Northwest, principally in Idaho, Oregon, Washington and British Columbia. Alaska he did not penetrate far into.

Prospecting In Alaska.

After our brief sketch of some of the leading features from a prospector's point of view of the Northwestern field, we will take up some of the prominent mining and prospecting areas in that vast region.

Beginning with Alaska, the most northerly, the least explored, the most attractive and unique. A glance at the map shows the outline of its coast to be the most ragged on the globe. The coast line is made up of an intricate network of islands divided from one another by a labyrinthine network of channels, which lead you so far inland that it is doubtful where the island zone and the true continent begin or end. These labyrinthine channels are only paralleled in their intricacy by the network of great and little rivers which seem to cover the surface like the ramification of ditches in a quagmire swamp. It is a land, too, especially near the coast, of great mountain ranges, which, like the other characteristics, are cut up ad infinitum by ravines and canyons;: and lying in the depths of those canyons is the mighty glacier, the key to all this extraordinary sculptured and tattered and river-traversed and canyoned aspect of the region. Alaska, from its extreme northerly position, has been intensely glaciated both by the primeval ice sheet of the glacial epoch and by sub-

7 allie. 140 135 CALIERY ENOINEER AND Midian AR,

Sr ERE TOME ye te sate Se Oe Bet Een g AUR as te wr ee

Pirate XCIX. Mab of Alaska.

Pe Oe a gee

a

sequent glaciers, many of which are still remaining in the mountain fastnesses, or running down into the fiords that open into the sea. These are still doing the work of their predecessors, viz., wearing down mountains, cutting canyons, exposing veins, grinding down gold-bearing rocks, and filling up ravines and valleys and river bottoms with placers and gold bars. Consequently the prospector will expect to find this country the paradise of placers. But, again, the mountains being a continuation of the Great Cordillera system have the same crystalline granite core, the mother of gold, and this is traversed by many eruptive rocks, porphyries, and old lavas, and even overflown in places by modern lavas from "craters" still in a state of active eruption. Here, then, are elements the readers of this book will have recognized as " good sign" to the prospector for finding gold veins and gold and silver deposits, viz., granite, eruptive and volcanic rocks, and much disturbance, heat and metamorphic action. Like all pioneers in a new country, the prospector will most likely begin with placer mining, and end up, it may be, by the discovery of the lead or vein from which the gold came.

Vast areas of gold-bearing territory lie partly in British Columbia and partly in Alaska, known as the Yukon country. In 1887 coarse gold was found on tributaries of the Yukon. At low water these tributary streams yielded large profits, from $50 to $100 per day by sluicing. The rich spots on the low bars were worked out and led to discoveries on Forty Mile, Glacier, Birch Creek and others. High bars are also rich and untouched, owing to the difficulty of getting water on them and the frozen condition of the ground. The largest nugget found was valued at $42. Sonie deposits are covered by twenty-five feet or more of loam before pay gravel is reached. Single clean-ups have been made of 55 pounds of gold and $36,000 in gold dust taken out ina season. On Glacier Creek pans of dirt run from a few cents to $4. On Birci: Creek, remarkable for the number of elephant bones found in its gulches, very rich finds have been made. Prospectors have got as high as $13 tu the pan. The gold is described as like pumpkin seed, yielding $3 to $10, and sometimes under a big boulder or a little stone on bed-rock they could pick up from $15 to $20,

Silver Bow Basin,

The first important discovery of gold in Alaska was in Silver Bow Basin in 1880 in gravels of Gold Creek. The discovery and progress of this district is very instructiv: to the prospector. The first prospectors came on the deposits on the hillside, and soon, as they supposed, cleaned out everything in the Basin. But a Mr. Nowell, quietly looking over things, decided to tap the bottom of the basin

Naty y

vai TAM Mo '

ve

Plate C,

Silver Bow Basin Looking Southeast, Showing Placer and otier Mining Operations,

with a tunnel to be used as a sluiceway and so work the entire basin on a large and systematic scale. The first prospectors on the hillsides exposed numerous quartz veins, and stringers of quartz under the placers in bed-rock. They located a few holes on these veins, but having nothing but an arastra to work with, soon abandoned the vein mining. Several patterns of mills were tried on the flintlike quartz unsuccessfully, till a Webster mill with five stamps and later ten stamps proved a success. The veins

are called " contact vein fissures," the reef having a black slate hanging-wall and a greenish gneiss foot-wall. Between the walls of contact a space of several hundred feet occurs, filled in with schists, quartz veins, and vein matter. The filling is networked with veins from a knife blade to several feet in thickness, according to the Alasku Record, which also says: " The ore in Silver Bow Basin is iron pyrites and galena with zinc blende, antimony, copper pyrite, carrying gold and silver, but richer in gold. In some veins in this basin now silver and now gold predominates. Milling consist in reducing their bulk by concentration without free gold-saving appliances. Where the gold reef leaves the valley and climbs the mountain sides, veins outcrop on the surface. So there was not much difficulty in tracing the reef through Silver Bow Basin to the summit of the divide, where veins were found cropping just beyond the upper break of the glacier. Some of these croppings showed upwards of 48.6 ounces of gold to the ton. The Gold and Curry mine lies north of the reef and is a chimney or up-shoot from the main mineral zone. It shows on the surface for several hundred feet a number of well-defined perpendicular veins running high in gold. Great granite dykes cut through the slates east of Takon Inlet, and run for a long distance down the coast from north to south, belonging to the same general zone of mineralized disturbance."

Sum Dum Bay, Shuck Bay and Basin Reef have all their noted ore deposits, and along the mainland and numerous islands indications of mineral-bearing bodies exist in veins of quartz with "colors" in the streams, while in the limestone of Glacier Bay rich silver ores occur. In Admiralty Island the Willoughby group of veins cut diagonally across a gneissic formation. The veins are from a foot to ten feet wide and entirely gold-bearing.

Beach Sands.

Ruby and black sand are found along the beach at the foot of the Fairweather range for many miles up the coast. They are rich in fine gold, but heavy and bright, amalgamating readily and by sluicing. The deposits come from grinding glacial action in the ranges back of them, streams

carry the sand to the sea, and the surf rocks and pans and separates the heavy material, leaving it in alternate layers and windrows along the beach. The black and ruby sand and gold, being the heaviest materials, naturally affiliate.

Copper River,

The Copper River section is one of romantic interest and speculation. Natives living at the headwaters used copper implements and brought down to the coast chunks of native copper to the Russians, who were thus tempted to explore the source, but ill-treating the natives after their wont, the exploring party were brained when asleep. Prospectors, since, who have tried to ascend, have been intimidated by glaciers, swift currents and rapids, high precipitous banks and other almost insurmountable difficulties. So the upper Copper River is still an unsolved problein.

At the head of Cook's Inlet Russians placer-mined for years. Rich diggings and much coarse gold were found lately at Turn-again Arm. Bothsilver and gold are mined in Unja and Unimak Islands, the ore running from $24 to $143 to the ton. A stains mill here high above the mouth of the Yukon is the most northern mill in the world.

Discovery Of The Treadwell Mine,

The discovery of the Treadwell, the most noted mine in Alaska, as told in the Alaska Mining Record, is another instructive lesson to the prospector.

Like many other instances, the discovery of gold in placers led to the discovery of the renowned Paris or Treadwell mine.

On the 27th of January, 1882, prospectors from Juneau crossed Gastineaux Channei to Douglas Island and found pay dirt upon the beach, and the following March they washed on ground called Ready Bullion, and in three days washed and cleaned up 27 ounces of gold-dust. This led to finding another deposit of gold dirt and decomposed quartz, and tn washing the gravel from the bedrock, the great Treaawell ledge was exposed, Peter Erussard, or "French Pete," located the ledge, calling it the " Paris." Placer miners, however, by right or might, held the surface for two years

and washed out amounts estimated at $50,000 to $100,000. Nothing was done by " Pete," as he considered the ore too low grade to work profitably. Then came along one of those characters so often figuring in the history of great mines, a far-seeing man, named John Treadwell, who made a thorough examination of the ledge, its facilities for working and opening up, as well as the character of the ore by assaying, and opened negotiations for purchase. French Pete was glad to let "the worthless thing" go for $400. Treadwell organized the Alaska Mill and Mining Company, and began driving a cross-cut prospecting tunnel toward the veins, and erected a five-stamp mill (not a hundred-stamp mill as is often so foolishly done at the outset) to test by mill-run the true value of the ores before he went further and while the tunnel was being driven in toward the ledge. When the cross-cut reached the opposite wall it showed up, instead of the obscure veins on the surface, a ledge of four hundred feet width of nearly solid quartz! And the little stamp mill proved that the average value of the ore was sufficient to make the mine pay ¢/ worked on a large systematic scale. In 1883 a 120-stamp mill was erected, and in 1890 added chlorination and doubled the capacity to 240 stamps. More claims were purchased, and wharfs and railway tracks and the largest works in the world soon showed that this mine, from the little beginnings of the prospector, had assumed the rank of one of the foremost in the world. The power that drives the great machinery is an 18-mile ditch, extending along the mountain-side, applied to a Pelton water-wheel under a 520-feet pressure, with Corliss engines also added. The 240 stamps weigh each 850 pounds, with 96 drops per minute. The mill has a capacity of 700 tons of ore per day and chlorination of 18 tons of pyrite daily. The average grade of ore is only $2.75, carrying 2 per cent. sulphurets; and the expenses of reduction are at the extraordinary low figure of $1.35. Formerly the ore was quarried out in great pits, dropped down ore shutes into cars, and conveyed through a tunnel by steam and dumped into bins, thence into crushers and batteries; but with deeper working a shaft was sunk 250 feet below the tunnel, and immense hoisting works put in to raise the ore to this level. Two hundred men are employed daily at $3

to $7.

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Mr. H. P. Cushing, speaking of the Treadwell mine vein, says: " The gangue is for the most part white transparent quartz, which has been considerably crushed and thereby rendered granular and opaque. A peculiar greenish rock is also found, poorer in gold than the quartz. Pyrite is evenly, but sparingly, distributed in small crystals. Occasional streaks of quartz free from pyrite occur, and at times pyrite alone constitutes the mass. Horses of slate were occasionally met with, which were taken out with the ore and sent through the mill. The quartz carries a certain amount of free gold, but the main portion is enclosed by pyrite and cannot be amalgamated. Streaks of molybdenite (like graphite) occur, running high in gold. The Treadwell is an example of an ore body in which the content of the precious metals is low, yet the property a good paying one on account of the vastness of the deposit and the ease and cheapness with which it is worked. It is close to water and steamships, plenty of mountain waterpower and abundance of fuel and timber. Six hundred tons are pee daily by 240 stamps in the enormous stamp mill. The outcrop of the vein stood up to the prospector's gaze, owing to its hardness relatively to the enclosing slates, as a considerable peak, and the first mining done was simply the working off of this peak. Later a tunnel was run into the mountain side, cutting the vein, from ich the ore is dumped into cars below."

Chapter Xv. Geology And Mineralogy Of Alaska,

From what we can gather from Mr. Cushing and the Alaska Record, the following appears to be the general geological features of this region:

Along the headwaters of the Yukon are high ranges with lofty snow-capped peaks and many chains of lakes. In the gravel along the sources of the streams gold is found and bars have pac fair wages. In the ranges, veins of silver, copper and lead exist, but, their location being somewhat inaccessible and remote from any ore market, are

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passed over by the prospector, who seeks for placer digging only. Bed-rock is mostly granite, together with some ancient feveatones and crystalline slates and schists. Serpentine also appears (usually a green or purple-streaked rock), showing a continuation to the north of the celebrated serpentine schist and slate belt of California and the Kootenay, Caribou and Cassiar districts. Some ranges are like the highly colored mineral belt of Red Mountain in Colorado. Placer mining on the Yukon is still in infancy.

According to Mr. H. P. Cushing: " The geological structure of this region is very complicated, due to the disturbances which have taken place. There have been two or more different periods of crust movements. The original shales and limestones have been shattered, fissured, faulted and metamorphosed, and at certainly two different periods outflows of eruptive rock have taken place. Great numbers of these fissures have been filled with metalliferous matter. Small veins abound, carrying gold-bearing pyrites, generally in a quartz gangue or silver-bearing galena, and silver sulphurets in a calcite gangue. These veins are found both in metamorphic slates and limestones and in eruptive rocks. In the large majority of cases the deposits are of no value, due tu their small size and prevalent leanness of ore. When they hold out promise for the future, it is more often from the size of the deposit than from its richness."

Vegetation Obstacles To Prospecting,

" Owing to heavy precipitation and hot summers," says the Record, "the region is covered by a dense mantle of vegetation of almost tropical luxuriance, and forests cover the land from water's edge to timber-line, save where cliffs are too steep for a seed to lodge, or a glacier fills a ravine.

"No forest fires have devastated these shores. The scars of winter avalanches are quickly covered with a mantle of living green. For the first 1,000 feet above sea level the forests are choked with densest undergrowth. A jungle of bushes covers the mossy pitfalls of decaying logs beneath. Above that zone is a belt where ferns and mosses riot, and trees spring up slender and straight as columns in a vast cathedral, where there is ever a sombre green light and dew and damp moisture left by tangled clouds.

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"The foot sinks in a thick carpet of moss, and one treads with muffled steps in deference to the sombre silence and solitude that reign in an Alaskan forest."

"At altitudes of 2,000 feet above the sea there are the wildest fantasies in trees—wind-swept, gnarled and crouching hemlocks, borne down by the weight of winter snows (like the stunted spruce at timber-line in Colorado) until what should be a lofty tree spreads out flat like a mat, the stump growing only a few feet high, its limbs elbowing out in all directions and the whole tree covering several square yards of ground. In places these dwarfed forests cover the surface of the country, and the traveler has at times to crawl and wind his way by lying flat on his belly under the low-spreading branches, or clambering up through an opening finds a sudden seat astride a limb or in some other awkward position among the boughs in this novel mode of traveling over the top of these singular Alaskan forests."

A picture of every-day life of the pioneer prospectors is thus drawn by the Record;

"Imagine a group of bearded, roughly clad men squatted under a brush spruce or hemlock around a cracker box, with a pot of steaming mussels between them, with French Pete's Siwash sugar and blackstrap molasses as dessert, and later in the evening gathered around a roaring log fire discussing the results of the day's 'run' in the diggings or spinning yarns of the huge nuggets they had taken in the Caribou district, or of the extreme cold in the Cassiar region. A devil-may-care life was led vy the pioneers with many a hardship, yet through it all they thrived, growing strong and enjoying the hard .ocks incident to a prospector's life. Nor were these hardships and dangers confined to land in this semi-aquatic country. In trying to reach the coast, parties were blown ashore and their canoes wrecked. The sole resources of many of these men consisted of a sack of flour, a side of bacon, a few pounds of beans, a pick and shovel, and canoe. But they were not discouraged, for they knew that gold lay in the basin above them, and they set to work cutting down the monarchs ot the forest and building cabins for their shelter during the long months of approaching winter."

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Chapter Xvi. British America,

The most reliable account we have of this great sh. gr is from the Canadian geologist, Mr. G. M. Dawson, and in it we shall see much that will remind us of Alaska and of other regions of the Northwest as well as those bordering on the Pacific coast. There is a family likeness between all these, owing to the comparative similarity of their geology. British America, like Alaska, is traversed by the same Cordillera system of mountains, and in the second place has been glaciated like Alaska, Hence it is a region of fissure veins and of placers. There is scarcely a stream in British Columbia that will not show "colors." The variability of the product depends on the season; the great winter snowfall or heavy rainfall retards work in clearing deep claims from water till late in the spring.

The general distribution of alluvial zold indicates that several rock formations produced it in greater or less quantity, though it is only where course gold occurs that the original gold veins may be supposed to exist in the immediate vicinity of the deposits.

Colors travel far on beds of rapid rivers before they are reduced to invisible shreds. Glacial drift also distributed the gold widely. The formations are talcose and chloritic (#.e., greenish), or blackish gray slates and schists much altered by heat, they appear to be the prolongation north of the richest gold-bearing rocks of California. Denudation of these veins concentrated the gold in placers.

The noted Caribou district is a high plateau cut by V- shaped canyons, whose lessening slope is concealed by gravels which increase in thickness till the valley becomes U-shaped or flat-bottomed, through which streams flow tortuously and gently. The banks are densely clothed with firs and the country covered with drift.

