BANCROFT 
 LIBRARY 
 
 THE LIBRARY 
 
 OF 
 
 THE UNIVERSITY 
 OF CALIFORNIA 
 
THE- ORES OF Li: ILLE 
 
 
 MORNING EVENING STAR M 
 
 
 METHODS OF THEIR EXT > s 
 
 
 LOUIS D. RICKETT- 
 
 Ward Fellow in Economic ' 
 
 
THE ORES OF LEADVILLE 
 
 AND 
 
 THEIR MODES OF OCCURRENCE 
 
 AS ILLUSTRATED IN THE 
 
 MORNING AND EVENING STAR MINES, 
 
 WITH A CHAPTER ON THE 
 
 METHODS OF THEIR EXTRACTION AS PRACTICED 
 AT THOSE MINES, 
 
 BY 
 
 LOUIS D. RICKETTS, B.S. 
 
 fc s 
 
 Ward Fellow in Economic Geology of the College of New Jersey. 
 
 WITH FIVE PLATES AND ONE COLORED LITHOGRAPH. 
 
 PRINCETON, 1883. 
 
*f 
 
 ibr 
 
 ft Library 
 
 PREFACE. 
 
 In accordance with the requirements of the W. S. Ward fellowship in Eco- 
 nomic Geology for the year 1882-3, I spent over four months of that year at Lead- 
 ville, and devoted my time to a study of the ores and their modes of occurrence, 
 and to the extraction of ores in the Evening and Morning Star mines. 
 
 To these mines I had free access, and would here tender my thanks to their 
 officers, who afforded me every facility in their power for the prosecution of my 
 work. The analyses of the rocks and ores were made and the thesis completed 
 at the School of Science, Princeton, during the remainder of the college year. 
 
 I have been greatly stimulated throughout by the personal interest taken by 
 Mr. Ward in the work ; and it is at his request and expense that this thesis, writ- 
 ten in compliance with the terms of the fellowship, is published. 
 
 Part First is also presented as a thesis for the degree of Doctor of Science. 
 
 L. D. RICKETTS. 
 
 PRINCETON, N. J. 
 
 June, 1883. 
 
PART FIRST. 
 
 THESIS FOR THE DEGREE OF DOCTOR OF SCIENCE. 
 
INTRODUCTORY. 
 
 This thesis does not so much attempt a general description of all the mines 
 of Leadville as a more particular description of the mines to which the writer has 
 had free access for several months. And it is hoped by a more detailed descrip- 
 tion of these quite extensive mines to give a better idea of this type of deposit 
 than could be done by a more superficial description of a greater number of 
 mines. Other mines, both on Carbonate and Iron Hill, have been visited in 
 order that common features may be noted and peculiarities distinguished, but 
 almost all the data for the following pages have been derived from the MORNING 
 and EVENING STAR MINES. 
 
 The Morning Star especially has been studied, for this mine is only at pres- 
 ent undergoing development, and large bodies . of ore stand open, completely 
 explored by drifts but otherwise untouched,"thus affording most excellent oppor- 
 tunities of examination. 
 
 The Evening Star, on the other hand, is much smaller, and the ground devel- 
 oped is practically 'exhausted. Its enormous ore-body has been removed, and 
 only lofty cribbing and timbers, reaching up set over set, show the great 
 spaces once occupied by almost pure ore. The present shipments (October and 
 November, 1882) are obtained from the smaller ramifications of the ore through 
 the gangue, and the apparently interminable number of these smaller bodies 
 promises to be the source of much more ore. Further prospecting work is now 
 being pushed forward, through which it is by no means impossible that new 
 ore-bodies may be struck. It would be truly rash to assert that the Evening Star 
 mine is nearly exhausted without adding the qualifying clause, if new ore-bodies 
 are not presently developed. 
 
 The excellent report of Emmons, an abstract from his final report on the 
 geology and mining industry of Leadville, has been of the greatest assistance to 
 the writer, and is used as an authority in the short description of the general 
 geology deemed necessary for an intelligent comprehension of the subject treated. 
 For a fuller description of the general geology that pamphlet is referred to, as 
 
8 INTRODUCTORY. 
 
 space for this is lacking here. The statements of Emmons concerning the strata 
 and their nature at different horizons have corresponded very well to the facts 
 gathered in the limited field here treated. As will be mentioned later, the posi- 
 tion of the Carbonate fault is found to be further down the hill than it is stated 
 to be by that authority, and indeed no direct evidence of its existence could be 
 obtained on the property. These and a few other points of minor importance 
 rendered apparent by the developments lately made on the lower part of the 
 properties disagree with his statements. All the others correspond very nearly. 
 
GENERAL GEOLOGY OF THE DIS- 
 TRICT. 
 
 The stratified rocks about Leadville are almost altogether Palaeozoic, with an 
 immense amount of Quaternary debris on the lower slopes of the hills, and run- 
 ning into and over the broad valley of the Arkansas. Between certain of these 
 stratified Palaeozoic beds are found a complicated series of interlaminated intru- 
 sive sheets of the igneous rocks so intimately connected with the ore-deposits. 
 The upper part of the Mosquito Range and of the opposite Sawatch Range is. 
 composed of Archaean rocks, principally granites and gneisses. These are of dull 
 colors, for the most part gray and pinkish. Gneisses predominate, and in these 
 a distinct bedding is often recognizable. They split up and disintegrate along 
 these lines as well as along the jointing planes. Frequently, along the Sawatch 
 Range at least, they are intersected by dikes of igneous rock which weather to 
 thin plates and blacken and form prominent stripes of slide down the mountain- 
 side wherever they occur. 
 
 The sedimentary beds form a belt around the base of these mountains and 
 extend well up on their sides. About the granitic rocks and immediately above 
 them there is a bed of quartzites of the Lower Silurian age. It has an average 
 thickness of about 1 50 feet. This sheet is not homogeneous, but consists of nume- 
 rous layers of quartzite, some shales and some calcareous rock. The lower half 
 is by far the more pure. Conformably upon these there follows a bed of impure 
 siliceous dolomite, and then, ending the Silurian formation, a thin though gener- 
 ally persistent stratum of quartzite. This stratum is both thin and irregular. Its 
 thickness varies from 10 to 40 feet. Emmons thinks this irregularity in thickness 
 may be due to erosion, especially as he was unable to find any Devonian formation 
 at this point. This stratum was the only one not identified on either the Morning 
 or Evening Star, and, as the White limestone was found to be much thinner here 
 than the average, erosion may have removed all of the quartzite and a part of 
 the limestone at this place. 
 
 The Carboniferous strata are the most important, as it is in these that all the 
 ore of Carbonate Hill and almost all that of the rest of Leadville is found. They 
 consist first of a layer of blue dolomite, very pure when unaltered, but in the 
 
10 OCCURRENCE OF THE ORES. 
 
 neighborhood of the deposits very much stained and changed. This is the stra- 
 tum in which the ore occurs. The rest of the beds of this formation form a series 
 of coarse grits and sandstones, with a few narrow layers of dolomite. When 
 least eroded they are 2500 feet thick, but in the vicinity of the deposits now 
 worked they have been almost entirely washed away. 
 
 Although places have been found where the various sedimentary formations 
 succeed each other without interruption, such occurrences are extremely rare. 
 There is scarcely a spot where," at some horizon, igneous rocks have not 
 forced themselves in between the strata. These igneous rocks are acidic. They 
 are regular quartz-porphyries or felsites, and are called by Emmons, and generally 
 throughout the camp, porphyries, and that is the name that will be given them 
 here. Many varieties may be recognized. White and Gray porphyry, of which 
 more hereafter, are the varieties most intimately connected with the ore. These 
 rocks are, comparatively speaking, seldom found in ordinary dikes, but occur 
 for the most part as intrusive sheets, following the bedding of the formations in 
 which they occur. Regular overflows are never found, and if they had once ex- 
 isted erosion would long ago have removed them. The most important sheets 
 of porphyry occur above the Blue limestone, or in it. The larger occur above it. 
 In thickness they average about the same as the Blue limestone, though in some 
 cases they are much thicker, and on Carbonate Hill the White porphyry almost 
 certainly attains a thickness of 1000 feet. 
 
 Besides this great complication, due to the intrusive masses of porphyry, the 
 geology of the district has been rendered additionally complex by a series of 
 faults which break the continuity of the beds. That these were made after the 
 eruption of the porphyries is proved by the latter being broken too. Like evi- 
 dence proves that the faults occurred subsequent to the deposition of the mineral 
 matter. In direction the principal of these faults have a trend north and south, 
 parallel to the mountain-range, though numerous minor faults run off from these 
 at various angles. There are five or six of the larger ones. The western wall has 
 fallen on all but one of them. Only two of these faults have any connection with 
 Carbonate Hill ; the Carbonate fault, running along the western slope of the hill, 
 and the Iron fault, far to the east and dividing Carbonate from Iron Hill. The 
 deposits were first discovered on the exposures made by erosion along these 
 faults or the anticlinal folds in which they terminate ; for here the superincum- 
 bent rock has been worn away and the ore itself, or the iron so indicative of ore, 
 brought to the surface. The deposits thus outcrop like enormous contact veins, 
 and some of the early locators took their claims parallel to the outcrop, supposing 
 they could follow the ore with the pitch for an indefinite distance, a right denied 
 them by the local courts, on the ground that the ore is not continuous from the 
 outcrop down. 
 
POSITION OF THE DEPOSITS. II 
 
 POSITION OF THE DEPOSITS. 
 
 The principal mines of Leadville are situated on Fryer, Iron and Carbonate 
 Hills, all three of which form a group together at the foot of the Mosquito or 
 Park Range of mountains. The distance from the summit of Carbonate Hill to 
 Fryer Hill is about one mile to the north, and from the same point to the top of 
 Iron Hill is three quarters of a mile south-east. By far the larger portion of the 
 ore of the camp is derived from these three hills. Fryer Hill has so far produced 
 the most, and Iron Hill next. It is Carbonate Hill that principally interests us. 
 
 Carbonate Hill lies south-east of the town of Leadville, and rises directly from 
 its outskirts. Its summit rises to a height of over 10,600 feet above the sea-level, 
 and over 400 feet above the main street of Leadville. To the east it slopes gently 
 to the valley which divides it from Iron Hill. To the south it slopes into Califor- 
 nia Gulch, and to the north into Stray Horse Gulch, which divides it from Yan- 
 kee and Fryer Hills. The claims which now have shafts sunk are situated along 
 the western, south-western and north-western slope of the hill, and the oldest, in- 
 cluding the Carbonate, Glass-Pendary, JEtna, Catalpa, Evening Star, Morning 
 Star and Henriette, are along the outcrop of the ore-horizon, which approxi- 
 mately follows a contour about 200 feet below the summit of the hill. This outcrop, 
 unlike the others, is covered with very little wash, much less than on Fryer Hill, 
 yet it was late in being discovered. The distance of this outcrop to the Iron 
 fault is about three quarters of a mile. 
 
 The Evening and Morning Star mines lie side by side on the north-western 
 slope of the hill. The former lies to the south-west of the latter. The Blue lime- 
 stone outcrops on the lower quarter of each claim. The Evening Star, though 
 one of the best, is one of the smallest mines in the camp. It is a little less than 
 half a claim in size, being 1305 feet long by 163 feet wide, or less than five acres 
 in area. Its bonanza was so thick and covered so much of its area that it has 
 afforded an enormous quantity of ore. Its location was in fact an extremely for- 
 tunate one, for it cut the great ore-body of this part of the hill through its thick- 
 est and richest part. If the nature of the body had been exactly known a better 
 belt of this width could not have been chosen across it. To the south the ore be- 
 gins to thin into the Catalpa, and to the north into the Morning Star, and it 
 never again approaches in either of these mines the thickness it attained in the 
 Evening Star. 
 
 The Morning Star mine lies next to the Evening Star. It is a consolidation 
 of a number of smaller claims, of which the old Morning Star and Waterloo 
 claims are the most important. It extends in width to the Henriette line, a dis- 
 tance of about 502 feet. Its eastern boundary is continuous with that of the Eve- 
 
12 OCCURRENCE OF THE ORES. 
 
 ning Star, but it extends further down the hill than the latter claim. The lower 
 part of this property, however, is of little or no value, and there are now no work- 
 ings run below 1300 feet from the east end. The relative size of the claims may be 
 seen on Plate II. In both mines the ore occurs immediately below porphyry and 
 in Blue limestone, as will be later fully described. 
 