Shallow placers, as usual, first attracted attention, and. later, deep diggings in due order were attacked and found most profitable. Williams and Lightning Creeks yielded the greater part of the gold of Caribou, being well suited

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for dee,' work, having a hard deposit of boulder clay beneath the beds of the present water-courses which prevents the access of much of the superficial water to the workings below. The rocky bottom of the vailey is followed beneath 50 to 150 feet of overlying clays and gravels, the course of

PLaTE CI,

British Columbia Gold Fields. cAfter Locke.)

the ancient stream being traceable by the polished rocks of its bed and coarse gravel and boulders filling its channel. The richest lead of gold is found in the hollow of the rocky channel, but following the rock surface laterally, side ground rich enough to pay well is found fora greater or less width, Old stream courses of Caribou pursue the

same direction as the modern rivers, crossing often from side to side of the valley with different flexures, but never leaving the line of the old and modern valley or crossing it as in California. We may take the Van Winkle mine as a type. On reaching the buried channel a shaft is sunk on the down-stream end of the claim in the sloping side of the valley to bed-rock slate. The shaft is continued toa certain depth in this, and then a drift is started at right angles to the course of the valley. The right depth is estimated by that found in other workings. The old channel is struck in such a way as to enable the subterranean water collecting in it from the whole upper part of the claim to be pumped to the surface by the shaft. The old channel, once reached and cleared of water, is followed up its slope by the workings to the upper part of the claim, and where paying side ground occurs it is also opened. The richest pay is obtained in the rock channel of the old stream, but where this is much contracted the force of the water has swept the gold away to those places where its width is increased. The hard rocks retain their polished water-worn forms, but the slates are rotten to a considerable depth, and on cleaning up on the bottom a thickness of one to two feet is taken out with a pick and shovel and sent up to the surface with overlying gravel for treatment.*

In the central channel most gold Mes directly on bed-rock and only occasionally in pay streaks or gravel above tt for a Jew feet.

The side ground is worked up from the channel in successive breasts parallel to it. The lowest layers of gravel contain many boulders of quartz and slaty fragments fallen from the hillsides. Water is the main difficulty met with, the workings being annually filled by spring floods. In working over the deep ground in early days in the Cariboo district much was left that would even now pay handsomely, but cannot now be found on account of the treacherous nature of the moved gravel (a lesson, first, that old carelessly worked placers may pay to work over again; secondly,

Rotten rocks, especially slates or schists below placer gravel, are favorite repositories for gold in placer mining, and the prospector should never stop his search till he has dug down well into this rotten bed-rock.

the difficulty of working old ground, new firm ground being far easier; and lastly for prospectors to work a placer scientificaily and exhaustively before they abandon it).

In this as in most other gold-bearing countries the placers have led later to the discovery of veins. Several of these veins have been traced for miles. The gold occurs associated with iron pyrites and galena, through crystalline masses of which the gold is sometimes strung.

Kootenay District.

This district is rugged and mountainous, comprising the south portion of the Selkirk range and the Columbia or gold range. Between these ranges are astring of lakes. The ranges are not very continuous. The rocks are mainly massive granite, in places overlain by stratified rocks. The ranges average 8,000 feet above sea level. The country is densely wooded. Two long, deep valleys traverse the district north and south, one occupied by the Columbia River and Arrow Lake, the other by the Kootenay lakes. The lake discharges into the Columbia.

Geology.

The oldest stratified rocks are mica schists and gneisses and some crystalline marbles and quartzites of Archean age. Overlying these at Hot Springs are gray and green schists unconformable and newer thanthe Archean. Over these are massive gray limestones changed locally into white marble with conglomerate below. The green schists are composed of volcanic detritus made schistose or slaty by pressure. The thickness of the series is 32,000 feet.

West Kootenay is of massive granite with many eruptive dykes. The granites are of intrusive eruptive origin, and later than the stratified rock which they have altered by their heat at the contact. They areclosely connected with metalliferous veins or stratified rocks deposited at the time of their intrusion. These new eruptive granite dykes of a reddish color cut the older gray granites (as at Cripple Creek, Colorado). Most of the mines are in the stratified rocks. few veins traverse a hard,dark-gray mica syenite (a rock not unlike granite), and are gold-bearing associated'

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with iron pyritesin quartz. Those in stratified rocks carry galena, blende and pyrite, and are low grade in silver. Such are the Hendryx and Hot Springs mines. The richer ores at Hot Springs are in green and gray schists and limestones. The richness is due to the influence of country rock and proximity to the granite. Stratified rocks containing the ore deposits of Toad Mountain are surrounded by granite. Alteration of rocks is due to the heat of the granite. So the country rock consists of altered old volcanic material derived from the detritus of an eruptive porphyry. Greenish-gray rocks spotted over with coarse porphyritic white crystals of plagioclase feldspar and black augite crystals are characteristic of the ore-bearing zone.

The Spokane Mine occurs near a wide belt of quartz and a dyke of eruptive andesite lava. In the " Number One" the rock is limestone with veins cutting across it north and south and veins traceable for miles. Ores range from 20 to 300 ounces in silver. The richest deposits are in lime- - stonesand black clay slates. The ore is principally silverbearing galena decomposed in the limestones to carbonates for some depth, together with native silver and gray copper occurring in irregular pockets and impregnating the limestone by substitution, as at Leadville, Colorado.

The Cassiar mines are worked at great disadvantage in an Arctic climate with the soil permanently frozen, with a short season of floods disastrous to mines.

The Peculiar Gold-Bearing Rocks,

On Leech River are some persistent gold-bearing rocks found through British Columbia, showing a great area and extent of these peculiar rocks. In the southern part of British Columbia these rocks are black slates and schists traversed by quartz veins. It is from these mainly that the placers derive both their material and gold. In prospecting the extent and distribution of these slaty areas is important, though only a portion of the streams flowing over them carry gold in paying quantities. Still, when once the prospector has become familiar with these rocks he keeps to them and avoids other and barren regions.

The slates are sometimes calcareous, micaceous and graphitic. Probably a small quantity of organic matter in

the sediments from which these rocks were made may have aided in precipitating metalliferous matter and accounts in part for their richness. Their fissile character later rendered them easily permeable by waters which have concentrated the minerals of economic value with quartz and other crystalline minerals of secondary origin in the veins. Geologically this set of strata appears to lie between the Carboniferous and Mesozoic rocks and may be metamorphosed Triassic or Jurassic strata. The group runs all along the west coast from California to Alaska, and a knowledge and recognition of them as the gold-bearing series is of great importance to the prospector. The rapid character of the Fraser River has distributed the finer particles of gold throughout its entire course, though the heaviest, coarsest gold is found in that part of the river occupied by the slates. Where the slates are absent it is derived from the igneous Tertiary rocks, volcanic tuffs, breccias, and lavas, which often yield gold placer matter just as certain volcanic andesites and breccias carry gold in Colorado, and are worthy everywhere of examination. Fine gold also was carried far by the ice and currents of the glacial period. On the Tranquille River the gold is scaly, and with it are particles and scales of platinum of the same shape as the gold; the same metal occurs in the beach sands and some of the placers of California, though no platinum in place has been found on the Pacific Coast, Besides the gravel in the bottom of the stream an older series is exposed 100 feet above it interstratified at the top with a white silt deposit. This deposit is a delta formed by the Tranquille when the water of the lake was at a. higher level, in times following the glacial epoch.

The gold is derived from eruptive rocks and slates, and the best paying ground is where the creek crosses a belt of soft slates. In some cases the pay is derived from a cement consolidated by calcareous matter resting upon rotten slate. Gold is found in gravels resting on the surface of the older rocks in irregular pockets and uneven hollows, and again it is not till these gravels are found spreading more widely and in thicker masses over the Tertiary beds that the richer gold deposits occur. The rocks underlying the Tertiaty formations are decomposed and shattered and pass upward into a clayey breccia followed by clays and shales.

The natural history of Cherry Creek is instructive as typical of how placer valleys and deposits are formed.

The actual valley of the stream is at the productive part a narrow depression scoring the bottom of a deeply rounded valley. This valley existed and carried a stream like the present in pre-glacial times. When the glacier from the gold range retreated, leaving the valley blocked with morainal matter and boulder clay, the stream again began excavating its bed down the valley. Soft materials were rapidly removed. The stream at first changed its bed frequently, but at last subsided into the deep narrow valley in which it now flows, cutting a new course in the rock of the wide valley and leaving the old channel yet buried with drift on one side of the present valley.

The best paying claim is situated on a little bench 30 feet above the stream. Indians obtained gold from the veins by lighting fires over them and dashing cold water on the heated rock, thus disintegrating the rock and exposing the metal.

Placer grounds extend over 100,000 square miles of Lower Canada. The gravels are generally covered by a layer of vegetable earth or by a bed of clay. They lie on Lower Silurian diorite and serpentine gold-bearing rocks, as in the Ural Mountains of Siberia; hence Russian engineers consider that the gold originates from the rusty quartz of the crystalline schists in the vicinity of serpentines and diorites. Diorite in appearance is commonly a greenishgray rock speckled over with little white crystals of feldspar and often too with crystals of hornblende or mica. From the alteration of the hornblende it derives its greenish-gray color, and hence is often called "greenstone," while its speckled character would name it by miners as a porphyry. Diorite is in many countries an accompaniment of gold, or gold-bearing, particularly in Northwestern America, where it is often associated with serpentine. The latter is commonly a green streaky rock like green marble, and is often the result of alteration of volcanic rocks and others containing magnesian silicate minerals; hence the frequent association of serpentine with eruptive rocks. Both serpentine and diorite are important factors in the vold-bearing zone of the Northwestern and Pacific Coast areas,

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Where the Chaudiere River makes sharp turns, gold is found in cavities and fissures of the clay slates, which run in parallel ridges and are uncovered at low water, when miners break it up and search the slates to a depth of several feet. The fissures are filled with a clay gravel which carries the gold. Many hundreds of dollars have been extracted from between the layers of slate. The gold is sometimes tarnished by a black coating of manganese. At Devil's Rapids the gold liesin a bed 200 feet thick of a hard alluvial conglomerate cemented by clay. The Des Plantes River runs over serpentine, diorite, and schist yielding grains of gold mingled with black sand. The gold occurs in the re-entering angles and cracks of the diorite. Insome streams in Lower Canada most of the gold is extracted from fissures in the sandstone bed-rock to a depth of five or six feet. In the joints and lamina where gravel has penetrated and indurated, gold is foundin the largest masses in abundance. The worn appearance of the gold implies that its source is remote. When gravel lies on blue clay with boulders in it in this region, it is poor, but becomes richer when resting on bed-rock. In two layers of gravel separated by a stratum of clay the lower only is gold-bearing. These clays are barren but contain cubic pyrites, pebbles, black sand, and garnets. The layers of gold-bearing alluvion are not continuous, but occur in sheets or belts of variable extent and thickness. The gold, too, occurs in patches, isolated or remote from one another. A week's work at a good spot is often better than months in poor ground. Quartz veins in Lower Canadarunin the direction of the stratification, northeast by southwest, often obscured by vegetable soil, and require prospecting by trenches as at Cripple Creek, Colorado and many other regions.

The veins contain pyrite, zinc blende, galena, and native gold. The pyrite and blende carry the gold, which is derived from lower Silurian rocks. These veins occur in soft blackish schists and greenish-gray rocks, or in fine-grained felsite trap or indurated volcanic ash with seams and stains of green epidote. The latter is a grass-green mineral often found associated with quartz and mineral veins, and with iron, garnets, and hornblende. It is a secondary mineral derived from iron-bearing minerals such as hornblende,

etc. Sometimes it occurs in distinct crystals, but more commonly as a grass-green staining to the rock. The prospector is likely often to come across this mineral in his searches among the crystalline rocks and veins. It is no particular sign of the presence or not of precious metals, but a common accompaniment of them; it is much lighter, more grassy-green than copper carbonate.

Gold In Slates,

In all parts of the slaty belt quartz veins abound. A band of slates is often characterized by small thin streaks of quartz and lenticular bunches through all its layers without showing any well-defined large veins. The quartz holds little pyrite. Good pay is obtained by cleaning up the bed of the river itself and by crevicing in potholes, pockets, fissures, or slates, or sides of the valley. In Leech River, the gold was generally diffused in small quartz seams through certain parts of the slaty rocks, of which a great mass was worn down in excavating the valley, leaving the heavy gold by natural process of concentration in a narrow line on the bottom of the excavation. Copper ores and gold in some localities are associated, especially where diorites, green slates, and dolomites are extensively developed. Gold has been obtained from "gossan," or surface float filling the crevices in a cavernous, rusty dolomite.

Dolomite is a magnesian limestone, the carbonate of lime of an ordinary limestone replaced in a great measure by carbonate of magnesia. As magnesian carbonate takes less place or volume than carbonate of lime, the replacement often gives by shrinkage a minutely cavernous incoherent structure to the dolomite limestone. And just such a structure is that of which metal-bearing solutions are liable to take advantage and to deposit in it their metals; as, for instance, the silver-charged dolomites of Leadville and Aspen, Colorado. A gold copper vein at Palmerston carries much copper pyrites; it is associated with dark greenish hornblende rocks and slates, and the gangue is a translucent quartz divided into layers or ribvons by strings of iron and copper pyrite and calcspar. The last mineral is sometimes, but not commonly a gangue of metalliferous veins.

Gold veins occur near Lake Ontario in fissures in syenitic granite, that is, in granite containing a good deal of hornblende as well as mica, with micaceous and talcose slates forming the walls and horses in the veins. The talcose or soft, greasy, greenish soapstone-like slates result from chemical decomposition of the syenite along the sides of the fissure, apparently a sort of indurated gouge or selvage to the quartz vein containing gold-bearing arsenical pyrites. These veins are irregular in thickness and quality, the fissure opening out wide in some places and pinching in others, and the ore richer in places than in others. Diorite is associated with some of these veins like the " porphyry contacts" of Colorado. All over the glacial drift of the plains from Lake Manitoba to the Rockies gold is more or less present, and appears to have been washed from the shingle terraces along the eastern base of the mountains where it is believed the precious metal is most abundant. On the Saskatchewan small red garnets and black or magnetite sand form the bulk of the residue of the pannings. The gold is not derived so directly from the mountains themselves as from the drifts of granitoid pebbles spread over the face of the country, derived from the denudation of the great belt of Laurentian rocks extending from the shores of Lake Superior northwest to the Arctic Sea, Ia New Brunswick gold is found in the pebbles composing the Carboniferous conglomerates of the coast. Gold veins also occur in diorite; some are short gash veins.

Newfoundland And Nova Scotia Gold.

In Newfoundland quartz veins occur in serpentine of the Lower Silurian, and where serpentine is absent there is no ore. It occurs in pockets rather than veins. Small veins intersect one another, forming a knot or bow, at point of intersection often rich in gold. The rock is a dark-green chlorite schist. In Nova Scotia the gold-bearing series is in Cambrian greenish-gray grits and sandstones with bands of shale overlaid by black earthy pyritous slates and sandy beds much crumpled and contorted. The lodes are in the most metamorphosed quartzitic rocks and in soapstone with rutile and garnets. These strata are thrown into waves (Plate CIII), the elevated points of which having

Leen planed off show the gold-bearing quartz lodes in the form of irregular ellipses. Gold occurs as spots and bunches up to 60-0z, nuggets. The leads conform with the stratification. It is alleged that much of the gold drift of Nova Scotia has been carried into the Atlantic to form the sub-

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Plate Ciii,

Contorted Gold Veins in the Caribou District, Nova Scotia, CLocke,)

marine banks of the coast. Copper Lake is a curious instance of gold occurrence. The lake was drained. A layer of tough clay and glacial drift was met underneath the mud and vegetable matter, and in this under-clay small round nuggets were often found. Irregularities in veins sometimes disappear with depth. Lenticular veins may die out before reaching the surface, but with depth may resume.

Chapter Xvil California,

California has many characteristics common to the Northwestern field,—the same general mountain features, the same peculiar set of gold-bearing strata, and the same characteristic placers, some of which are a little different from placers in general by being covered with heavy flows of lava. The country is divided into three great belts: One the Sierra Nevada range, a second 50 miles west of this main axis, principally including the great valley system, and the third the Coast range. The Sierra is the belt of intrusive granite and of Mesozoic strataintenscly altered by heat. The great valley is the belt of alluvial deposits, and the Coast range is a fold of Tertiary and Cretaceous rocks also much crystallized and altered by heat. The Sierra is the belt of the origin of the precious metal in

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place in veins; the Coast ranges, of quicksilver, cinnabar, asphaltum, etc.; the great valley, of gold-bearing alluvia which also cover portions of the Sierras. In the Sierras volcanic activity has ceased, but on the Coast ranges solfataric action is still apparent. The coast ranges are of shales and sandstones, and limestones altered by metamorphic heat into crystalline quartzites, slates, and sometimes serpentine and marble; volcanic rocks appear often, and granite but rarely. The slates are changed into jaspers and serpentines which carrv the cinnabar.

In the Temescal range, which is composed of granite, porphyry and metamorphosed sandstone of Cretaceous and Tertiary origin, is one of the few localities in North America where tin has been discovered. Large areas of the Coast range are covered with lava, pumice, and obsidian. Hot springs and sulphur beds occur.