 GEOLOGICAL STRUCTURE AT THE MINES. 
 
 The Evening Star mine is principally worked through four shafts. A fifth, 
 now unused, is near the Forsaken shaft. A sixth, No. 9, Plate IV, has never had 
 a drift run from it. It has, however, greatly aided in a thorough understanding 
 of the formation, for it has been sunk nearly 200 feet into the Blue limestone hori- 
 zon, and from this point a diamond-drill boring has exposed the succeeding strata 
 for 200 feet more, and has thus given a key to the nature of the underlying for- 
 1 mations. The Morning Star is worked through four shafts on its own property, 
 and a fifth on the Evening Star ground, sunk conjointly by the two companies 
 and used alternately by them. Three other shafts have been occasionally used 
 but are now idle, and numerous prospecting shafts, or rather pits, also aid in study- 
 ing the formation. The fact that the Morning Star is a consolidation of several 
 claims explains the existence of so many shafts. The new McHarg shaft, now 
 being sunk, was started October 1882, and is the only one that the present com- 
 pany has started. These numerous shafts and the underground workings which 
 connect certain of them together have given a complete key to the geological 
 structure. The data from which the conclusions are deduced are given, and ac- 
 companying these are two cross-sections, one through each mine. One of these 
 sections, Plate III, is through the Morning Star, and is made along the dip of the 
 beds. The shafts are projected on this plane and their depths given. A line of 
 levels was run over the surface to determine the relative heights of the shafts at 
 the top. The Evening Star is such a narrow claim that all the shafts lie nearly in 
 one plane in that section. The same number indicates a particular shaft on the 
 plan, Plate II, and on the sections, Plates III and IV. The numbers indicating 
 the various shafts are as follows : 
 
 1. Upper Waterloo shaft. 
 
 2. Morning Star main shaft. 
 
 3. Boarding-house shaft. 
 
 4. Discovery shaft. 
 
 5. Old Waterloo shaft. 
 
 6. Lower Waterloo shaft. 
 
 7. Forsaken shaft. 
 
THE MORNING STAR SECTION. 13 
 
 8. Old Forsaken shaft. 
 
 9. Evening Star No. 5 shaft. 
 10. Evening Star main shaft, 
 u. Evening Star upper shaft. 
 
 THE MORNING STAR SECTION. 
 
 The deepest shaft pf this section is No. i, the Upper Waterloo. It is the one 
 furthest up the hill. This shaft begins in the White porphyry and passes through 
 it for a distance of 360 feet. At this point the contact between the latter rock 
 and the Blue limestone is reached, and fine ore is immediately struck. The 
 second level, not shown in the section, is 45 feet below this point, and from here a 
 drift runs to the end of the property 120 feet distant, where contact is again 
 reached. All this region shows large bodies of fine lead-ore, which is indicated 
 by pen-dotting on both sections wherever it occurs. Below the Upper Waterloo 
 the Morning Star main shaft, No. 2 on the section, is the next. The surface at 
 this point is 33 feet lower than at No. i. The shaft, always measuring from the 
 collar, which in this case is a distance above the surface, is 265 feet deep to con- 
 tact. From here a main track incline, not shown in section, runs immediately 
 below the porphyry and along the contact to the end of the claim, a distance of 
 480 feet. This incline is connected with the Upper Waterloo workings in several 
 places, and the contact is always regular and void of all signs of disturbance. 
 The Boarding-house shaft, or what Emmons calls the Lower Morning Star, is 
 about 680 feet below the Upper Waterloo. It is shown on the plates as No. 3. 
 This shaft passes through 75 feet of White porphyry to contact. It is connected 
 with the shafts above by workings which show the porphyry to be continuous all 
 the way along, and undisturbed by any break. No. 4 on the section, which is 
 merely a prospect-shaft, sinks only 38 feet to contact, and here an incline runs for 
 some distance, between ico and 200 feet, and shows a regular contact. 
 
 If we connect the points where these shafts pierce the surface and those 
 where they strike the .contact we will have a section of the White porphyry, and 
 by producing these lines down the hill till they meet we have the point where 
 the White porphyry ceases. Immediately below the Blue limestone outcrops, or 
 rather what was once the Blue limestone, for it is here for the most part replaced 
 by vein matter, chiefly oxides of manganese and iron. This outcrop, in spite of 
 the wash being in considerable thickness, is very plainly marked by the numerous 
 boulders of iron-ore which are scattered in a broad belt along the face of the hill. 
 It curves around the hill, running almost due east across the Henriette, and fol- 
 lowing the contour of the hill quite strictly. Numerous pits sunk by early pros- 
 pectors along this zone show nothing but the iron-ore on the dump. 
 
14 OCCURRENCE OF THE ORES. 
 
 The lower shafts belong to a different series, as they develop the ore under a 
 second sheet of porphyry. They are many in number, but occupy little space in 
 the section, as they all start near the outcrop of the second sheet. Most of the 
 shafts have struck valuable ore here, and the Henriette has all her ore at this hori- 
 zon. The Forsaken shaft, No. 7, Plates II, III, and IV, sinks 80 feet to contact, and 
 25 feet further to a second level, from which a drift runs to contact. Owing to 
 there having been no record kept of the ground passed through in sinking this or 
 any of the other shafts, it was difficult, and in one case impossible, to note the se- 
 quence of the layers or sheets passed through by them. In this shaft and in the 
 Old Waterloo this was only obtained by climbing the ladders and looking between 
 the round timbers whenever these were wide enough apart. It was especially 
 difficult to do this in the 'Forsaken shaft, as the walls were generally some dis- 
 tance from the cribs and the intervening space was filled with wooden blocks. At 
 the top there was only wash, boulders of iron-ore mixed with water-worn pieces of 
 porphyry. More solid iron appeared below this and continued very nearly to the 
 porphyry. Here a zone of impure though undoubted limestone occurred, which 
 could be traced for 4 or 5 feet above the porphyry. Small pieces pried out 
 showed the rock to be highly impregnated and .discolored by metallic oxides, 
 though it effervesced freely-with warm dilute acid. At 35 feet from the surface 
 Gray porphyry was entered, and this rock continued to the first level, 46 feet 
 below. The layers passed through by this shaft were then as follows : Wash, 1 5 
 feet; iron-ore in place, from 15 to 30 feet; limestone in place, from 30 to 35 feet; 
 porphyry, from 35 to 8 1 feet. 
 