The geological structure of the Sierra Nevada, according to Bowie, is:

1. A central intrusive core of granite flanked by

2, Metamorphic slates of Triassic and Jurassic age composing the gold-bearing slate formation, overlaid by

3. A covering of Cretaceous, Tertiary, and Post-Tertiary deposits which are either river deposits forming the gold placers, or sediinentary volcanic layers, or lava or marine formations.

Granite occurs in the northwest part of the State, disappearing in the northeast under great lava beds, and reappearing in Butte and Plumas counties, increasing in mass and importance to the south.

The gold-bearing slates are metamorphic, crystalline, clayey chloritic, and talcose slates occupying the western slope of the Sierras, with occasional areas of granite enclosedinthem. In this slate occur the veins of quartz carrying gold. Some veins are very large and traceable for vast distances; others are small and short lenticular bodies.

Diorite ard serpentine, as throughout the Pacific Coast field, are often associated with gold veindeposits. Basaltic tufa is generally of a light greenish or yellowish color or rusty, and contains angular quartz pebbles. The gold deposits of sand and gravel rest upon the tufa, and in Stanislaus County are not capped bylava. Bones and teeth of the

elephant are found. An average section of a placer in this district is as follows:

Coarse red granite gravel and sand.

Sand and pebbles.

Loose yellow sand.

Dark colored gravel containing fragments of slate, granite porphyry, greenstone, serpentine, quartzite, diorite, materials derived from the Sierra Nevada.

Total, about 50 feet.

The greater part of the gold is confined to the lower stratum of gravel next to bed-rock associated with magnetic iron (black sand) and platinum.

Lava covers many thousands of square miles of Northern California and Southern Oregon, and buries up many a valuable area of gold placer ground, The latter are limited to the North in accessibility by the overwhelming shell of lava. Sedimentary layers of fragments of lava carried to a distance by water and deposited as breccia or conglomerate of volcanic ashes are found interstratified with the gold gravels orcovering them. The gravel deposits vary in texture from a fine pipe-clay to sand and coarse gravel, and from that to boulders weighing tons. These deposits were laid down by the action of Tertiary rivers which had the same general course as the present streams on the west slope of the Sierras, but whose channels were wider and slopes greater. These rivers eroded the gold-bearing slates with their quartz veins and concentrated the gold in deposits often 300 feet wide at bottom and several thousand feet wide at top, with a depth now varying from a few inches to 600 feet. Volcanic eruptions have in places covered these deposits with lava and tuff hundreds of feet deep. Quantities of fossii wood and remains of land and water animals found in these deposits attest their river fresh-water origin.

The top gravel sometimes nays but not generally. Gold may also be found at times literally in grass-roots entangled in the roots of the plant. But the best pay is generally near or at bed-rock. Where bed-rock is of slate upturned on its edges, gold frequently permeates it a foot or two, so a miner does not stop till he has dug up some bed-rock. Fine sand is generally poorer than coarse gravel. Deep

pot-holes filled with sand are often but not always rich. All this goes to show that to prove a placer a system of sluicing should be adopted which bottoms the entire deposit.

Beach Mining.

Beach mining is carried on in various places along the coast especially between Cape Mendocino in California and the Umpqua River, Oregon. The beach sands contain gold in a finely divided state in layers (one or two feet deep) of magnetic iron sand, which by concentrating action of waves and tide is separated from the lighter quartz sand. By the wash of the water the gold layers are sometiines exposed and sometimes covered by the non-auriferous material. With the gold platinum is found in flakes, like the gold only more compact. As the tides continually alter the position of the gold-bearing layers, it is necessary to prospect daily for the richest spots, which are generally covered at high water. The sand assays from $5 to $10 to $30.

Deep Lead Mining And Mother Veins,

Gold, in this State, is often mined in deep deposits overlain by lava, by tunnels and drifts. Where a pay channel has been found or is supposed to exist a prospecting tunnel is driven in to find and develop it. Whenever the nature of the deposit admits it, hydraulicking is the best method. The great mother veins or congeries of veins of California are extraordinary phenomena. That of Nevadaand Amador is an irregular disjointed outburst of quartz extending 80 miles from Mariposa to Amador. Ina series of lenticular bodies separated by barren intervals, it occupies a width of 12 miles, and the mines are located on intermittent outbursts of quartz. One of these veins 8 to 4o feet wide suddenly pinches out in 500 feet. Free gold averaging $10 to $15 and pyrite are the constituents. These veins are in slate. In the higher portion near the junction of slates and granite are isolated patches of ancient gravel capped with lava. Some of these veins change with depth into tellurides as at Cripple Creek, Colo. In El Dorado the belt of goldbearing slates, etc., is 30 miles wide. Some mines noted for free gold near the surface ceased at 250 feet, passing into

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barren, poor quartz. Diorite, slates, schists, greenstones, syenite and serpentine make up their gold formation. The greenstones seem responsible mainly for the gold here. Gold is generally sparingly distributed in the gangue, but rich in the pockets at intervals. Veins are commonly narrow though plentiful, and demand economic management.

The dolomitic or magnesian portion of the great mother lodes decomposes readily and becomes a rusty cellular " gossan" traversed everywhere by seams of white quartz which carry the gold values. The rich gravel belt is coextensive with the gold-bearing slates and is derived from them. The coarse gold lies nearest the place where it originated. The lenticular veins are rather intercalated beds or bodies between the stratification than true fissure veins. The rocks in many localities are penetrated in every direction by little irregular veinlets. Spots are rich even where not more than one inch thick.

The character of the gold varies in form and vaiue. It is coarse and in flat grains on bed-rock; in the upper part of the bank " flour" and scaly and 50 cents purer than the cease. Lumps occur, coarse and scraggy.

Coarse gold also is generally well rounded and smooth, the finer, more flaky with occasionally quartz adhering to it. If coarse gold is worth $17 fine gold is worth $18 per ounce.

A system of mining is carried on called "seam digings;" this is on decomposed bed-rock filled with irreyular seams of quartz containing gold. 'These rocks are commonly soft slates or sandstones filled with iron pyrites traversed by little quartz veins and serpentines. These veins are like the German stockwerks, a multitude of little veins ramifying in all directions with gold far from uniformly distributed in them, mostly in pockets, In these a miner may make nothing ora fortune, or strike, as one did, a $4,000 nugget. When these quartz seams leave the soft decomposed matrix and pass into hard rock they run out or disappear altogether, and gold invariably gives out. Veins occur as bunches of quartz quite thick or split into eight or ten strings which disappear before reaching the surface. Quite a number of quartz seams found below do not extend to the surface. On the other hand the great mother lode of California outcrops in places like an immense

white wall 60 feet wide. The likeliest vein-stone is seamy, oxidized, rusty, mottled, and marbly. The gangue of some veins is crystalline quartz, semi-transparent and ribboned in such a way as to present the appearance of a succession of layers parallel to the walls, one of these layers or lamina being more productive than another. These bands may be separated from one another by thin layers of quartz differing in color from that forming the seams themselves, or again lamine of slate may divide the vein into bands no thicker than paper. Very crystalline, pure, transparent quartz is "hungry" or poor, while if oxidized and showing the square little hollows left by the cube of pyrite that has oxidized out it is liable to break. Below the drainage line of oxidation the ore is liable to be hard of treatment.

Flakes of gold are distributed in the vein-stone in the vicinity of certain dark-colored streaks parallel to lines of deposits of quartz. When the gold lines a crystalline cavity it is in well-formed crystals. In narrow fissures the crystals are flattened to plates. Besides quartz, semi-opal and chalcedony occur interleaved between layers of quartz, showing clearly their origin from hot-spring action. Some California lodes have been worked to a depth of 1,500 feet without impoverishment. Bodie in Mono County is an isolated mass of porphyry, the centre of a great eruption. There are evident traces of igneous action comparatively recent in Mono Lake with islands of lava. The surface of the mountain is covered with an ochreous earth derived from decomposing porphyry and containing fragments of quartz, jasper and chalcedony derived from the breaking up of various veins and lodes which intersect the mountain, while parallel veins of hard, compact, uncrystalline " hungry" quartz occur on the surface of the hill; at a depth of 50 feet they become softer and are productive. The veins show a fine parallel ribboned structure indicative of their deposition by hot springs like those at Steamboat in Nevada.

Yuba And Other Placers,.

The Yuba placer is a good typical one of a certain kind of placer. It is composed of 250 feet of gravel protected by lava and cemented into a hard conglomerate. The

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colors of the upper and lower portion of the mass differ, due to oxidation of iron pyrites by surface waters staining the gravels red and brown in undulating lines contrasted with the blue color of the unoxidized detritus. The "blue gravels" are highly impregnated with iron pyrites, forming a cement. Isolated patches of fine sand exhibiting false bedding occur in the upper portions and contain much fossil wood flattened by pressure and blackened to coal. When covered by lava this wood is beautifully agatized. On bedrock the grains and scales of gold are very conspicuous and are inlaid so firmly upon the hard, smooth granite bed of the ancient river as to resemble a gilt mosaic. Beneath the lava of Table Mountain, Tuolumne, is a fine-grained sandstone interstratified with seams of clay and argillaceous shale. With these are beds of strongly cohering conglomerate or cement, at bottom of which is the pay gravel.

Deep Placers,

Professor Eggleston, on California deep placers, says:

"The great lava flow filled the deep channels and covered elevations also. The Yuba cuts canyons through the volcanic flow to a depth of 3,000 feet, showing in section: first, lava; second, gravel; and third, slate. The deep leads were found by miners, who could not get hold of the open, easily worked placers, and so were driven to prospect up hill till signs led them to a point underneath the lava. Deposits are sometimes found in basins formed by swelling of the bed-rock. The ancient rivers were on a much larger scale than now; they had "bars," " eddies," rapids, waterfalls, with gold deposited in crevices. There were long barren stretches and pockets of richness. Sometimes there was more than one channel. The problem of drift mining is to find the channels. Some of the best drift mines have been found by following surface placers up to the line of disappearance of gravel and gold; at this point is a channel and place to prospect. Sometimes a depression in the line or under edge of the country rock indicates an old channel and probable presence of gold. Gravels are not confined to definite channels, but old streams sometimes overflowed as modern ones do, carrying gravel and gold with them. In some localities two distinct sets of ancient river chan-ee

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nels have been found, one cutting across the other, very different in character, showing they were formed at different periods. Gravels sometimes cover the whole surface of the country without any apparent defined channel. Channels are subject to irregularities and are sometimes abruptly cut off by faults caused by a movement of the underlying pipe-clay or by erosion of ground beneath the flows."

Prospecting In Idaho.

The southern portion of Idaho is a continuation of the sage-brush and alkaline deserts of Nevada and Utah. The Snake is the principal river. The valley of the Snake isa plain 50 to 100 miles wide, covered by flows of recent basaltic lava (Plate CIV.). From Wyoming County to

' x "71 f Tue COLLISAY ENGINEER AND METAL MIKER.

PiaTE CIV.

Great Basalt Plain of Snake Rivet anes with Recent Cones. (After cke,

Owyhee County north of this plain the country is mountainous. This northern region is well wooded and watered and good for mining. The winters are long and severe. A large granite area occupies part of Southwestern Idaho, which has been greatly disturbed by eruptive action ata comparatively recent date. Dykes of basalt occur and hot springs abound, issuing sometimes from the granite, at others near volcanic rocks, showing that volcanic heat still remains below the surface. The numerous veins in the granite strike significantly in the direction of the ranges in the flanks of which they occur. The fissures containing the veins were inade by the upheaval of the range. The movements in the ground, the fissures, and heat action probably belong to the Snake River eruptions.

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The ores were probably deposited by solfataric hot springs accompanying the eruption of basalt. The living hot springs in the granite are charged with alkalies and sulphohydric acid, and may be called modern solfataras. These occur in the immediate neighborhood of the mines. As we have often before said, solfataric action, whether modern or extinct, is associated with ore deposits. And Idaho seems to be a region of past 2s well as present vein formation due to its volca2ic character. Some of the veins are faulted and their walls slickensided, showing that movements have occurred even after the veins were formed and filled. And veins, like old healed wounds, being weak places, the fissuring again took place along the old breaks.

Boise Basin,

The gravels of Boise Basin cover 30 square miles to a depth of 12 feet, representing an extensive erosion of the upper country by streams far greater than the present limited rainfall admits. They date from a time prior to some of the basalt eruptions, or locally the gravel is covered by a basaltic cap. Some veins are later than the basalt itself.

The mines are mostly in the granite or veins between granite walls, which are numerous, rich, and narrow. Some, like the celebrated De la Mar mine, are nothing more than rich impregnations of decomposed porphyry dykes. Ores carry both gold and silver, the gold generally free or in pyrites or zinc blende. Prospectors should carefully observe the float, the character of the croppings, evidences of disturbance, and especially the decomposition of the country rocks, particularly if that rock happens to be a porphyry dyke. The granite masses are the mother of the gold mainly. The veins here often grow less rich with depth, though strong veins may continue rich to a very great depth, and decomposed gold-impregnated porphyry dykes like the De la Mar are liable to continue rich to as great a depth as the decomposition lasts.

In Wood River district, ores occur in granite and slate. The placer gold gravels are of great volume and extent and have yielded some thirty million dollars. There are three classes of gravel. The bars of Snake River are goldbearing, but the gold is very fine or " flour."

Rich but small placers occur along the Salmon River: small placers are found near the croppings of gold veins, and these veins have been discovered by following up placers.

The deep gravels of Boise Basin are surrounded by mountains and receive no drainage from beyond the basin's own limits, yet it contains 125,000,000 cubic yards of placer material 250 feet deep.

Gravels are spread over the whole basin and occur even on the tops of considerable hills, and are at times capped by heavy flows of basalt as in California "deep leads.' The pay dirt is generally on bed-rock. Large boulders and fossil wood are abundant here as in California placers. It is evident that a great river once flowed through the basin and transported the gold-bearing gravels.

Chapter Xviii. Montana, Dakota, Arizona, And New Mexico.

THIS is a region of granite mountains and the sources of many great rivers. The geology isan Archean granite core with patches of ancient Paleozoic sedimentary rocks. A large portion of this so-called granite is really an eruptive diorite, that peculiarly gold-bearing rock. It is composed of augite, hornblende, and plagioclase feldspar with grains of magnetite. The more modern eruptive rock called rhyolite, usually a light-colored gray or white rock, occurs as well as porphyries. Rhyolite breaks through the diorite granite at Butte City. The prospector sees here the usual good signs for a mineralized region, viz., plenty of eruptive rocks. The vein material is simply an alteration of the country rock along certain places in which calcite quartz and metallic minerals have replaced portions or all of the original constituents. There is no definite wall generally to the ore deposit, at least on one side only. There was no pre-existent open fissure of the same width as the present vein. Gold at times seems merely to impregnate the country rock. A considerable portion of the ores consists of gold-bearing pyrites and quartz sufficiently oxidized to

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melt freely; others require smelting. A good deal of copper ore is present.

The placers have produced richly. The deposits are mostly in open valleys comparatively high upon the mountains, and consist of coarse gravel varying from 5 to 65 feet in thickness. Bones and tusks of elephants have been found in the placers of the glacial epoch. Bed-rock is not always reached, but aclayey seam or false bed occurs, below which the gravel is barren: Alder Gulch is the most noted placer; it has yielded upward of thirty million dollars, For a distance of 15 miles from the summit of the mountains to the Ruby River the pay has been continuous and rich. The ground is worked to profit along the banks as high as the water can be carried, and is known to be rich still above the highest elevation to which the water has reached. In Deer Lodge County, where the first discoveries of gold were made, the ore is in diorite granite. The Butte of Butte City is a rhyolite lava dyke. The ore is not confined to veins, as the country rock often yields pay material for a varying distance from the main ore body. At Heiena the ores are mainly gold-bearing in veins in granite and in slates. The veins are segregations of quartz and metal in bodies lying parallel with the formation. At Big Hole the river for ten miles runs through a canyon cut in gneiss in which are abundant gold-bearing quartz veins.

Prospecting In Dakota,

The Black Hills of Dakota are in many respects geologically an epitome of the great Rocky Mountain system. It is a wooded island rising 3,000 feet above the ocean-like prairie. It is an independent uplift 100 miles distant from the Rocky Mountains. The uplift is oval, about 120 miles long by 50 wide. The central mass is granite with sedimentary rocks of all ages from Cambrian to Tertiary, dipping away from it on all sides. Large veins of coarse pegmatite granite occur in the granite; and eruptive rocks, porphyries, etc., are intruded between the sedimentaries. The hills contain iron, copper, tin, gold, and silver. The deposits in the granite and schists are lenticular in shape and composed of gold-bearing pyrites.