 Below the Forsaken this sheet of Gray porphyry outcrops, as shown by the 
 Old Forsaken shaft, No. 8, Plate III, which begins in that rock, and strikes the 
 contact and ore at only 25 feet below the surface. The Forsaken workings follow 
 the ore right to the outcrop, where the ore and wash mix with each other. The 
 Portland shaft, not shown in the section, is a little further down the hill and does 
 not touch the porphyry, but sinks down through iron-ore far below the ore- 
 horizon and into barren ground. 
 
 The Old Waterloo shaft, No. 5 in the section, affords the best view of the 
 ground along the zone below the White porphyry. This shaft, which is 135 feet 
 deep, strikes the contact at 129 feet. There is but one level, from which two 
 drifts are run ; one horizontal, following the strike of the porphyry, and one an 
 incline which follows the dip. The latter is shown on the section. The same iron- 
 boulders and wash, merging into iron-ore in place, was passed through as in the 
 Forsaken. At a depth of 63 feet limestone appeared, which soon became solid 
 and quite pure, and which continued for 18 feet. At the top of this limestone 
 layer there were seams of yellowish and much decomposed rock which resembled 
 precisely some of the limestone found below the porphyry. Lower down the 
 
THE MORNING STAR SECTION. 15 
 
 rock became massive and as pure as any encountered below the porphyries either 
 in the Morning or Evening Star. The color of the more pure was hardly changed 
 from the normal blue. The bedding-planes were plainly marked and corre- 
 sponded in dip to all the sedimentary formations. The Gray porphyry began 
 below this limestone. The contact between the two was finely shown, and the dip 
 of the porphyry sheet was markedly different from that of the limestone layers, 
 being much steeper. The existence of this limestone in place above the porphyry 
 is alone sufficient, if there were no other proofs, to show that this sheet is a 
 different one from the main sheet above. 
 
 As to the Lower Waterloo shaft, it could not be examined, so that the thick- 
 ness at that point is not known. A rough record kept of the ground passed 
 through in sinking the Evening Star shaft No. 5 (No. 9, Plate IV) shows it to have 
 there had a thickness of 50 feet. 
 
 It will be seen on referring to the section that the Gray poryhyry has a much 
 steeper dip than the White. This dip, though it has been maintained as far as de- 
 velopment has gone beneath it, may lessen further down. Thus far it has cut 
 across the limestone bedding to a lower horizon. Its course below the point 
 where development has been carried is unknown. The course it probably takes is 
 indicated in the section, this part of the outlines of the sheet being put in in broken 
 lines. The Gray porphyry has been followed over 400 feet from the Lower 
 Waterloo shaft. This distance takes it far under the White porphyry sheet. In 
 fact, directly over the line of this incline, and only 205 feet from the shaft, there is 
 an old shaft but 20 feet deep, which, though the bottom is filled up, shows walls of 
 White porphyry, solid and apparently in place. Consequently the Gray porphyry 
 has been traced at least 200 feet beneath the White. 
 
 The evidence of a second sheet of porphyry of no great thickness existing 
 below the main sheet is therefore indisputable. This fact is recognized by 
 Emmons, who mentions that the Half-way House and Henriette claims are on it, 
 but owing to the undeveloped condition of the ground at the time of his survey 
 he did not think that the Forsaken was under the same. He considered the For- 
 saken and the Lower Evening Star shaft (No. 9, Plate IV) to be under White por- 
 phyry, but cut off from the rocks above by a fault (the Carbonate fault) whose 
 western wall had fallen. This fault he thought also ran above the Waterloo shafts. 
 Recent workings have shown the Forsaken and Lower Waterloo to be under 
 the same sheet of porphyry, for they are connected, and pay-ore runs from one 
 shaft to the other almost without a break. Moreover, it has been shown that the 
 White porphyry is broken at no point from the upper end of the claim to the 
 point where it ceases, and that the Gray porphyry runs beneath it without a 
 break for at least 200 feet. Consequently there can be no fault between the upper 
 and the lower shafts. Acknowledging the existence of a second sheet of por- 
 
1 6 OCCURRENCE OF THE ORES. 
 
 phyry alone, there can be no doubt of this, for then there is no possible room for 
 the displacement such a fault would cause. 
 
 The Gray porphyry goes unbroken to its outcrop. Below this no ore has ever 
 been taken out. Some of the shafts below this outcrop have been sunk quite deep, 
 but none could be visited as work was abandoned on them. Porphyry was cer- 
 tainly never struck in any of them. The Niles and Augusta, just below the Even- 
 ing Star, was sunk all the way through the White limestone and into the upper 
 strata of the Cambrian quartzites, so that these lower formations must come quite 
 near the surface at this point. No shaft along the foot of the hill strikes White 
 porphyry. The fact that the fault does not lie above the outcrop of the second 
 sheet of porphyry by no means proves that one does not exist below. If, however, 
 it does exist below, the displacement must be much greater than that inferred 
 by Emmons (170 feet). It seems more likely that the outcrop of the Blue lime- 
 stone marks the crest of an anticlinal fold which the beds make at this point, and 
 which has been eroded until the White porphyry cap has been worn completely 
 away. 
 
 The section through the Evening Star, Plate IV, has been used in this descrip- 
 tion as well as the other section, Plate III. It shows little that has not already 
 been mentioned. In this section the Gray porphyry is seen to send up a wedge- 
 shaped dike into the limestone, which almost reaches the White porphyry. Such 
 dikes, breaking up from the lower sheet, occur elsewhere. 
 
 To sum up, the following are the important points regarding the ore-bearing 
 sheets : 
 
 (1) All the formations dip towards the south-east (.25 to 30 S.). To this there 
 is no exception. At the same time the surface rises towards the south-east. 
 
 (2) The upper sheet of White porphyry is not continuous over the face of the 
 hill, but the Blue limestone outcrops below it. 
 
 (3) A second sheet of porphyry different from the first lies below it. The 
 intervening space of about 175 feet is taken up by vein-matter or Blue limestone. 
 
 (4) No porphyry sheet of any kind has yet been developed, and no ore found 
 below the outcrop of this second sheet of porphyry. 
 
 (5) The formations from the eastern end of the properties to the outcrop of the 
 second sheet of porphyry (Gray porphyry) are undisturbed by fault or fold. 
 
 The formation below the Gray porphyry is well shown by the No. 5 shaft of 
 the Evening Star (No. 9 on Plate IV), or rather by the core of a diamond-drill 
 boring made from the bottom of it. A meagre record preserved of the ground 
 passed through in sinking this shaft gives only the depth at which Gray porphyry 
 was struck and the thickness of the sheet. As the shaft was not in use and had no 
 ladders it could not be examined^but the dump showed only iron, Gray porphyry 
 and Blue limestone, but no parting qnartzite. The drill-core also showed no 
 
THE WHITE LIMESTON&. fj 
 
 trace of the latter stratum, but White limestone began immediately. This rock 
 continued for a distance of only 100 feet, and then the sheet of Cambrian quartzite 
 came in and the rest of the boring was in this formation. There was no way of 
 determining the exact boundary between the Blue and the White limestone, and 
 it is accordingly put in in broken line. It will also be seen that at this point the 
 White limestone has not its average thickness (about 1 50 feet according to Emmons). 
 
 DETAILED DESCRIPTION OF THE VARIOUS ROCKS. 
 
 The various formations and their order of occurrence having been described, 
 there remains to be given some idea of their nature and characteristics before 
 leaving them and passing to the especial consideration of the ore-deposits and 
 vein-material in the Blue limestone horizon. The different rocks will be taken in 
 order, beginning at the bottom and going towards the top. 
 
 THE CAMBRIAN QUARTZITES. This formation, though not entirely passed 
 through by the drill, was, in all probability, nearly pierced, for the description of the 
 strata given in Emmons's report closely tallies with the section here exposed, and 
 would lead one to infer this. As it is, the lower 100 feet of the boring is in this forma- 
 tion. At the bottom of the boring the rock was very hard. No large pieces of core 
 came up, but generally coarse powder and small fragments of very hard quartzite of 
 dull gray color. A few feet further up the ground was more impure and contained 
 much ferruginous material. Numerous assays, made by Mr. Bonner, the assayer 
 at the Evening Star mine, show that this material carried silver. One sample gave 
 him 14^ ounces, and another 5 ounces ; all the rest ran much lower,. An assay of 
 material very near that which ran 14^ ounces gave the writer only if ounces. This 
 impure streak ceased 8 feet above the bottom of the boring, and very pure, white, 
 saccharoidal quartzite came in and continued with but one break for 60 feet. The 
 break was caused by an impure streak 10 or 12 feet thick near the bottom. At 70 
 feet from the bottom the quartzite began to be impure. Red, iron-stained, calcare- 
 ous quartzite came in which at times showed micaceous specks. The succeeding 
 space of 25 or 30 feet marks a gradual change into the White limestone, and is 
 occupied by layers of impure rock sometimes containing little calcareous matter 
 and sometimes a great deal. Some of these layers are shaly, and one streak of 
 very fine-grained argillaceous shale, soft, slaty and of even texture, occupied a 
 zone of 8 or 10 feet just at the top of these quartzites. This stratum comes in 
 mixed with almost pure quartzite, and goes out mixed with impure limestone. 
 
 THE WHITE LIMESTONE. The White limestone comes in above the quartzite, 
 but the change is so gradual that no point can be taken as the boundary between 
 the two. It is most impure and siliceous at the bottom, but is characterized 
 
i8 
 
 OCCURRENCE OF THE ORES. 
 
 throughout by a high percentage of silica. It contains very little organic matter. 
 The color is a dirty white or grayish, very different from the characteristic blue 
 of the Blue limestone. An analysis of this rock is given a little further on. The 
 drill-core showed very little vein-matter in this rock, only a few streaks of wad 
 tilling crevices. These occurred near the upper part of the bed. 
 
 THE BLUE LIMESTONE. Although this rock contains all the ore, and though 
 all the workings are situated in its horizon, the drifts seldom directly encounter 
 the rock, as they run where the ore and other vein-matter occur. The limestone 
 has, however, been struck in some places both on the Evening and Morning Star, 
 and especially in the southern workings of the Forsaken and Lower Waterloo. 
 It is always stained and altered in color, and more or less highly impregnated 
 with iron and manganese. Some of the shafts which have been sunk deep into the 
 formation have struck more pure rock, notably the upper Evening Star, at ico feet 
 below the White porphyry. An old quarry on the side of Iron Hill, towards 
 California Gulch, from which this rock used to be taken for fluxing at the smel- 
 ters, shows a face of 35 or 40 feet of very pure Blue limestone. Here it is massive 
 and deep gray-blue in color. It shows the bedding-planes very perfectly. The 
 only thing that breaks its homogeneity is the narrow streaks of calc-spar which 
 have frequently separated along the bedding-planes. The rock splits easily along 
 the bedding-planes, so that flat plates may be split off six inches or more across. 
 
 An analysis shows the Blue limestone to be a very pure dolomite. The rock in 
 the mine resembles the rock exposed in the quarry in every way except purity and 
 homogeneity of color. The specimen already referred to from the upper Evening 
 Star shaft was just like the quarry rock, even in color, but was the only perfectly 
 pure specimen found in either mine. Wherever found elsewhere it was always 
 stained brown by manganese and iron, and altered in composition by the addition 
 of these ingredients and of silica. The bedding is always easily recognizable even 
 when in a very much altered state. Below are given three limestone analyses. No. 
 i is of the White limestone ; No. 2 is of a pure specimen of Blue limestone from the 
 quarry on Iron Hill ; No. 3 is of a very much altered specimen of Blue limestone 
 from near the White porphyry in the Upper Waterloo. 
 