There are placers of stream tin, and also of gold, anda

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remarkable ancient consolidated placer, found at the base of the Potsdam or Cambrian rocks and of Cambrian age. This was formed by the ancient ocean advancing upon the slowly sinking granite island, sorting over the material washed from the land and depositing it as sand, gravel and pebbles as the basal member of these rocks. The particles of gold were derived from the granite veins; it was a very ancient primeval gold placer now consolidated into hard rock as shown at the Homestake mine. It forms the hard cement beds of the miner and is stamped as an ordinary free milling proposition. We have called attention to this before as an instance of what we call conglomerate rock, rather than an orthodox modern placer, producing gold.

Homestake Mine,

In the sketch (Plate CV) the porphyry cap of the Homestake vein is shown. The porphyry flowed sometimes beneath the Potsdam, sometimes on it and beneath the Carboniferous, sometimes it lifted up the overlying strata by a thick intrusive sheet. The lower contact line is the old Potsdam beach. The gold in these ancient placer conglomerates is finer than that in the veins, as is commonly the case with placer gold. The Homestake property or a section 6,000 by 2,000 feet constitutes the gold belt. The deposits were of course originally laid down as beds, but have since been much altered. 'The beds contain a good deal of carbonaceous and graphitic material, which were doubtless relics of organic substances in the placer which may have helped in precipitating the gold and chemically changing the iron that carried it. The ore is not continuous, but in great "shoots" or " pipes" of a lenticular shape ; in cross section the shoots cross the dip. In the Homestake are sheets of porphyry cutting across or parallel with the stratification. The influence of this porphyry on 'tthe lode is good, enriching the bed and by oxidization rendering the ores more free milling.

Mr. W. B. Devereux gives a very interesting and instructive account of these peculiar gold deposits, which he aptly calls "a fossilized placer:"

"The underlying rocks are metamorphosed crystalline Paleozoic schists which contain the gold-bearing quartz

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veins. Resting unconformably on these is a sedimentary formation composed of debris derived from the schists containing fossils of the Potsdam period. The base of this formation is a conglomerate. Gold in early days was found in the lowest stratum of this conglomerate. It was obtained by horizontal drifts, and many hundred thousands of dollars were taken out in a short time. The mines were called 'cement' mines; the conglomerate needed the stamp mill forreduction. This conglomerate merges upward into sandstone or quartzite. It is a mixture of quartz boulders, pebbles and worn fragments of schist with pebbles of hematite. Gold occurs in this both as mechanical and

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Plate Cv.

The Homestake Mine, Deadwood, Black Hills. /, Porphyry ; D, Potsdam Conglomerate; C. Cement Mines ; 5S, Schist.

chemical constituents. The horizontal character of the sediments and the fact that their fossils belonged to salt water types shows they were ocean sediments formed in shallow water where there was strong wave action. These deposits were later overlaid by the porphyry. Ore mined from this ground milled $50 per ton, and the stratum lying next bed-rock was exceedingly rich. Small channels and depressions caused local concentrations, and these channels were followed in mining. The ore was hard and required blasting.

There were the same variations of quantity as in ordinary placer gravels. Local channels showed alternations of rich and poor material due to different conditions of current, and the occurrence of the greater part of the gold at bed-rock about six feet thickness as a rule paid. The

gold was like placer gold in shot gold or smooth rounded grains slightly flattened. The cementing material was iron oxide, and bed-rock gold was often attached to the overlying boulders by this medium. The gold was most abundant with large quartz boulders or pebbles of hematite. The latter nearly always carried gold. Each grain of gold is generally covered with a thin coating of iron oxide which needs a blow to loosen it. The richest ore is not always found in the deepest portion of the channel but sometimes upon one slope. Basins occur in these channels which are rich, They seem to have been formed by whirlpools."

Where the slate was soft cement, gold worked down into the crevices for several feet. The history of these singular deposits appears as follows:

"The gold veins were in existence before the Potsdam period. The Potsdam seas washed away.the debris resulting from the disintegration of the quartz veins and deposited it in deeper water according to its specific gravity; at the same time gradual wave action carried the gold to bed-rock in the same manner as it settles in a miner's pan. The Homestake vein was a hard reef or low island. In time the sediments became an island gradually cementing into rock, until later eruptions of porphyry caused great local metamorphic action. The gold now became partially dissolved and was again precipitated as thin films in the schists below. A period of rest ensued until fresh-water streams cut through the upper strata and disintegrated the matrix of the gold and afforded material for a new concentrating process. This disenveloping process has continued to the present. Gold from the conglomerate found its way to the bottom of Deadwood gulch and was joined with supplies from the Homestake vein and formed the great Deadwood placer."

The gold belt is a zone of slates and schists with many lenses and shoots of ore. Zones impregnated with pyrite pass into quartzites forming foot and hanging walls. Such deposits have to be worked on a large scale to pay, and concentration and chlorination are necessary.

The "contact" gold deposits carry silver also and vary in thickness from a few inches to 10 feet, averaging $15 to $60 in value. They are in connection with igneous intrusive

rocks. In the Potsdam placer conglomerate the gold occurs along the bedding-planes of the rock and in vertical joint planes or impregnating the quartzite and replacing the cementing material of the original sandstone in close connection with igneous rocks. On the surface the iron is oxidized. In the deeper workings a bluish quartzite constitutes the ore containing minute pyrites occupying spaces between the grains of sand like a cement. he ore also occurs in large bodies replacing beds of loose shales which occur in the Potsdam, The porphyry eruption gave rise to hot solutions necessary to collect and redeposit the gold in an available form. The Oro-Fino mine is a crater in Archean granite with vertical walls filled with breccia. The diameter of crater is 150 feet. The breccia consists of angular, worn fragments of slate, quartzite and porphyry, cemented together by pyrite, galena and blende derived from hot ascending solutions, The prospector may notice here certain good concomitants for a rich lode, viz.: the presence of eruptive porphyry and close to it a loosely compacted rock or breccia supplying good places in its interstices for ore solutions to circulate.

The outcrop of the galena deposits is lead and iron carbonate, but with depth sulphides.

Tin Deposits,

The Black Hills of Dakota have long been noted for the occurrence of that metal so very rare in America, viz., tin. Miners in 1875 working for gold found a troublesome heavy black sand in their sluices. Some of this was sent to Prof. Richard Pearce of the Argo Works, Denver, and found by him to be tin. The veins carrying tin in the igneous and granite rocks of Harney's peak also carry gold and pyrites. It is probable that both gold and stream tin were derived from the Potsdam sandstone. The veins in the granite are a chain of lenses. They varyin width, sume being upward of 100 feet. When tin is present one of the mineral constituents of the granite is generally wanting. The vein matter is composed of quartz and mica alone, or of soda, feldspar and mica, or of pink feldspar and quartz,

Minerals Associated With Tin.

The Etta tin vein is columnar and oval, 150 feet by 200. The minerals in it are arranged concentrically. The central portion or core is quartz and feldspar surrounded by albite feldspar and mica carrying tin. Another zone surrounds this with large crystals of lithia mica. The interstices between these crystals are filled with an aggregation of albite feldspar also carrying "tin-stone," but in more massive form. 'Tourmalines or "schorl" also occur as in tin-bearing rocks in Cornwall. Tourmaline is a long, jet black crystal not unlike hornblende. The commen mica associated with these tin deposits is of a light greenish yellow color, and the feldspar is white. When mica, quartz and feldspar are all present in the granite, tin is absent; when only mica and quartz, tin is present. If the vein is of feldspar alone there is no tin. The quartz is usually banded. If the crystals of the rock are large the tin crystals are large also. Tin occupies interstices between crystals. Apatite, columbite, beryls, garnets, barytes, zircon, corundum minerals also occur. Stream tin is not so pure as the vein tin. The yield is about 74 per cent. tin.

For our knowledge of the deposits of the Black Hills we are indebted mainly to Prof. F. C. Carpenter's admirable report.

Prospecting For Placer Deposits In Dakota,

Experiences in this region with the gravels as related by Jenny are very suggestive to the placer prospector.

" The placer gravels result from decomposition and erosion of the rocks, and these included gold deposits in Tertiary times. The gravel deposits of French Creek show a local rich concentration of gold on the outer edge of the bed-rock. Though very encouraging at first, on driving an open cut into the bar where the gravel was undisturbed the richness of the pay dirt rapidly decreased and soon became uniform, showing the result iirst obtained was only a superficial rim rock 'prospect.' The richest layer was rarely on bed-rock, but 10 to 20 feet above it in a sort of false bottom of compact clayey gravel which had retained most of the

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gold. The gold was in flattened scales free from black sand but associated with little-worn garnet crystals. The gold is derived from quartz ledges in schists rather than from the intruded granites, as shown by the fact that the gulches paved wholly with granite were barren. Pay gravel is of heavy pebbles, clayey sand, and many garnet crystals derived from the schists. Itissoft, rarely cemented to a conglomerate, and easily washed in a sluice. There was a general diffusion of gold in the creek beds but little concentration in rich deposits, due to slight denudation of the ledges and want of sufficient grade in the valley to cause a concentration of gold intoa paying channel. Down Spring Creek where a large quartz vein crosses the gulch, gold is found in the stream bed, derived from a decomposed stratum of clay slate which retained the gold swept over it from the quartz vein. It is noticeable that enormous quartz ledges carrying gold in place are in the vicinity, and these have made the placers. In another locality the richest layer was the lower part of the red garnet gravel resting on the surface of blue plastic clay. Where the bed-rock is soft and decomposed it is liable to be rich, but when hard and smooth, poor. Large placer flats and elevated bars occur at bends of the stream and are rich. The region is just such as would lead the prospector to expect rich placers. The source of supply is great, the side valleys are excavated for miles along the outcrops of gold-bearing veins, slates and quartzites, all contributing to the placer of the main valley. Gold has been partly retained in the gulches and then carried out and scattered far and wide in the drift. In flats and creek beds where a stratum of soft slates is found crossing the gulch below, a high and hard bar with rich deposits may be sought for. Pits were sometimes sunk in the flats near the channel of the stream, but failed to reach bed-rock owing to uprising springs of water which could not be controlled. Panning has varied from 1 cent per pan to 1o cents on an average. On Bear Creek one pan yielded $27 and a rocker in 8 days took up $165. On Deadwood Creek gold is derived from igneous rocks and the gravel is of the same material, yielding 12 colors to the pan. Manganese and limonite iron were found associated with the gold sand, showing the gold came froma heavy manganese and iron ledge in the cliffs. The-gold

being entirely free from quartz appears to have been derived directly from the igneous rock itself, not from quartz veins. A gravel wash from the Black Hills is found all over the surface of the plains, made of every kind of rock found in the hills and doubtless carrying a certain amount of scattered gold. Miners prospecting up a dry guich of Whisky Creek obtained 25 colors from dirt shaken from the rou' of a small bush growing in acrevice in the bare sandstone bed-rock at the bottom of the ravine; hence the locality is called the Rosebush diggings, which derives its gold trom the washing down into ravines, by occasional heavy rains, of gravel deposits capping the hills; such asudden stream would sluice the gravel accumulated in the gulch, the gold being caught in the crevices of bed-rock. It yielded 5 cents to 15 cents per pan. The gold was in fine particles associated with garuc.s which came from the schists of Harney's Peak. The ravine is hollowed out 200 feet through red sandstones. Its bottom is paved with Carboniferous sandstone, and the hills on bot! sides are covered with deposits of slate and quartz which furnished the gold. The supply of water was so small in force, though the deposits were rich, that miners waited till spring rains filled the water-holes and made it possible to work the pay dirt in rockers in rich spots. Most of the streams sink in their beds among the foothills miles from the placers. In dry ravinescutting through gravel deposits ininers can make wages by washing the earth from the bottom of the gulches during early spring months when there is water enough."

Prospecting In Arizona,

Arizona is in the northern portion of the great plateau system. We visited Prescott some time ago and the mim ing region around the Hassyampa Creek. Between the Union Pacific and Prescott the country is very sterile, composed mainly of contorted granitic schists and lavas. About Prescott we come into massive granite and syenitiec ' rocks traversed by dark greenish-gray dykes of diorite. f These dykes are in places gold-bearing, especially in the oxidized decomposed surface, yielding a good dea! of free gold over aconsiderable width of the rotten dyke, which at

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the time of our visit was being treated by an arastra in the creek below. Atalittle depth, however, we found the free character of the ore changed to rather rich gold-bearing pyrites requiring smelting. On examining a cross section of the dyke, which was upwards of 100 feet wide, we found it traversed by numerous little veinlets, which assays showed to carry the gold, the diorite matrix being pcor or barren. The main difficulty in this region is the general lack or uncertainty of water, the creeks being liable to dry up at certain seasons and to boom at fitful intervals, Arizona is noted also for its rich copper mines. In the southern part of the State near Tombstone you rise from Post-Ptiocene gravels to a granite plateau of gray, crystalline eruptive granite, weathering in gigantic rounded blocks lying on one another. Near Tombstone stratified formations overly the granite, consisting of quartzites, limestones, and slates of

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gun ectier evade wilhiaave, wlio. Piate CVI,

Arched Fold, Toughnut Mine, Arizona. 1, Novaculite under Limestone; z. Limestone bending over the Novaculite; 3, Shale. bending over the imestone.

Lower Carboniferous and of Paleozoic age, dipping at alow angle toward the east. The Toughnut miue, described by W. P. Blake, is an instructive one to the prospector. "Here porphyry dykes cut through the strata following the general faulting lines of the country, the veins also following the same general course. The stratified rocks are shales and quartzites very fine-grained, the latter rock changed to the variety called 'novaculite' or whetstone rock. Abundance of iron pyrites occur in the layers of quartzite. Above the quartzite are dark blue limestones and black shales, The black limestones above the novaculite are silver-bearing. These beds are folded into arches, The Toughnut is on the anticline' of one of these arches. The ore was discovered cropping out in the soil and vein stuff. The rich ore lies in the folds. The folds have also

broken into faults. The Grand Central Chief mine is located in the outcrop of a dyke of diorite porphyry which carries ore, in, through and alongside it. The prospector found the outcrop obscure, being a confused mixture of porphyry, flints, quartz and porous quartzite. None of the outcrops rise high above the soil. He was led, however, to the spot by aconsiderable stain of iron, and a little digging revealed good ore near the surface.

"The dyke varies in thickness from a few feet to 70 feet, ripping west 55 degrees. It cuts through the shales, quaitzites and limestones. The dyke is vertically laminated or divided from top to bottom by layers or cleavage planes filled with thin veins of quartz (in this respect as in many others resembling the phonolite dykes of Cripple Creek with their cleavage zones produced by shearing or slight faulting movements and filled with richore). Large portions of the dyke are so penetrated by quartz as almost

Tt Ss

Plate Cvii.

Cross Section of the Mineralized Dyke, Contention Lode, Arizona. Showing vertical laminated structures with seams and cavities of quartz crystals and ores.

to consist of that mineral. The dyke itself is much impregnated with pyrites in cubes, many of which having dropped out leave square cavities and produce a honeycombed structure of the quartz. Though it has been worked 600 feet deep and there are 12 miles of workings, undecomposed ores below water level have not been reached. The minerals are oxidized and so red with iron oxide that miners emerge from the mine like red men.

" Along the upper 300 feet of the dyke extensive decomposition of porphyry has produced pure white or stained kaolin or china clay. This kaolinization extends to the adjoining shales. The ores are gold and silver, the gold being free, the silver as chlorides with carbonate of lead. Metallic gold and silver chloride are disseminated through the mass of the porphyry, while portions of the porphyry

PS oq §

carry quartz veins. The porphyry also passes into soapstone and serpentine.

" Gold occurs in crystalline flakes and scales chiefly in and along thin seams and cracks in the mass of the rock as if infiltrated and deposited from solution. Free gold is found in the quartzite. Both dyke and strata have been moved

Piate CYVIII.

Dyke Matter Penetrated by Veinlets of Mineral-Bearing Quartz. Biack, Quartz Veinlets, Light Shaded, Feldspar.

and faulted as shown by breaks in continuity and by brecciated cross courses, seams traversing both igneous and stratified formations. This breaking up of the dyke and fracturing and brecciating of the country rock, accompanied by the movement of the dyke upon itself and the formation of heavy clay seams, provided suitable places for the accu-

Vue Co.weny Enemasr ano Mara MmER.

Plate Cix.

Faulting of Ore Body or Vein, Contention Mine, Arizona.

mulation of ore found in the softer, more broken portions of the dyke. Bedded ore deposits are associated with bedded dykes and vertical fissures parallel with the Contention lode. One lode is traceable for two miles till it passes into underlying granite.