 
 I 
 
 2 
 
 3 
 
 
 
 
 6 87 
 
 Iron sesquioxide and alumina. 
 
 i 18 
 
 o 28 
 
 i -*8 
 
 
 
 
 
 
 
 
 28 64 
 
 Magnesia 
 
 i* 48 
 
 
 
 
 
 46 80 
 
 
 Sulphur trioxide 
 
 O7 
 
 
 nc 
 
 Phosphorus pentoxide 
 
 
 
 
 Organic matter , . . 
 
 
 jo 
 
 
 
 
 
 
 
 IOO.O6 
 
 100.05 
 
 99.91 
 
THE GRAY PORPHYRY. 19 
 
 The very high percentage of silica in the White limestone is characteristic of 
 that rock. The very low percentage of silica in No. 2. is prominent. No. 3 has 
 probably derived much of its silica from the porphyry, which is but a few feet 
 from it. This analysis may represent the composition of the deeply stained rock 
 occurring elsewhere in the mines. 
 
 The jointed structure in this stained rock is always distinct, and it is a very 
 significant fact that wherever found, whether as isolated " boulders" in vein-matter 
 or in large bodies, the dip is always the same. The ore and vein-material found 
 at this horizon will form the subject of the following chapters. 
 
 THE GRAY PORPHYRY. This rock, where exposed to view by the workings, lies 
 entirely in the Blue limestone and in the lower part of that formation. As the sec- 
 tions show, it corresponds in dip very closely to the enclosing rock for a distance of 
 150 to 200 feet from the outcrop, but from a point just above the Lower Waterloo 
 shaft it takes a much steeper dip and cuts down across the limestone stratum to a 
 lower horizon. Probably it again takes the dip of the formation lower down 
 (Emmons). It is not at all improbable that originally this sheet continued to rise 
 across the Blue limestone until it reached the White porphyry, and that the point of 
 juncture is now entirely worn away by erosion. The steeper dip is, on the whole, 
 very regular from the Lower Waterloo shaft as far down as the incline has been 
 run, but there are many minor local irregularities in the pitch which often seem 
 to bear some relation to the deposition of ore. These will be mentioned later on. 
 
 The popular name for this rock is Bird's-eye porphyry, on account of its spotted 
 appearance, due to the separation of feldspar crystals from the ground-mass. It 
 differs very much from the White porphyry, even when both exist in a very de- 
 composed condition side by side. This sheet of rock is so thin, being only from 
 46 to 50 feet in thickness, and has been so subjected to decomposing agencies, that 
 an approximately fresh specimen could nowhere be obtained. Consequently no 
 analysis of the rock was made, as it was thought that one would give no idea of 
 the original composition and nature of the rock. Even at the centre of the sheet, 
 where the firmest specimens of the rock were found, kaolinization, which is the 
 peculiar form of decomposition of this rock, had reached an advanced stage, and 
 all the specimens were softened and crumbled when dry. The feldspar-crystal 
 outlines could be recognized. They occur with great frequency, ordinarily as 
 small grains a sixth to an eighth of an inch in diameter. Very rarely the outlines 
 of much larger crystals an inch or so in length could be recognized. They are 
 always soft and almost completely changed to clay. 
 
 The quartz exists as small, vitreous, transparent, white crystals about as 
 large as the smaller feldspar crystals. They are not numerous, but any small 
 lump weighing an ounce or so would be likely to show a few of these granules 
 shining through it. 
 
 The ground-mass is generally of a dull gray color and harder than the rest. 
 
20 OCCURRENCE OF THE ORES. 
 
 The feldspar crystals appear as granular white dots through it and occupy about 
 one half the surface. Sometimes the ground-mass has a decided pinkish color, 
 which is probably due to the oxidation of the protoxide, which is said to stain the 
 fresh rock greenish. 
 
 It is not an uncommon thing for branches to run from this sheet into the 
 formation above, and even to extend as far up as the White porphyry and to 
 flatten out against that rock. Such a dike occurs in the Evening Star. The 
 main shaft, No. 10, Plate IV, penetrates it, and shows that it comes almost to the 
 White porphyry. This dike is shown in the section. Another dike, not shown 
 in the sections, occurs in the Morning Star. This body rises all the way up to and 
 flattens out against the White porphyry and cuts off the ore-body in that direction. 
 Another such dike occurred in the workings of the Boarding-house shaft. All 
 of these dikes show all the characteristics of the sheet below, and have also de- 
 composed in a like manner. 
 
 Immediately along the lower contact of the Gray porphyry, except where 
 undecomposed limestone comes in direct contact with it, the rock has been com- 
 pletely changed to clay which is soft and perfectly plastic and devoid of all 
 signs of the original texture. Further from the contact the rock, still very soft, 
 begins to show the characteristic mottled appearance, and further in yet, gen- 
 erally two or three feet, it becomes firmer and the jointed structure appears. 
 Though very prominent, the jointing is not carried as far as in the White por- 
 phyry, but only splits the rock into large lumps. 
 
 THE WHITE PORPHYRY. The White porphyry .is a more regular sheet than 
 the Gray, and seems to follow the dip of the Blue limestone with great regularity. 
 The facts concerning its position have already been stated. The Brooklyn 
 mine, lying east of the Maid of Erin (a claim adjoining the Morning Star on the 
 east), finished a shaft through this rock last fall, so that a section through 500 
 feet was exposed on the dump and as fresh specimens as occur were obtainable. 
 The rock is light gray in color and has a fine-grained, even surface on which only 
 very few porphyritic ingredients can be distinguished. The jointed structure is 
 exceedingly prominent and is carried very far, so that the rock, especially if at 
 all decomposed, breaks into small angular blocks. The jointing faces are always 
 smooth and sometimes have an almost perfect polish. They commonly have 
 stains of black oxide of manganese which are often beautifully dendritic and give 
 rise to the popular name of forest-rock. Besides this light homogeneous-looking 
 rock a peculiarly banded variety is found, of a light rusty or reddish-brown color 
 which is due to stains of sesquioxide of iron. A little of this variety occurred in 
 this shaft. In other places on the hill it is very abundant. Except in the banded 
 appearance, which is only due to the coloring matter, it does not seem to differ 
 very much from the rest. 
 