"A line of fissures cuts across the arch of the Toughnut

which h&s been followed in ore and is connected with the side bedded deposits. This lode is marked by heavy outcrops of quartz and by flinty boulders lying above the limestone on the surface. The bedded deposits fill irregular cavernous spaces eroded in the strata by metalliferous

PLATE CX. Bedded Deposits of Lead Passing from Stratum to Stratum, through Joint cracks, (Arizona.)

solutions without definite boundaries, and are apparently explained by the metasomatic or substitution theory.

" There have been shearing movements of the dyke upon itself resulting in heavy clay seams from attrition, also

Plate Cxi.

Section of Moose Mine Vein, Cripple Creek, Colorado. 1, Country Rock breccia; 2, Yellow Jasper with Cavities of Quartz Crystals; 3, Blue-gray Jasper with Seams of Quartz and Iron containing Gold.

lateral and vertical displacements from west to east and downward, the top of the dyke having been carried off in successive blocks by the sliding of masses of the stratified

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pint

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on lso

bck ay

formations upon the planes of deposition of the beds and partly on steeper planes of fracture. These movements have been accompanied favorably by ore occurring in the softer, most broken portions of the dyke, coincident with great original metallization and subsequent movement attended by clay seams. The fragments are not cemented by quartz but loosely by clay, showing mere mechanical force."

The vertical lamination of the dyke by shearing and the filling of the interstices so caused with quartz and mineral is like to what we find so often at Cripple Creek, Colorado, in the mineralized dykes of phonolite forming the lode of many of the mines such as the Moose, Elkton, Raven, and others—phenomena to which the prospector's attention is particularly called, as he is likely again and again to meet with it. Mr. Penrose in his description of the veins of Cripple Creek gives avery clear account of these peculiarities in ore deposits. According to him, "the nature and mode of occurrence of ore deposits at Cripple Creek depend on the character of the fissures containing them. Fissuring occurred before the

a formation of the dykes which filled the j fissures. Sometimes veins alone occupied

these early formed fissures, sometimes dykes. Generally, however, the veins

were formed at a late date long after the fissuring and dyke filling, as the veinsin- ™1gpquen tersect the dykes following the course of AEAS pre-existing fissures and intersecting the PLATE CXII. dykes longitudinally or crossing them Section of the Zenodiagonally. There are sometimes two Qa .V°Ryamolent systems of parallel fissures. The fissures a clean cut fissure are very numerous and their course fol-occupied hy a Bree lows that of the veins and dykes, viz., Vein.

northeast and northwest or generally

north and south. Fissures were not open gaps, but closed lines of fracture and veins in them are due to replacement of country rock along these courses. These fissures were at times held open by loose fragments of rock broken from the walls or by protruding parts of the walls brought opposite each other by movements along the fissures.

The course of fissures is sometimes a clean-cut break but

con anncnaarntnae e e

usually with parallel cracks on either side so numerous as to give the rock a banded, shected or slaty structure, sometimes not parallel but intersecting, producing 'linked fissures.' Outside this fissured zone fissuring becomes less and less and farther apart with receding from the main

Plate Cxiii.

Shearing Parallel Fissures sikh te a Fault. C. O. D. Mine, Cripple reek.

zone. This parallel fissuring is due to strong compressive stress in which dislocation is spread over a series of parallel surfaces instead of confined to one fissure. The distribution of these lines of dislocation in a homogeneous mass follows definite mathematical laws. Fissures occupied by veins result from movement and faulting as shown by presence of breccia, groovinys or striz and slickensides. These movements were of the nature of earthquake shocks. The character of fissures depends on the nature of the rocks they intersect. In massive hard rocks the fissures are sharper than in soft plastic ones like Pate CXIV. breccia. In one case force causing a rene . fissure overcomes cohesion of hard Section of Elkton Vein, . ; Cripple Creek, Show: rock, making a sharp break, in the ing relation of a vein other only to the extent of faint fracto sheared Phonolite ; Dyke. 4, Vein; #, tures without any one well-defined Sheared Dyke; C, break. The ore deposits are bodies of Country Rock. F ' secondary minerals filling the fissures, sometimes a single fissure, sometimes a number of thin parallel seams filling a fissured zone. Ore deposition was a sequel to dyke action depending on heated rocks for its effect. Dykes may have cut water channels in country

y pr!

1S Be S- 3S in

n

rock, and water from these channels forced up the sides of the dyke caused ore deposition. Shrinkage cracks also in the dykes at their contacts with country rock may have offered favorable places for ore deposit. Hence the connection between veins and dykes."

Prospecting In New Mexico,

This is a region characterized by great flows of basalt and recent lavas, so recent that they often cover the placer grounds and modern river deposits. Oldcraters occur here and there, and the foothills and prairie border are studded with lava-capped mesas. To the west the country is a continuation of the Rocky Mountain system, with many rocks and formations similar to those in Colorado and producing much the same ore deposits and in much the same geological relations. Thus there are contact deposits between porphyry and Carboniferous limestones as at Leadville, and fissure veins in granite as in Clear Creek County, Col., and mineralized dykes as at Boulder. The Rocky Mountain system is lower and more broken up into individual ranges than to the north. Besides the veins of gold and silver in place there are vast areas of gold placer ground; but the prevailing feature is a lack of water to work them. The great Rio Grande system, it is true, traverses the region, but the fall of the river is not sufficient in most part to bring its waters out of its bed for mining operations.

Gold occurs in the Jicarilla Mountains but no water, and the gold ores in the veins distribute their wealth in beds of dry gulches furrowing the sides. In Grouse gulch a placer occurs resting on hard red clay from decomposition of red granite bed-rock. At Santa Fe the gold placers lie in the Placer Mountains, for the placers in this region are true "hill deposits" on slopes and ridges of the Rocky Mountains carrying coarse gold like those of the high plains of California. Pay gravel lies deep below the surface and is generally very rich. Absence of water leaves many of these untouched. Mexicans sink well-like shafts, according to Locke, through the soil to the gravels and tunnel upon bed-rock, and take the richest gravel to the surface in sacks, cart it two or three miles to water, and pan out the gold in wooden bowls called "bateas." In winter they obtain water by melting snow with hot stones.

Gold occurs locally in quartzose sandstones of Carboniferous age and in rusty beds rather than in veins. The sandstone appears to have been charged with gold-bearing pyrites, by decomposition of which the gold has been liberated. In localities there are regular quartz veins bearing gold pyrites which have been worked for twenty years. The erosion or breaking down of a bed of sandstone would supply gold to a stream or deposit without its being accompanied by beds of quartzose gravel. So rich deposits may exist on the hillsides without indications of their presence by beds of rolled gravel or broken fragments of veins on the surface.

Professor Silliman, speaking of the great placer deposits in New Mexico, says:

"Here are countless millions of tons of rich gold quartz reduced by the great forces of nature to a condition ready for the hydraulic process, while the entire bed of the Rio Grande for 40 miles is a sluice on the bars of which the gold derived from the wearing away of the gravel banks has been accumulating for countless ages, and now lies ready for extraction by the most approved methods of river mining. The thickness of the Rio Grande gravels exceeds often 600 feet, or three times that of the like beds in California, while the average value per cubic yard is believed to be greater than in other accumulations yet discovered."

The area, according to him, covered by these gravels is 400 square miles; only three portions of this area are available or within reach of the Rio Grande waters, and the lava circumscribes much of the river-frontages. Nothing corresponding to the "top dirt," " pipe-clay" or fossil wood of the California gravel beds occurs. The gravel for many miles is unbroken except by valleys of erosion cut down 200 feet deep in them, with yet 400 more before bed-rock is reached. The gravels above the second " malpais" will be of less value than the under bed, and zones of poor gravel may occur. Over limited areas beds of fine yellow sand occur which are poor or barren, but the great mass of these heavy beds are compact gold-bearing gravels and contain boulders of quartzite with blue or gray stains and seams of magnetic iron and rusty quartz stained by decomposing iron pyrites, with but few pebbles of granite, syenite, porphyry or greenstone characteristic of the mountain

'

nm

wri nenendoan

ranges, and with no volcanic debris or ashes. Quartz and quartzite pebbles form 80 per cent. of the gravel in these beds; the source of the material is from corresponding beds of the Sangre de Cristo Mountains north and east. Prospectors claim that the gravels will average 50 cents to 75 cents to the cubic yard. An artesian well was sunk at the Ranches de Taos 425 feet, and through the entire depth only gravel was met and the material showed the presence of gold for the whole distance. Along the Rio Grande mining operations by ground sluicing have been carried on ever since this locality was first possessed by the Spaniards. Dredging is being carried on in some parts of the Rio Grande on the bed of the stream itself.

Chapter Xix.

THE GOLD OF THE ORTIZ MOUNTAINS AND GALISTEO AND RIO GRANDE PLACERS, N. M.

IMPORTANT mineral deposits and placers lie at the base of the Ortiz Mountains and along the Galisteo and Rio Grande rivers. The placers are being worked by dredges by the Santa Fe Placer Mining Company, to the chief engineer of which, Mr. F. E. Nettleton, and to Prof. E. Walters (geologist), we are indebted for our information on this region as published in the Southwestern Manufacturer.

The Ortiz Mountains are 25 miles from Santa Fe city. The elevation of axis of this mountain is 10,000 feet above sea level, the valley of the Galisteo River at its foot is 5.674, at Los Cerillos railroad station. Along this axis are granite, syenite and porphyry. East and west of the axis, paralleling it, are black trap rock, volcanic dykes extending across the country indefinitely from three to five miles from the axis of the range. Between the axis and the dykes, about three-fourths of the distance, are well-defined lodes parallel to the axis of the range. At right angles to these lodes are secondary lodes reaching from the primary down to the dykes, especially on the east side of the range. The great western primary lode extends south to San Pedro,

On the secondary leeds are fine bodies of low grade ore, such as Cunningham Hill near Dolores.

The main western lode is rich in copper, and copper mines, as the San Pedro copper mines. Orhers, such as the Gipsy Queen and" Lincoln-lucky," are gold producers, The nain primary lode on the eastern side of the range has been worked at intervals since 1711, soon after the second conquest of New Mexico by the Spaniards. Sefior Ortiz located on this lode the celebrated Ortiz gold mines. The vein matter of the Ortiz lode is decomposed quartz carrying free gold, with depth changing to sulphides or pyrites. The Spaniards worked out great quantities of this ore by means of old-fashioned stopes and inclined galleries, but owing to their crude methods they could not successfully

Plate Cxv.

The Ortiz Mountains and Galisteo River.

work the mines below the depth that yielded the free milling ores.

The axis of the Ortiz Mountain range is in close proximity to the newer formations closely flanking its slopes. This uplift came, as in the Colorado range, after the Cretaceous period. The axis is raised some 2,000 feet above the sandstones flanking the mountain, which contain both anthracite and soft coal. The green trap-rock dykes were thrust up through the newer formations. These Cretaceous sandstones are soft and easily eroded, and form the country rock that usually includes the gold-bearing veins, hence a large quantity of gold is freed and carried to lower levels by each rainy season. The slopes of these mountains are so steep and the sandstone so soft, that erosion is extraordinarily rapid.

On the east side the range are large fields of rich placers —decomposed quartz in sand and gravel which have inundated the entire eastern slope. Here are millions of cubic yards of gold-bearing material resting on soft sandstone. These deposits were made in a past age after the mountains uplifted and had afforded great quantities of gold-bearing material freed by the rapid erosion of the country rock. Above the main eastern dyke and paralleling it for several miles is probably the richest "dry placer" in the entire field. The geology of the region is simple: the strata rise from the Galisteo River at an angle of 10 degrees up to the pemary main eastern lode. Between that and the axis of the mountain the incline is much greater. The lode is in a true fissure into which the vein material has been injected,

The sandstone constituting the general matrix of the country rock is so soft and porous that the vein matter lying near the surface rapidly oxidizes. The oxidized honeycombed quartz remains, with its vast supply of free gold that erosion is gradually freeing and carrying down the slopes to feed the placers below.

The great trough that affords a line of rest for these enormous placer deposits is the bed of the Galisteo River. This river is four to ten miles from the main eastern lode, and close to the dry placers which are from hundreds to thousands of ieet higher than the river, though the deposit extends in more or less richness down to the banks of the river. There is considerable uniformity of values throughout the field. Placers of workable richness are found almost anywhere where there are drift deposits on the entire eastern slope of the range.

Water supply is the most difficult problem. The Cunningham mesa, or "old placers," on the eastern slope has been worked for hundreds of years by ancient Aztecs and later Spaniards, yet it is said by experts that if water could be brought to bear the placers could yield a million annually for twenty-three years despite the hundreds of past years they have been worked. These dry placers have only been worked hitherto by the Mexican dry washer and by "batea" and dry panning and hauling the material to the nearest water on the backs of burros. Hundreds of thousands of dollars' worth of gold have been extracted, and

aot ten:

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Se

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still but a minute fraction of the deposit has been touched. For five miles from Los Cerillos to Ortiz station 'he bed of the Galisteo River is a rich placer and will pan weil whereever samples are taken. The sandstone bed-rock is 15 to 35 feet below the surface. There is not enough fall and pressure power in the river for hydraulicking the dry placer above. The next nearest is the Rio Grande. The water in the river is mostly "sub-flow" penetrating the deposit from top to bottom, hence all the material is ina

Assay Value

per Cu. Va. ..River bank, ro feet,

Coarse drift sand, 3 feet.

Adobe clay, 3 feet, Coarse gravel, 1 foot, .. Adobe clay, 1 foot,

Coarse sand and gravel, 4 feet.

Zz

..Gravel and stones, 2 feet. .. Fine sand, 2 feet. .. Large gravel and stones, 4 feet.

...Coarse sand, gravel and stones 3 feet.

<Gray sandstone, dipping 20° FE. (bed-rock),

AND Mera. MINER. PLATE CXVI.

Section of Rio Grande River Bed, showing Strata Values,

partial state of suspension. so that any particle of gold lodging on the surface finds its way to the bottom, where it remains, Thus the material near the surface shows $2.46 and at bed-rock $6.42 per cubic yard.

The Santa Fé Placer Company used the air caisson for making tests of the materials, the strong sub-flow prohibiting the use of the ordinary cut and pumps. The stratification of the matter penetrated is shown in the sketch.

Mode Of Working Placer.

The process proposed for extracting the gold is by the Nettleton placer iiachine, 4 powerful steam bucket dredge of a capacity of 1 cubic yard of material per mipnute, having as an auxiliary a six-inch centrifugal pump whose suction pipe will extend down the dredge ladder to within 12 inches of the lowest point reached by the buckets. This pump will not only bring up the necess@ry water for sluicing, but such loose material as may be lefi by the buckets and in a great measure clear the bedrock of gold. The product of dredge and pump is deposited in a sluice

Plate Cxvii.

The Nettleton Placer Mining Machine for River Work. Capacity, 1000 Yards per Day.

box 25 feet ubove the deck of the barge, from which elevation the work is done by gravity until the material and water is disposed of. Passing down the first sluice of 30 feet a grizzly or grating is reached, removing stones over 3 inches in diameter, finer material passing through screens which reduce it to one-half inch. Sothe non-productive material is removed at once and deposited behind the barge. Having passed through the screens, the material and water fall into a box containing quicksilver and thence flow into table sluices, giving additional length of sluice of 70 feet, by which time even the freest gold has gravitated in the rifles of the sluices and been held there by quicksilver, with which they will be charged, The percentage

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ra oa og

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anes peti: sis

of fine flour gold being very large, the material is passed over a burlap siuice, the fibers of which arrest and hold the gold. The usual accompanying " black" or magnetic iron "sand" carries a great deal of gold, as high, so it is reported at times, as $2,000 per ton, the gold probably in sulphides. To save this, after passing the burlap, the matter comes in contact with strong magnets placed in the circumference of a cylinder, the iron adhering to the magnets, from which it is removed b, a revolving brush, the non-magnetic matter passing on to a revolving screen, where it is reduced to one-sixteenth inch preparatory to being run over amalgam plates, such as are used in stamp mills, or into a series of boxes filled with quicksilver. By this time all collectable gold will have been saved, and after being run through traps to save any stray amalgam or quicksilver the now unproductive material will pass into a tailings well and be taken up by an 8-inch centrifugal pump and deposited far behind the boat. Fine sand settling in the riffles of the siuices or burlap will be treated with cyanide. Depressions in bed-rock the dredge cannot reach will be reached by the air caisson and bed-rock thoroughly cleaned.

Another plan suggested is to raise the material and water for sluicing with a centrifugal pump to the ainalgamating plant placed on the bank. Large stones and gravel from the screens will be deposited in the excavation back of the workings and the fine tailings, sluice and surplus water will be conducted down the river by flume a sufficient distance to prevent its return. This plan will enable the bedrock depressions and crevices to be cleaned by hand at less expense than by dredge or caissons. The water flow of the river will not exceed 10,000 gallons per ininute during 10 months of the year. So no great capacity of pumps will be needed. The natural conditions have made the Galisteo River a promising placer proposition. The extent of its gold deposits can only be conjectured.

Chapter Xx,

The Gold And Silver Ore Deposits Of The Mercur District, Utah,

For our information on this district we are indebted to the valuable reports of the United States Geological Survey by Mr. S. F. Emmons and Mr. E, Spurr, From the base of the Wahsatch Mountains on the east to the Sicrra Nevada on the west is an arid region called the Great Basin, be-

Plate Cxviti.

Mercur Basin, Looking South, Mercur Hill on the Right,

cause it has no external drainage to the ocean, This was once occupied by two large fresh-water seas, represented now by only small salt lakes. The Basin consists of broad level valleys 6,000 feet above the sea, intersected by mountain ridges called the Basin ranges. The Oquirrh range, in which is the Mercur gold-mining district, is the first of these ranges west of the Wahsatch, about 13 miles from them. The Great Basin is an arid, save-brush desert. A few small streams are in the Oquirrh range but insufficient

for mining purposes. The range is 30 miles long, culminating in Lewiston Peak, 10,628 feet above the sea.

Utah has hitherto been celebrated more for its silver than gold products. Hence the importance of the gold-mining district of Mercur.

Bingham Canyon, Ophir, Stockton, Camp Floyd and Tintic have atl been noted inore for their silver than for gold. The Oquirrh Mountains are composed of Carboniferous limestones and quartzites compressed into a series of complicated folds, accompanied by metamorphism and in-ee

LT

Plate Cxix.

Mercur Basin, Looking North, Marion Hill in Left Foreground.

jection of porphyry sheets and dykes with subsequent mineralization in the more disturbed districts. The Lower Carboniferous limestone of Lewiston canyon is the ore-bearing horizon of the Mercur district. On the north side of Ophir canyon an arch of Cambrian quartzite has been uplifted by fault. There are no large exposures of eruptive rocks such as result from eruptive overflows, but rather narrow dykes and intrusive sheets. In Bingham Canyon the ore occurs only in the vicinity of porphyry bodies that occur there. In the Mercur district the igneous rocks are in thin sheets parallel to the stratification, and beneath these sheets the ore deposits occur. There have been two distinct periods of mineralization. During the first the silver ledge was formed, during the second the minerals of the gold ledge were deposited. In both cases the ore was de-

5s rH 6 St oe

posited along the lower contact of a porphyry sheet where a porous or brecciated zone has been formed by intrusions of igneous rock which the mineralizing solutions reached through fractures or fissures extending downwards from the respective sheets. The principal vein materials of the sliver ledge are silica, barium, antimony, copper and silver brought up by ascending hot solutions as sulphides and sulphates. They were deposited in the contact zone below the lowest porphyry sheet and occasionally above it. The limestone in this zone is replaced by silica. The fissures 'hrough which the mineral solutions ascended have since been filled with calcite.

There are two kinds of quartz porphyry. The Eagle Hill porphyry is a light white rock, like Leadville white porphyry; the Birdseye is gray and speckled with hornblende mica quartz and feldsparcrystals. Two ore-bearing beds or zones too feet apart occur near the middle of a great series of limestones. The lower bed is of a dark Silicified quartzose limestone, brecciated and porous, carrying silver, copper, antimony, but no gold. It is called the Silver ledge. The upper zone, called the Gold ledge, is of decomposed bleached red or yellow limestone and shale containing realgar and cinnabar 'vith low but uniform percentage of gold.

The Silver ledge, owing to the hardness of the rock, causes it to stand out as a distinct ledge and is easily followed, but the Gold ledge of softer material could only be traced by a slight ochreous appearance in the rock. The gold is invisible. Certain beds supposed to be clay or shale in the mine proved to be altered sheets of white porphyry. Three of these were traced on the ore-bearing zone and revealed the oft-observed connection of igneous rock and ore deposit. The vein materials of the gold ledge are realgar (sulphide of arsenic), cinnabar, pyrite and gold, with these are barite, calcite and gysum. The deposits occur at the intersection of zones of fracture with the lower contact of the middie of the three porphyry sheets, reaching a thickness of 20 feet. Some of the fissures are still open, showing no evidence of filling or erosion by circulating waters. (See Plate CXX.) These fractures cut across the silver ledge and, as a rule, do not extend above the gold ledge,

he section of the region is as follows 1, Blue gray, Lower Carboniferous limestone occupying the bottom of the canyons, 200 feet thick. 2. Interbedded limestones or calcareous sandstones, 600

feet. 3. Thick blue gray limestone, 5,000 feet thick, containing

'

Tae COLLEY. ENGINEER AND M&@TAL MINER: PLATE CXX,

Natural Open Fissures in the Face of the Drift of the Silver Cloud Mine, in Silver Ledge, Mercur,

thin strata of water-bearing shale, and in its lower portion

it carries the ore horizons. 4. Above this again more limestones and sandstones, 5,000 feet thick. So in Mercur Basin a total thickness of

12,000 feet of strata is exposed.

eer

ws

atc

As the hills around Mercur are not covered by drift it is easy for the prospector to trace the line of contact between the eruptive porphyries and sedimentary rocks. The

Zx

Map and Section of the Oquirrh Mountains. JD, Drift; 7. C, Lower Carbo. niferous; U C, Upper Carboniferous ; C,Cambrian ; & /, Eagle Hill Porphyry; 42 P, Birdseye Porphyry.

zone can generally be identified by fragments lying on the surface. !n the weathered rock limestone chips are of the typical dark-blue color, while those of porphyry are yellow

, brown or green, On a bare hillside the line separating the two can be easily traced, The Birdseye porphyry weathers an olive-green coler and the Eagle porphyry generally breaks up into small blocks and chips.

Most of the rocks in the Mercur Basin show traces of gold like at Cripple Creek, Col., suggesting a widespread mineralization. The porphyries showed the highest traces and the limestones the least. Pure white calcite veins unconnected with the main mineralization showed small quantities of gold. Certain localities are so greatly mineralized as to furnish profitably worked bodies of gold and silver

Plate Cxxii.

Geological Section of Mercur Basin.

ore. These localities are at the contact of porphyry sheets with enclosing limestone. In localities only is this contact line rich. In one group the limestone is hardened at contact with the porphyry into what miners call " black quartz" showing silver chloride, antimony, copper carbonate and barite. In the other groups limestone and porphyry are decomposed into a soft black shaley substance. The first group contains silver, the second only gold together with arsenic and cinnabar. The one is the silver, the other the gold ledge. The rock forming the contact of the silver ledge is much broken or brecciated, the fragments composed of cherts and silicified limestone inclosed in cement of white calcspar and barite. The greater erosion of the — porphyry leaves a distinct shelf or ledge 20 feet wide.

In the limestone below the ledge are many vertical calcite veins formed by the intrusive action of the porphyry, as was also the breccia or broken element in the ledge, and the interstices were healed by solutions of calcite. Hardening and darkening of the limestone are noticeable at this upper contact for 3 feet. Three sheets of porphyry are developed on the hill, one 20 feet thick associated with the silver ledge, and the lowest, above this a smaller sheet, much decomposed, associated with the gold ledge, and above this a third unmineralized. At the bottom of the Silver Cloud mine are many open fractures without vein filling, indicating the action of faulting. They were later than the vein filling of the silver ledge. Large geode cavities lined with calespar crystals occur in the vein, together with a network of calcite veins; bunches of barite, stains of green malachite, and azurite copper occur, and a good deal of kaolin in crevices. The open fissures show their later origin by cutting through all these. The softer and decomposed porphyry is actively prospected for gold.

A black, flinty impure quartz accompanies the ore. Changing of the limestone into a quartz-like condition was one of the first stages of metamorphic action. The quartz is generally this "horn" or flinty amorphous Quartz. Crystals arerare. The latter occur inirregular cracks and cavities produced by solutions. The honeycombed nature of the rock is what mainly shows the intensity of the action accompanying mineralization. The calcite veins are generally barren. Barite or heavy spar is closely associated with the ores occupying t#regular spaces in the rocks and is a sure sign of considerable mineralization, Barite often forms the gangue in Which the ore is imbedded. Antimony occurs in radiating crystals and bunches. Copper stains are associated with the silver. "Chinese talc" or gouge, a clay resulting from decomposition of the porphyry, occurs as at Leadville. The silver ore consists of small films of chloride of silver disseminated through altered silicified limestone.

Mineralization has taken place at the contact of porphyry and limestone. From this it extends into the limestone away from the porphyry, mineralization decreasing in force as it recedes from the line of contact. (See Plates CX XIII andCXXIV.) The mineralizing agents were heated waters,

circulating along the contact, containing silica, barium, antimony, copper and silver. The work of these solutions was the leaching out and removal of lime and replacement of it by silica without destroying the original features of the rock. Quartz in the vicinity of eruptive rocks is apt to

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Limestone. Porphyry. Gold bearing ore. Vertical fissures. PLATE CXXIT!,

Geological Section of Part of the Mercur Mine, accumulate in compact crystalline masses or in a flint-like jaspery or chalcedonic condition, and the silicifying of the limestone at contact with porphyry at Mercur is only a natural and common result of metamorphic action,

Limestone Porphyry

Limestone...

PLaTE CXXIV.

Section along Geyser Tunnel, Mercur.

Water contained in lavas is not given off till just at the moment of solidification of the lava, when it is separated out and appears as a fluid. When this solidification takes place at the surface it forms clouds of steam so generally visible on cooling lavas, but when the lava is forced in, in a molten state underground, between strata the water is still under sufficient pressure to keep it ina liquid state. From

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this result, intensely heated solutions arise capable of much corrosive effect on the rocks and of aiding ore solution. These solutions act most violently at the contact and become rapidly cooled on penetrating the adjoining rock.

The phenomena at the silver ledge indicate brief intense action, highly heated waters with great metamorphosing and corr ding power. The mass is full of cavities showing this. The barium found in the silver ledge was derived from the porphyry, as probably were the metals, which were deposited as at Steamboat Springs, Nev., by ascending hot solutions. These exuding at every point in the cooling porphyry found in the limestone a zone where the passage of solutions was easy by opening of fissures and formation of breccias. The heated waters under great pressure would move along this broken weak zone, as also occasionally in an upward direction. Where porphyry sheets cut across the strata water would rise rapidly. Where circulation was retarded accumulation and mineralization would be greatest. In the case of the gold ledge the mineralizing agents were probably more in a gaseous than a liquid condition. The various metals, antimony, cinnabar, etc., found associated with the gold are such as would easily pass into the state of vapor and be the last deposited. After the eruption of the porphyry a disturbance brought about a set of vertical fissures establishing a communication with a body of uncooled igneous rock at an uncertain depth, affording a vent for moist volcanic vapors, and along the porous zone at contact of porphyry and limestone, and in the brecciated limestone the vapors spread out and becoming cooled deposited the gold and associate minerals.

The gold . -dge is a mineralized zone in the lower part of Mercur Basit. It consists of an altered limestone following the under contact of a thin sheet of altered porphyry. The thickness of the contact zone varies from 20 feet down to nothing. The lines of greatest mineralization coincide in direction with a set of vertical fissures forming shoots or channels.

The ores are oxidized or else sulphides. The former are extracted by the cyanide process, the latter by roasting. The zone is soft and pulverulent and full of cherts. The amount of gold in the ores rarely exceeds 3 ounces to the ton. Silver is absent.

CHAPTER XxI. SALTING MINES.

In these days when, owing to the depression of silver, so much attention is being turned towards gold and gold mines, too much care cannot be taken by those investing or acting as examiners or experts in gold mines, that there are no tricks played upon them by the astute miner; for "for ways that are dark and tricks that are vain" the Western miner is at times " peculiar." One of these tricks is what is known as "salting" mines or ledges; that is, by various means and ways introducing into the mine or into the samples taken from it, certain rich minerals which do not rightly belong by nature in the mine or property, in order to raise the value of the mine in the eyes of the investor or expert. When samples are taken from such a tampered-with mine the values and results must be accepted cum grano salis, with a very large grain of salt indeed. Whether this classical allusion be the origin of the word " salting" we do not know.

"Take care you ain't salted" is the advice to the inexperienced investor or novice expert. So clever are the miners, that cases are on record where even a most experienced expert has been taken in, and comparatively or wholly valueless properties sold for large sums, the purchase followed later by woful dismay and surprise, when dividends were called for and did not appear.

Gold mines, of all others, are the most easy to salt, hence the precaution in these days is timely.

Whilst a mining engineer or expert can hardly prevent salting, with care he can and ought to be able to avoid being taken in; to be forewarned is to be forearmed.

On entering a mining camp in the far West, especially in the more remote outlandish districts, an investor or an exert

may consider that the whole village, from the hotel bell-boy to the mayor (who, by the way, may be the principal saloon-keeper), is in league against him. Directly he arrives, everybody in town wants to know his business; on

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this he should keep as mum as possible, and, if he can, throw impertinent inquirers off the scent. The idea is, " Here is a capitalist to fleece and an expert to delude." Every one, too, has a "hole in the ground" of his own to present. Should they get wind of the particular property in view, there are confederates and middlemen anxious to share the spoils. Moreover, it is considered to the general credit of the camp to sell a mine, be it whose it may, good or bad, and if you mention any property, you will invariably hear it "cracked up." The Eastern "tenderfoot" is somewhat of a "sheep among wolves" in such a camp. The expert, too, is at acertain disadvantage on entering into a strange mining camp, not being familiar with the local conditions. Ores, for instance, in one section or region are not always of the same value as similar ores in another, the rocks may look new and strange to him, and there are a hundred local conditions known only to the resident miner. It would be well, when poss'ble, for an expert, before passing a decided opinion on an important property, to stay around in the vicinity for a while till he knows the "hang of things."

On his way to the mine there will be plenty to fill his ears with the untold value of the property he is about to examine; this friendly duty is not unfrequently performed by an officious middleman. To favor and "soften up" the expert's mind and heart and make him " feel good" toward the property, attentions of all kinds are showered on him. He is driven about town like a nabob, and if he shows weakness for a " wee drappie," champagne and whiskey are at his service ad /id., as judicious preparation for the coming examination. It may be observed here that attempts are made sometimes to "salt" the expert as well as the mine, not merely by befuddling his brain with intoxicants, but by offering bribes, and as an expert is often not too well off, the latter is a great temptation.

We will now suppose, after this ordeal, he goes to the mine with the superintendent or miner. All may be, and we may say generally is, honest and square, or it may not. The expert looks over the exterior and surface signs of the property studies the outcrop of the vein on the surface, its probable surface continuity, the advantages and disadvantages of the situation of the mine, its proximity to railroads

, smelting works, markets, etc., and then enters the mine in company with the miner. As a rule the latter will naturally point out 'o him the richest portions and ignore the poorer; sometimes he excuses himself from taking him down into the latter because it is dangerous or full of water. If full of water the expert if possible should have it pumped out. He may suggest, here and there, that such and such a spot would be a good one for the expert to take his samples, and so forth. The expert of course assents to all he is told, but with one eye open, and does not stop to take any samples for assaying until he has seen the whole of the mine; then he requests his companion to go out on the dump and smoke his pipe there, as he insists upon having no one with him in the tunnel when he is taking his samples for assay. He will be inclined to rather avoid those particularly favorable spots suggested to him by the miner, as probably giving too rich an average for the general run of the mine, or as not impossibly being "fixed" for him. If he suspects the latter, he will take a sample or two to see if the mine has been tampered with, taking a little of this out on the dump, crushing it, and washing it in an iron spoon. If avery astonishing amount of goid colors show up, his suspicions are aroused. The judicious miner does not generally want to salt too heavily, for fear of the enormous results exciting suspicion, but despite his care he nearly always salts a little higher than he intended. Ina mine where the rock is hard, a miner may salt by drilling holes and inserting mineral or ore and disguising the hole. In loose ground or one full of cracks, a shot-gun loaded with a moderate charge of gold-dust will do the work. The skill of the miner in this case lies in his choice of a spot where he thinks it probable the expert will take samples, or in coaxing the expert to take samples from such ground. In hard ground the expert may avoid such salting by having the work blasted out in his presence till a purely fresh, virgin face is shown and then taking his sample. These precautions are not necessary under all circumstances, but only in such cases where the expert has a suspicion that there is an attempt to " put up a job' on him. After getting his samples, and as many as possible, he will sack and seal them then and there in the mine, and never lose sight of them until he has expressed them to his

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own home. Sometimes a mine is so timbered up, that sampling is difficult. Now as they go down the shaft, it may be the expert remarks, "I should like to take a sample in this shaft, but it is so timbered up that I don't see how we can do it without ripping out some of these boards." "Why of course, so you oughter,' says the miner, "and see here, I think this board is loose." Now beware lest that board was purposely loosened and behind it the ground is salted.