 The macroscopic crystals are scattered very thinly through the fine-grained 
 
THE WHITE PORPHYRY. 21 
 
 base. QUARTZ occurs in irregular crystalline granules, not more and generally 
 less than o.i inch in diameter. They are colorless, semi-transparent and vitreous, 
 just as those of the Gray porphyry, but they occur much less frequently than in 
 the latter rock. MICA is of more frequent occurrence than quartz. Some of it 
 exists as black mica or biotite, and some of it as the white mica or muscovite, the 
 latter being a product of the decomposition of the other constituents. The biotite 
 is in larger pieces than the muscovite, but is less frequent. In some cases it is 
 much decomposed. The muscovite is fresher than the biotite, and frequently 
 shows hexagonal sections very nicely. The FELDSPAR crystals were very seldom 
 recognizable in the ground-mass. Very rarely a small, shining crystal of this 
 mineral could be seen which resembled sanidine. Orthoclase is the essential 
 feldspar of the rock. Many cavities now empty or only partially filled with oxide 
 of iron were observed in this rock, and though none of them contained any of the 
 original mineral which once filled them, it is probable that it was iron pyrites, all 
 of whose sulphur has been completely washed away. 
 
 When a thin slide of this rock was examined under the microscope it was 
 found to be a true felsite or quartz porphyry, though it has been much altered by 
 secondary changes. The feldspar has become, as a rule, opaque from kaolinization. 
 The ground-mass was fine-grained, and a high power had to be used to examine 
 it. The porphyritic ingredients were quartz and monoclinic feldspar, the former 
 predominating. Between or about the larger crystals of quartz the ground-mass 
 was sometimes twisted in currents with a peculiar feathery arrangement of the 
 small crystals which strongly suggested the fluidal texture. In another slide of 
 the banded variety mentioned above the decomposition had proceeded much 
 further, and the characteristic features could not be seen nearly so perfectly. In 
 both sections the ground-mass was feldspathic, but contained much free quartz as 
 tiny angular specks. On comparing the section of the freshest specimen with a 
 number of slides of normal quartz porphyries from Europe it was found to have 
 a precisely similar structure, though the porphyritic ingredients were generally 
 larger and more prominant in the foreign specimens. 
 
 The following is an analysis from as fresh a specimen of White porphyry as 
 could be obtained, yet it Has evidently lost some alkali : 
 
 Silica 74.98 
 
 Iron sesquioxide l 
 
 Alumina 1527 
 
 Manganese dioxide x o _ 
 
 L; me --: ..:.'".' 1.03 
 
 Ma S nesia trace 
 
 Phosphorus pentoxide . , 
 
 Sulphur trioxide , < 
 
 Soda 
 
 1. 80 
 
 Potash 
 
 2.10 
 
 2.00 
 
 99.61 
 
22 OCCURRENCE OF THE ORES. 
 
 It is true that the White porphyry decomposes and gives rise to large bodies 
 of clay, but the whole rock does not soften in this manner as the Gray does. 
 Commonly it decomposes to a dry siliceous mass in which the jointing is per- 
 fectly distinct and which crumbles to small bits along those planes. Such decom- 
 posed rock caves easily and has to be supported with stout timbers. Ground of 
 this kind is most damaging to timbers, not so much because it swells and crushes 
 them, as because it is so loose that it caves and a great weight of rock is let down 
 on them. Where the rock decomposes to a soft clay-like product this caving does 
 not occur to such an extent, and the drifts do not have to be so stoutly timbered. 
 Thus beneath the Gray porphyry in the Lower Waterloo the timbers need not 
 be nearly so strong nor so close together as under the White porphyry. 
 
 THE ORE-DEPOSITS. 
 THE ORE-CURRENTS. 
 
 The position of the ore in the formations is shown in the sections, Plates III 
 and IV, by pen-dotting. It occurs in the horizon of the Blue limestone and 
 immediately under porphyry. In some deposits about Leadville the ore occurs 
 in White limestone and other formations, but by far the larger part of the output 
 of the whole camp comes from the Blue limestone, as in the Morning and Evening 
 Star mines. The contact between the limestone and the porphyry is also the 
 normal position of the ore, especially on Carbonate Hill, but there are important 
 exceptions to this rule in the camp, notably in the deposits of the Silver Wave- 
 Cord group on Iron Hill, in which the ore occurs as lenticular bodies in lime- 
 stone and in no way connected with the porphj-ry. On the Morning Star a large 
 amount of ore has been found beneath the Gray porphyry sheet, as already men- 
 tioned. This body differs in no essential way from that underlying the White 
 porphyry, the ores being similar and the laws governing their occurrence 
 the same. 
 
 Speaking roughly, we may say that the Blue-limestone bed is now occupied 
 by two classes of matter, (i) the original limestone, and (2) vein -matter of 
 various kinds which has supplanted the original rock. Of these the latter class 
 lies immediately under the porphyry. The limestone is below. The lower 
 surface of the porphyry is comparatively even, and there is, as a rule, an abrupt 
 boundary between it and the vein-material. Between the limestone and the vein- 
 matter the boundary is very irregular. Sometimes the vein-matter is so thick 
 that it almost supplants the limestone, and again so thin that the limestone comes 
 
THE ORE-CURRENTS. 23 
 
 very near the porphyry, and even in direct contact with it, pinching out the min- 
 eral matter entirely. Thus, on going to the lowest level of the Evening Star 
 main shaft, No. 10, Plate IV, and following the drift to the point where it 
 emerges from the Gray porphyry, limestone is found, which, however, is deeply 
 stained and discolored, while numerous heavy seams of hydrous oxides of iron and 
 manganese run along the bedding-planes. It is, in fact, so altered that there can 
 be no doubt that vein-matter proper would appear only a short distance above, 
 though the ground just above could not be examined. The south-western work- 
 ings of the upper shaft of the same mine, No. 11, Plate IV, show a quite pure 
 limestone rising up to contact and cutting off the vein-matter altogether. 
 
 Though the vein-matter occurs along the contact, it by no means occupies all 
 or nearly all of it. Also, it does not occur in isolated patches which have no rela- 
 tion to one another. It is found to follow well-defined courses or channels in the 
 limestone and along the contact. These courses are much longer than broad and, 
 though they vary in both width and thickness, are perfectly continuous and unin- 
 terrupted. Such streaks have been excellently named ORE-CURRENTS. 
 