By taking a great number of samples at comparatively close intervals, provided afterwards the samples are not tampered with, the expert is less liable to be deceived by salting, than if he took very few. A mine cannot be salted all over from end to end. if it is a large one, only at judicious intervals, and it will be hard if the expert does not escape soine of those intervals and get some true samples.

Besides taking his regular assay samples by cutting all around the walls, roof and floor of the tunnels at intervals of five, ten, or twenty feet, according to circumstances, crushing and quartering the debris, and finally sacking and sealing his sample bags, he should occasionally take a "grab sample," or a bit of rock at random, or a small sackful from the great mass of his samples, and put them in his coat-pocket, and keep them on his person, to act as a reference in case of any possible tampering or accident to his samples whilst in the vicinity or in transit. He should also take bulk samples, good-sized chunks of uncrushed rock which should agree with the assay results of his quartered samples.

A disadvantage an expert is under in a strange camp, if he cannot take his own assistant with him, is, that he is very much at the mercy of the miner, if any hard work has to be done, such as blasting or hard digging. Whilst engaged in such work the miner, if he pleases, has many chances of scattering around a little gold-dust on the rock of the vein or the loose dirt of a placer.

Whilst gold-dust is the favorite medium for salting a gold mine, chloride of gold is sometimes used. The latter, however, is rather a dangerous and barefaced trick to try on a competent expert, as its quality caa readily be detected by the chemist, it being soluble in water. Ina case of this kind that came to our knowledge, an experienced

expert had examined a certain mine and condemned it. Later, the owner who was an honorable man, asked him if, as a special favor, he would re-examine it, as in his absence the assay values from the mine had of late shown much better results. The expert reluctantly consented to do this, though contrary to his general rule. In going along the workings he noticed here and there on the walls certain patches and streaks of clay or mud, he had not observed on his first visit. Guessing what they were, he casually observed to the miners, " Seems to have been raining in the mine since I was here." However, to the great delight, doubtless, of the miners he took several samples of these, and forwarded them toa reliable chemist. The latter pronounced them chloride of gold. This of course gave the salting scheme away, as chloride of gold does not occur free in nature, much less ina mine. The owner of the mine was exceedingly angry when he learned what the miners had done without his knowledge or connivance. The men themselves being commonly more or less interested in the sale of a mine, are apt to try and salt it without any connivance of tke owner or superintendent. We heard of a case in the San Juan district where a mine that was fairly good was about to be examined. This mine carried occasionally specimens of the very rich ore called ruby silver. Not satisfied with the fair, natural richness of the mine, the miners must needs import into the hole quantities of ruby collected from other mines in the district, whose men were of course in sympathy with the scheme and probable sale. This was acting without the knowledge of the owners.

Salting Gold Placers.

Although a gold placer usually covers a very large area of ground, it is possible to salt it. Usually a miner shows up his placer by opening up pits at convenient intervals, so as to cover the property. Nothing is easier than to salt these pits with gold-dust. Consequently whilst an expert will examine these holes and pan the dirt, he should be on his guard, and insist, where possible, on holes being freshly dug in his presence. Even then he is not safe. Generally in a placer, by the cutting of a stream, sections are shown

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sometimes from grass roots to bed-rock. From such he should take and pan samples at different levels in the exposure; this too, privately and without too much supervision of the interested miner.

Salting Assay Samples.

This may be done in several ways. If the expert is imprudent enough to allow a miner to accompany and assist him in breaking down or crushing bape a or panning them, then the infusion of a little gold-dust is easy. Again, after the expert has made up, sacked and duly sealed his samples with wax, should he leave them anywhere within reach of the miners, they are not wholly safe, for the miner may insert the point of a fine syringe containing gold-dust into the bag, or he may make a bread mould of the wax seal, open the sacks, and either change the ore for richer, or infuse some gold-dust. Changing of samples for others is not an uncommon trick. The expert cannot watch his samples too closely. He should sack and seal them on the ground, sleep with them under his pillow if need be at night, yet even then cases have been known when the wary miner has succeeded in extracting and changing them for bags to all appearance exactly similar. The samples are never safe till boxed up and expressed and on the way to the city address. He should never fail, as we have said, to have partial duplicates of these about his person.

If the expert wishes to assay the ore at a friendly assay office near the mine, whilst he is grinding down his sample to dust, an innocent looking miner may loaf in, and whilst

'watching the operation, accidentally upset the ashes in his

pipe over the sample. Probably these ashes contain golddust, and we might here observe that a single grain of gold smaller than a pin's head may materially alter the results of an assay.

Some years ago an individual who had succeeded in booming a certain placer district and getting up an excitement and a rush, constituted himself as a referee, and professor; and when miners brought samples for his inspection, they were always found to be very rich in gold. But similar samples from the same spot if uninspected were

somehow invariably barren. The wizard's mere look seemed to change the sand into gold, until it was found that he concealed in his finger-nails " which were taper" not wax, but fine particles of gold. Hence, Midas-like, whatever he touched he turned into gold. Whilst the salter may lay traps for the expert, the expert may sometimes lay traps for the salter. An expert, who had reasons to suspect a certain mine he was examining had been tampered with, and guessing there was a likelihood of an attempt on his samples, after securing himself with duplicates, left his samples exposed on the floor of his room at the hotel, then went out and hired a reliable Mexican boy to watch his room and report to him immediately if he saw any one enter it. He had not long to wait. At dinner the boy tapped him on the shoulder, and he went to his room and caught the miner in the act of tampering with his samples.

Sometimes miners, if wealthy enough, will go to great expense to salta property. Some miners took a couple of well-to-do eastern capitalists to a certain placer, panned the gravel before their eyes and showed up wondrous colors. The investors having been warned of miners' ways, refused to entirely swallow the bait, but told the boys to go ahead and develop the property, and if at their next visit, it showed up as well as the pans did on this occasion, they would buy it. When the easterners were gone, ata cost of several thousand dollars they built a flume, put in a hydraulic plant, and gathered a pile of loose dirt to wash down the flume, where the gold is gathered upon quicksilver. The "sharks" raised $50,000 for a gold-dust fund. This dust was run evenly over the quicksilver so that, when the capitalists returned, there was everything to show an enormously rich placer-ground. The capitalists insisted upon a clean-up after the first fortnight's run, which added so much more joy to the sharks. This time the bait was swallowed whole, string and all. The capitalists paid down promptly $250,000 for the ground. The sharks left the country. Ina few weeks nothing could be found but the amalgam of the sharks.

An ingenious trick once baffled some experienced experts and came very near selling a mine. The mine was a well-developed one and had done great things in its day. It was claimed that at the face of the tunnel, or where the

workings left off, there was still a fine showing of ore in place to go on with. The experts found it as stated; on the face or end of the tunnel there was a fine showing of ore, and the probable amount in place and for the future was duly measured up and estimated. It leaked out later that this block of ore was only a thin screen purposely left, all back of, and behind it, having been carefully worked out and the opening for the miners' ingress and egress skilfully concealed. The mine was re-examined, the cheat discovered, and the reputation of the experts saved as well as many thousands of dollars from the pockets of guileless investors.

This brief sketch of some of the ways of some miners, for some regions and properties, would give an unfair idea of some mines and miners as a whole, if it were supposed that all miners are given to salting, and all properties for sale are beset by a network of dishonest devices. On the contrary, many, very many, miners are as straight as a string and hundreds of properties are to be examined without fear of tampering. But it often happens that a miner, who in every other relation of life is as honest as the day, draws a line, when it comes to the selling of a mine, which he considers " fair game."

But, as elsewhere the world through, honesty pure and simple is the right policy, and in the end would be found the best paying one. For the notorious dishonesty connected with mines (much more common in the past than in the present) scares away capitalists from investing, whilst if truth and honesty were maintained, money would roll in freely.

One lesson at least may be learned from what we have said, and that is, that if in some cases a professional expert is ever taken in, what chances has a capitalist, ignorant of mines, to buy a mine on his own examination? What man ignorant of horseflesh would venture to buy a steed from a professional horse-jockey, without taking with him a friend who is knowing about horses?

How much more so in such a difficult and delicate problem as that of purchasing a mine, is it the duty of an investor never to purchase or induce his friends to purchase a mine, until he has employed the services of a competent expert to previously examine it. If the expert's fee should

amount to a few hundreds, and after all he should decide on wi prragnra the property, it is far better for the company to entail this expense, and perhaps lose this small sum, than to involve themselves in the loss of thousands of their own as well as other people's money in a bogus, worthless, or wildcat scheme.

Chapter Xxii.

Prospectors&#x27; Tools And How To Sharpen And Temper Them.

The principal tools a prospector takes into the field are picks, drills, hammers and shovel.

A prospector, especially when climbing mountains, likes to be as light-handed and unencumbered as possible.

For his trip as a whole, he may carry several different tools packed on his donkey, but when he has arrived at a locality, the vicinity of which looks likely, he leaves most of his heavier tools in his temporary camp, or near to where he pickets his pack animal. He makes a short excursion up the mountain for a general reconnoitre, armed with nothing more than a light prospecting pick, weighing not more than three or four pounds. This little pick is about ten inches in length, with a handle about fifteen inches long; the longer portion is sharpened into a pick, and the shorter ends in a square-faced hammer. We recommend a square sharp-cornered face to the hammer, in preference to the bevelled face, as the sharp edges and corners ate better adapted for breaking rock than the rounded or bevelled ends, This prospecting pick or geological pick and hammer, should be all of good steel, with a good sized eye to admit a springy handle of hickory. See Plate CXXV, Figs. 1, 1, 1.

Armed with this little weapon he climbs the hillside, hunting for " float" or for rusty outcrops of ledges. Loose pieces of rock he cracks open with the hammer end, softer rock in place he explores with the pick. "When I am climbing over the hills," said an old weather-beaten prospector to me, "I want nothing but my little pick, then if

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I find anything likely 'in place,' I mark the spot, and go on, and at noon I come down to camp, or to where the 'burro' is feeding, I take up my heavy digging pick and shovel and 'open up'; this will occupy me till evening at least, then if I find there isa ledge worth more thorough capleritis, I leave my tools by the hole, and next morning bring up the drills, hammers and blasting outfit. But the first thing I would advise a tenderfoot, is to get his eye trained, trained to looking for float and observing mineral signs, trained to the whole business of close observation. Why! I myself, old hand as I am, after being away for some months about town or looking at other things, can't get my eye in and down to it for two or three days; then it kind of comes natural.

"You must have an eye for PLATE CXXV. float and rocks like an artist has an eye for color, and a musician an ear for music. A tenderfoot had better go along with an old hand for a few days to get into training."

Description Of Tools, Picks And Drills,

Picks and drills are the main tools that need sharpening and tempering. The kind of sharpening and nature or degree of tempering depend upon the kind of work or kind of rock to be worked, whether hard or soft, loose grained or fine grained, siliceous or clayey. Drills, for example, would have to be differently peed i and tempered for

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hard vitreous quartzite than for so e or hardened clay. The same remark applies also to picks. Picks may be double pointed or single, or with a hammer head called a poll, if it is to be used for breaking rock. The main points of a pick are, strong cutting tips, stout eye and a tight handle. The little prospecting pick is made of the best steel throughout, but in the heavier pick, the wearing

parts are the tips, which should be replaceable. An all steel pick is liable soon to be shortened up and useless, whilst the iron pick eye, a 14 inch length of best iron, gives long service by welding on tip ends, whenever desired. Professor Ihlseng, in his " Manual of Mining," as also Mr. George Andre, in his book on " Rock Blasting," gives excellent descriptions of tools used as well as the mode of sharpening and tempering them; to them we are indebted for many of the details of this article, and to their works we refer the reader for futher information on this subject. "The picks are sharpened to form on an anvil, and commonly drawn to a four-sided pyramidal point, for hard rock, and a slim taper for fissured rock, and a bluff taper to cut crisp ground, and to a chisel nd for chipping the ground. The eye is oval and well surrounded with metal. All the strain of the prying falls on the eye, which must be true and stout."

"The aril! is a bar which has one cutter edge and one hammer end. It is of round or octagonal steel. Drills may be of various lengths, from a foot to four or five or even more feet. For prospecting purposes two or three

medium short drills from two to four feet are generally enough, as the prospector's business is rather to find than to develop. In beginning to drill, itis common to usea short thick drill, with a stout 'bull edge' rather than a thin, tapering one, especially in hard rock; smaller sized, #.é., narrower drills may be used for increasing depth. "The rock drill consists of chisel edge, bit, stock and striking face. To allow the tool to free itself readily in the bore hole, and to avoid introducing unnecessary weight onto the stock, the bit is made wider than the latter. In hard rock, the liability of the edge to fracture increases as the difference of width; the edge of the drill may be straight or slightly curved, straight edge cuts more freely than the curved; a bull bit for hard rock is generally curved, a straight edge is weaker at the corners than the curved. The width of bits varies from 1 inch to 2 % inches. Figs. 1, 2, 1a, 26, Plate CXXVI, show the straight and curved bits and angles of cutting edges for use in rock. The stock is octagonal in section. It is made in lengths

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varying from 20inchesto 42 inches, The shorter the stock, the more effectively it transmits the force of the blow. To insure the longer drills working he in the hole, the width of the bit should be very slight y reduced in each length. Diameter of stock is less than the width of the bit generally by ¥% of an inch.

"The smith cuts up the 'borer' steel bars into desired lengths to form the bit, the end of the bar is heated and flattened out by hammering to a width a little greater than the diameter of the hole to be bored. The cutting edge

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Forms of Drills,

is then hammered up with a light hammer to the requisite angle and corners beaten in to give the exact diameter of the bore hole intended. The drills arc: made in sets and the the longer stocks will have a bit slightly narrower than the shorter ones for reasons already given. The edge is touched up with a file. Heavy hammering and high heats should be avoided. The steel should be well covered with coal, in making the heat, and protected from the raw air. Overheated or burned steel is liable to fly, and drills so injured are useless until the burned portion has been cut away. Care is required to form the cutting edge evenly, and of the fullform. Ifthe corners get hammered as in Fig. 3a, Plate CXXVI, they are said to be 'nipped' and the tool will not free itself in cutting. When a depression of the

straight or curved line forming the edge occurs, as Fig. 36, "the bit is said to be 'backward' and when one of the corners is too far back, as Fig. 3c, it is spoken of as 'odd cornered.' Either of these defects causes the force of the blow to be town upon a portion only of the edge, which is thereby overstrained and liable to fracture."

Sharpening Tools.

Professor Ihlseng in his " Manual of Mining" says: " The best fuel for blacksmithing may be a slightly caking coal, giving flame and high heat. Coke is hotter but harder to keep fire in. The fuel should be as free from sulphur as possible. White ash coal is better than red ash; sulphur makes the iron hot short, and tends to produce scales. The coal should be clear of shale or slate, for they fuse and make a pasty cinder that is annoying."

A prospector away from civilization may have to use wood; in that case he should use chips, and blow them with a portable bellows.

The prospectors who try to get along on as small an outfit as possible usually take one to three blasting powder cans and cut the heads out of all but the bottom one, and one head of that must be cut out; these they place one on top of the other to make furnace. They punch an inch and a half hole in the side of the bottom one at the bottom for draft, and to put in the points of the tools to heat them.

They use charcoal for fuel and then a chunk of steel or railroad iron about 6 inches long serves foi an anvil. Some take a small bellows and anvil with them. For tempering drills they give the drill, when red, a plunge in water. After two or three rubs on wood, to brighten it, they hold it up to the light and watch it until it takes ona straw color. Then they dip it in water again. For picks a blue color is the most satisfactory in general.

"Steel is a compound of iron and carbon, and its homogeneity and presence of carbon impart to it a capability of hardening and tempering to a degree depending on the temperature of the heating and subsequent cooling. As the amount of carbon increases, the melting point of the iron decreases, and this greater fusibility reduces its welding quality.

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"A steel is called 'hardened' when it has been suddenly cooled and thereby become as hard as possible. This is owing to the presence of carbon, for pure malleable iron is not affected by the operation, while both steel and cast iron are to a marked degree.

"The operation consists in forging the steel to a certain degree of temperature, and then plunging it into some fluid which abstracts the heat from the tool. The quicker it is done, and the greater the difference of temperature, the harder is the tool. Either water or oil is used; both volatilize at a temperature much below that of the immersed tools, so the hardening takes place in a vapor; oil generally produces the best effects. On the first plunge the metal is chilled and coated with soot, after which a slow process of cooling takes place."

Tempering.

"Tempering follows hardening, whereby the steel is subjected to a subsequent lower heat, which softens it, and removes its brittieness. When the hardened iron is slowly reheated, its surface gradually assumes phases of color, beginning with a light straw, passing through shades of yellow, brown, purple, blue and red. At a cherry-red heat, the original color before hardening, the effects of the chilling are practically removed.

"Tempering consists in carrying the second heat to one of the above mentioned colors, according to the amount of the brittleness to be annealed. This depends upon the use to which the article is to be put. A second stage of the operation finishes the job. The aforementioned reheat goes on a little way beyond the desired color. The tool is carefully plunged part way into the water or oil, till the disappearance of the steam indicates that it is cold, when another portion of the distance is further immersed for a moment. The tool is withdrawn, the scales rubbed off and the heat of the remaining portion draws to the edge, until it has assumed the proper tempering color. It is then thoroughly cooled. The idea that the steel is coo!=r at a blue, than at a yellow, in final drawing, is erroneous; for more of the heat is conducted from the red portion to the point, than it radiates to the air, and the first heat to the edge

only gives a yellow; with more, it becomes purple, and so on. Hardened drill and pick points are treated in this way, 4" of the end being heated to a yellow; and, in thirds, the tempering is procecded with as above.

"Care should be taken that the plunged tool, while tempering, be not held too long a time at a certain color line, as it has a tendency to break at that point. The tool should be slightly waved in the water. 'Pieces' which are to be tempered throughout must be allowed to soak, #.¢., become uniformly hot, before plunging.

"The proper color for a given ground is only ascertained by experience. Generally speaking, the picks and drills are stopped at a 'straw,' if intended for hard ground; at a blue, for mild ground. The toughness of the steel should be preserved as much as possible, therefore select the lowest color compatible with the service to, be performed. A high carbon steel is given a lighter color than steel of low carbon,

"A pick is made of a square iron bar 14" x 1" heated at the middle, and then struck endwise, till about 1%" across. This spot is softened, and at red heat cut open, and swelled by a drift to form the eye. This is then slit at the ends, and softened, while a 6" length of pick steel is being heated, When ready, this steel is tongued into the iron, and hammered. A reheating with borax, and a hammering complete the weld, after which the picks are sharpened and tempered; no signs of the weld should be visible."

" Pick-steel" is a special steel that can be had in bars 1%" or 1%"x %" or %"', and used only for tips.

Steel bars for drills come in lengths of about 14 feet each and from 5" to 2" diameter. The American " Black Diamond" brand isa favorite. The bars are cut into pieces as long as can conveniently be used, ¢.g., 30' and 36". The bits are wider than the tool, to prevent it sticking to the hole. They are wideried according to pattern, so they can "follow" well. The first drill has the widest bit; the followers narrower ones. In hard rock the flare is smaller than that in soft rock.

"The temper is a lighter color for hard than for soft rock. If the edges of the returned drills are cracked or broken the steel is too brittle, and should be made softer or other coal used. If the edges blunt much by wearing

round they are all right, though a harder temperature may give them longer life. Cast steel borers are never heated above cherry. They are annealed at the striking end."

Practical Suggestions And Points By A Blacksmith.

A prospector must have something to act as an anvil; a hard pebble won't do, he can carry a small anvil or a chunk of railroad iron. A small hand bellows or even a portable forge worked with crank will make his outfit complete. The following practical hints I picked up from a blacksmith whilst watching him at work tempering both picks and drills for some prospectors. He said: " You must temper your drill according to the character of the rocks.

"For hard rock, use a short thick edged 'bull bit' which will stand a high brittle temper such as 'straw.' For picks, a light blue color is a good temper, rather than 'straw' which is too brittle. Cherry red is the heat of your bar, not hotter; Jaying this on the anvil and hammering it well all over giv it toughness. If blisters show on the steel you must hammer it over again. By occasionally dipping your hammer in water and then striking with it, you get the steel down . - a fine grain. When you are dipping for tempering, put the point in the water, that cools the point, and the heat runs the color down to the cool point; when the color reaches the tint you want, then is your time to cool off quickly. The color progresses from a white or pale straw to copper color to blue. Copper tint is a good one to stop at for a drill,—blue, fora pick. The right moment to stop and cool is just at the turning point from one color to another."

He took a piece of steel, heated it to cherry red, laid it on the anvil and pounded it lightly with his hammer all over, to toughen it by blows, occasionally dipping his hammer in the water to " water temper" it; this further toughens it, by partially cooling it. Now the bar was again put in the fire and heated to a cherry red, care being taken not to keep the bar too long in the fire, as that would tend to take its toughness out, or produce blisters. The bar was plunged about an inch into the water, and then rubbed against a brick, to show the colors plainer. These passed from the point upwards, gradually through the colors we

have inentioned, to arrest it by suddenly cooling off at "straw," would make it too brittle for ordinary drills, ex. cept a" bull drill." Now the "straw" turns into a copper hue, a good point to cool off fora dri//. Now it passes into a blue, at this point it would be well to cool off for a pick. The edge of a drill is almost of secondary importance to the sharpness of the projecting corners; when these are gone, the drill is used up, and clogs in the hole. Some rocks like sandstone will, by reason of the quartz in them, wear off the corners very rapidly, others, like limestone or granite, less rapidly.

Another blacksmith advised me not to dip (as is commonly done) the point on/y an inch in water as it is apt in use to break at the water line, but plunge it @// over in the water. '" Who shall decide when doctors disagree?"

A prospector should take with him a regular blacksmith's hammer for sharpening, as well as the 4 or 5-lb. hammer he uses for striking drill or the rock.

Chapter Xxiii.

Some Elements Of Mining Law Rezating To Prospecting.

A prospector would do well to acquaint himself witha few elements of mining law, so we will give a few samples of Colorado mining law for his benefit.

Extent of Lode or Claim.—The length of any lode may equal, but not exceed, 1,500 feet along the vein.

Dimensions.—The width of lode claims in Gilpin, Clear Creek, Boulder and Summit counties, shall be 75 feet on each side of the center of the vein or crevice.

Certificate of Location.—The discoverer of a lode shall, within three months from the date of discovery, record his claim in the office of the recorder of the county in which such lode is situated, by a location certificate, which shall contain:

1st. The name of the lode.

2d. The name of the locator.

3d. The date of the location.

4th. The number of feet in length claimed on each side of the center of the discovery shaft.

5th. The general course of the lode as near as may be.

Discovery Shaft.—Before filing such location certificate, the discoverer shall locate his claim by first sinking a discovery shaft on the lode, to the depth of at least 10 feet, or deeper if necessary, to show a well-defined crevice.

Second, by posting at the point of discovery on the surface a plain sign or notice containing the name of the lode, the name of the locator and the date of the discovery.

Third, by marking the surface boundary line of the claim.

Staking.—Such surface boundaries shall be marked by six substantial posts, hewed or marked on the side or sides of which are in toward the claim, and sunk in the ground, to wit, one at each corner, and one at the center of each side line. Where it is impossible on account of bed-rock, or precipitous ground, to sink such posts, they may be placed in a pile of stones.

Open Cuts.—Any open cut or cross-cut tunnel}, or tunnel which shall cut a lode at the depth of ten feet below the surface, shall hold it, the same as if a discovery shaft were sunk thereon, or an adit of at least ten feet along the lode from the point where the lode may be in any manner dis- 'covered, shall be equivalent to a discovery shaft.

Time.—The discoverer shall have 60 days from the time of uncovering or disclosing a lode, to sink a discovery shaft thereon.

Construction of Certificate.—The location certificate of any lode claim shall be constructed to include all surface ground within the surface lines thereof, and all lodes and ledges throughout their entire depth, the top or "apex" of which lies inside of such lines extending downward vertically, with such parts of all lodes or ledges as continue to dip beyond the side-lines of the plane, but shall not include

any portion of such lodes or ledges beyond the end lines of the claim, or at the end-lines continued, whether by dip or otherwise, or beyond the side-lines in any other manner than by the dip of the lode.

Cannot be Followed.—lf the top or " apex" of a lode in its longitudinal course extends beyond the exterior lines of the claim at any point on the surface, or as extended vertically downward, such lode may not be followed in its longtudinal course beyond the point where it is intersected by the exterior lines.

Proof of Development.—The amount of work done, or improvements made during each year shall be that prescribed by laws of the United States.

Placer Mining Claims.—The discoverer of a placer claim shall, within 30 days from the date of discovery, record his claim in the office of the recorder of the county in which said claim is situated, by a location certificate, which shall contain:

ine The name of the claim, designating it as a placer claim.

2d. The name of the locator.

3d. The date of the location.

4th. The number of feet or acres claimed.

sth. The description of the claim by such reference to natural objects or permanent monuments as shall identify the claim.

Before filing such location certificate, the discoverer shali locate his claim:

ist. By posting upon such claim a plain sign or notice containing the name of the claim and of the locator, the date of discovery, and number of acres or feet claimed.

2d. By marking the surface boundaries with substantial posts sunk in the ground, one at each angle of the claim.

On each placer claim of 160 acres, not less than roo dollars' worth of labor shall be done by the first of August each year, and upon less or more ground a sum in proportion.

Index.

PAGE. TAL poser rar EC FEUE CUEALEU EERE ERT REED beh Ol 199, 204 RI iv hocks eke Cod RECEMC Er AO) 68 Ee OLEA EERE CRED EED UE 61 UME oes huh py WERE EH OER ERE COOK REO NEE COE HORS Eb 21, 27, 42 Argentite 0.00... cece cece reece ener neon ncn ener cen etneees 67 PT UN co CCL UE COREE HELE DERROOMEEE NEREL BORER CORE OCUIEED 240 PONE Uae he hen eines ceeues pen eVernercceenbber 68, 177 Augite BELG CEA CER UROL CURE ERCEE CEEOL AIEEE CECE Oe COBOL ES 54 13 (Fa Ce a arse ev re are AR rie ene UPURG TU Er st erlersverer ether yrar ure 55 IAGO aE CG CEEOL DOU RRO Coe bbus 25, 61, 62 PROACH MINI i ici ect cestneweerscrecvennseereeerege 121, 226 JL fa) ULES CL aR RIG a tere ne AEN CL Roe De ECSU Cer ut piariar Lia Wy ary 207 PGA S ea ech sal eeale RAUL He COME ECE Ub Cem Ee NEL Miles 88 PSEAITLCHUHETI ECS: 55h co eo odo ie ea bal OE ECOL SUI OONBEEUS 66 Pe Gk ie vite bev en Bs ob Weathered eenee be scene she 237 WT EE he cic ies beck CELE RAMA PL LER beeece cre hee rEnne 112 Ee VEE oak evi chen wis bike eneamncceunnndrs 79, 80, 162 Blossom : SPIE RICCI ER TEE UR EE TLES REED 94 Me Dre NONG ey eek ee chee UEC Ee ees 23 ee rN io os BEd FRO CEL Cans CORECLEU RENAE 231 DONWINE DEINOE ii cre eeci ee heed bere iearerecncebnrens 126 SRO CONE ooo cian) 1 en Medco ro Scere See Oh oveitie ea bs Toe bebo pae ole teal aigualers 62 PGCOIRING: VOIR: Ceicii ices cckeeblrevianeketeons covet auce ee) 82 EAPTUIOR MEIMOIOR Ly 6 cs ea Cire hice ie Renee Chere Eee 213 PPD COLMA oo ccc es cer exert ete breeensecbarede 200, 214 MOV RLOINE MIM GT. cies. beer facs CR bo Lees base pen) a nbacrk ae 68 [CUO SARA sans lly Satta ra ese i rianae Ren T ca Oya Mareen ire Siem aca sri 55 WO RITA, ics ck nlereih shock badly pe aasecace ere Qa eee ecaeaibace e bade ama d 223 CRUSOE. PIACONE i56c Siar Co aoe Sareea hea thee ekenesces 224 CAMIDTB oe oe VON aeak ne oe LP a ek aL aed 22, 30, 42 CONVORB Ee hie Vetere er ee renee s Dees geben Been ec nee 38 aT]... Seana ee renner aaa tere arerer near ar arr rarer era ter pegare uty' 69 CBLOOMIOTOUG occ Oat Cob Ree eed ebewey ebenmens 23, 33, 45 CRU er EO ITA IE AE be IC ES 203 NN ee ts OOS a hE Ls GA 174 CGTGBRIG 5 i Se EAN AION RED, bee DH GR LAURE 70 GGURS WI DON co cic sek ve cee dee eevee evenrere tyne et 104 CHOMIStY Of ROCKS... ii ctor nto re emer e een neeebedere nes 143 CT ee aes seine coven utlensde bane hid Wid utun Huauaticdte War aticheR ave NES 55

PAGE SE oe SERRE HAE Cu Khe ELE COTR ERE MERTENS TEE LEAR ERED SEES 24 COTA PIMONTD oc iikicedccccedeeerehereeeecennenererecceves 123 COMME SOMONE i ciceseetetirtrnbeebereensedeee eoneeehews 76 pen ag LGEEC HPAP ESEE CRE ET ROUSE MEMCLD BRO R eer OreE bes 79, 101, 162

REG ae CLL PE OIE VEL e DEEP RCEENS CehD rie gurbes eb bearer 70 Country PO EUCLA WENDEL ECTREC ESC AGED EN COREE B ECO URLED 104 Cee ar lita kee henie hes Cee eecbabeebeweterl 24, 35, 47 GORE CUOO civ irbebhrebes bev ceeseusee cere: used 137, 151, 245 RR N ey CeehHe Noreen eben ea cesar beer eee hem ER 109 CNT iiiiie 6 Glin tod MOU RERL. CURR EUR LEM EERE ROERROE ERE 84 BN ie baba Rc ce cei UAE Oh PERE RE ELDER SE REC ER OMELET 233 DION OP elise ineceh Curt setae tunemecheeeeradee tue IIg 226 RE Fh) Sree ewe PRANK R MeCRORIUTE eb ce ERR EL eara Oe 31, 44 PEE GEE ache dldene et urbe nner nedeberebwans MeeuNE 81 oe GAL Gk CERES CE CRP RRERETRR CRUE LOR ROO 59, 219 PEMTTO UU R eet Olek COLA CACER NER EPOrELE WS USEREROLE EES 55 PAIR RERINYE osc f 4 156 Gale'a.d6 KG EKE Ode weno heey bad ceentre 182 BREE ES oc. Gk iu Ab, Ohh bs CLK Sikh eRe REO LMU iE HR 253 BOR eC RELA RERTUREE GHED EL RIA Bebe be KE KOK REET DMEM HER 101 OI oe cance enees DUL MOO MedbneeeTeehny Re kemE ens 26 Education of Prospector. ccc cece ee cee eee eee neon 8 TROT OGM ekki ee eee een bebe eee ede 61 ROME hVAt eC eRe CHOI ENE Cera EEE RCEMEC ERE REEER Parrerige 1, PEPPIRU MR OROGE isis Gees chaenecee nee bent oeeeaed MELON e REN 99 RMIATIUG OFINGE: Cok ocean Gh Chess Che cehe beeecnenpapenenes 187 BAS yee Cee MELA AVEC ALER 24 Ch Ob Chie sb Uoees eBe be 74, 84, 86 PGURE , oU ReR MELE TC HCOR REE UECEL EM MneheN Dime as ael panera 54 Fissures PREM OE 8.8 CR OES TEE Lace HEL ELLER nen 140 Fissure Veins 0000. 82, 89, 93, 96, 103, 125, 132, 258 IM MOGO ee este Ki NEVE Ree ROM HERE ECE) Cerebus VE mebN 55, 63 RR eNO eh ae hae CE LES EMR OCL CHOC RL Eee Ches Le Ea 86 POlding ANG: FPAUING occ cece core eseweeeeee eoenetoneens 77 BOURNE: 6 oad ck ei beecereUs toes ANP ay Panes etal gue ora Beare a 39, 41, 42 PROM ee OPN dA MESMERL Gel P ERE ed Redes Kew UP OUR TLS 203 POM icc ce cecyieiaimelosc en einlewne canaaceneeaancts 78 WENN Reta yl ne ops saya pak cubs 6 whe oh Hb tak NED Abe 8054 hag @c0 OTNLAL 8-8) os 55 Generalized Section of Rocky Mountains 065 21 Geological Section of the Earth's Crust 0...00 0s 17 GOOlOGICAl: PHANG ie ics ces eri h a pd eedeser ees ereenenet 15 GIAGISD POOH vive Rep ew hres See mee eb bcp elk © anne pate € 37 CO YTMRFR Fete coe gta: acre i gayi) ae Shae AIR AC Bude MUN HVE Bb BHeNE OER SSReN ASE Ble FINRS 56 Gold in Archeean Rocks. cece cece cee cece nee eees 29 GOOLE LE WETEUMER oes tis eau Wie sek beas ose eakciasban Marck baie A Rae eaves pee Ona 221 CPO ticle vad chain ana Had Wate ndin aoe s Bed kebab back 55 CRAY COPDO li nies Cals bebe Fee Gn noe maa wha tele le Wess ofemure eee 65 GRO TIB UTED Buss sacep cece acny. cane ace Lae eeu diec gate rege ode eae erenaeeS 55

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