 All the ore is found in these currents. The larger part of the ore of the 
 Morning Star and almost all that of the Evening Star has come from one great 
 current under the White porphyry, the only one yet developed under this rock 
 on these claims. This current begins on the western slope of the hill in the 
 Crescent claim. It starts from the outcrop and passes from here in a north- 
 easterly direction through the Catalpa and into the Evening Star. In the 
 Crescent the thickness of the ore alone is not very great, but it becomes thicker 
 and broader in the Catalpa, and passes into the Evening Star a splendid body 
 which rapidly develops till an enormous thickness is reached, the maximum 
 being 70 to 80 feet. The ore in the current as rapidly decreases in thickness 
 towards the Morning Star, and the current passes on much thinner but broader 
 and still bearing fine bodies of ore. It passes through the south-eastern part of 
 the Morning Star consolidated property into the Maid of Erin and Big Chief 
 claims. The Brooklyn shaft, beyond the Maid of Erin, also strikes ore and, as it 
 lies in the right direction, is almost certainly on the same current. 
 
 Below the Gray porphyry there is another current which, though not nearly 
 so large as the preceding, contains very fine bodies of rich ore. This current, as 
 the plan, Plate II, will show, has two branches which run into the hill and, joining, 
 go on together as one current. One of these branches, the smaller, starts at the 
 south-western corner of the Evening Star from below the outcrop of the porphyry 
 and runs in a north-easterly direction toward the Old Waterloo shaft (No. 6, Plate 
 II). The other, larger branch begins at the outcrop on the old Half-way House 
 claim and runs a little south of east into the Lower Waterloo and Henriette, the 
 boundary between these two mines being about the centre of the current. Con- 
 
24 OCCURRENCE OF THE ORES. 
 
 tinuing in this course it is joined by the smaller branch. This ore-current has 
 lasted as far as developments have been pushed, and there is every reason to sup- 
 pose that it will continue into the hill. It has already been followed from the 
 outcrop to a depth of 400 feet below the surface, and the breast of the main incline 
 is already over 250 feet beyond the point where the outcrop of the White por- 
 phyry ceases. 
 
 The pen-shading on Plate II and the pen-dotting, Plates III and IV, repre- 
 sent approximately the extent and depth of the ore alone in these currents. It 
 would be more difficult to give the boundaries of the entire current, gangue as 
 well as ore, as the gangue is not followed when there is no promise of ore. If the 
 entire amount of vein-material were represented on the plates, the axis of the cur- 
 rent would not be changed. The current would only appear broader and thicker. 
 Of the area represented in shading on Plate II, at least two thirds or three fourths 
 is occupied by pay-ore. No ore occurs outside of these limits. 
 
 Outside of such a current the limestone comes to contact. Under the White 
 porphyry it is not often met with. In the Morning Star it was found in only two 
 places, and there it was altered and impregnated with impurities. The Boarding- 
 house shaft showed a great deal. It was black and contained so much iron that it 
 became strongly magnetic on testing with the blowpipe. The other point was in 
 the face of drift 59 of the Upper Waterloo, where the same characteristics pre- 
 vailed except that manganese was relatively more abundant. These two points 
 indicate the boundary of the upper current on the north-east. The limestone of 
 the upper Evening Star shaft (No. u), which has already been mentioned, is on 
 the southern side of the current. 
 
 Below the Gray porphyry the waste vein-matter does not extend far beyond 
 the point where the ore ceases, and the boundary of the current is better denned. 
 All along the southern side of the smaller branch the drifts have exposed quite 
 pure limestone coming up to contact, once not more than 25 feet from where the 
 ore ceased. Limestone is likewise found in the barren ground just above the 
 junction of the two branches. The northern side of the main current has never 
 been determined. It extends beyond the Henri'ette and perhaps outcrops along 
 Stray Horse Gulch. 
 
 These are the only currents that have been developed on the property ; and 
 now the very important question arises, Do any others exist, and if so, where ? 
 It is simply impossible to say whether there are or are not other currents, and the 
 only way of finding out is by sinking shafts or running expensive drifts through 
 barren rock to the unexplored parts of the mines. As to where they will be found, 
 if they do exist, of course the answer is easier. It is almost certain that no other 
 body of ore underlies the White porphyry in the Evening Star, for the unexplored 
 area in that mine is very small. In the Morning Star there is a large area north- 
 
THE VEIN-MATERIAL. 25 
 
 west of the main current which, like the ground beyond it on the Henriette, is as 
 yet undeveloped. This area will be easily explored from the new McHarg shaft 
 which is being sunk to the current under the Gray porphyry. The probabilities 
 seem to be against there being another current in this ground ; for if there is, some 
 of the old prospecting-shafts lower on the hill should have struck it. The drifts 
 that will be run from the new shaft, which is already sunk 150 feet below the con- 
 tact (May, 1883), will solve this question. 
 
 The greatest unexplored area is on the second contact; that is, under the 
 Gray porphyry. It is the entire area south-east of the current laid open under 
 that body. This ground will soon be explored, for both the middle and upper 
 shaft of the Evening Star (Nos. 10 and n) are being sunk to explore it. If an ore-, 
 current does exist there, drifts run from these shafts will find it. In the mean 
 time the results of exploration have to be awaited. 
 
 THE VEIN-MATERIAL. 
 
 The vein-material as it now exists consists of carbonate, sulphide and sul- 
 phate of lead, sulphate of iron, oxides of iron and manganese, and silica. The 
 latter is sometimes in a very pure state as spongy deposits from solution or as 
 chert, but more often is mixed with greatly varying proportions of oxide of iron. 
 There is abundant evidence to show that the vein-materials originally existed as 
 sulphides and oxides (or carbonates), but owing to the decomposition of the former 
 by the meteoric agencies to which they have for ages been subjected the other, 
 secondary products have arisen. In the original deposits the minerals form- 
 ing them occurred pure in considerable quantity, but the larger part of the vein- 
 material consisted of mixtures of certain of them in almost every proportion. 
 Consequently, after the further changes due to the action of meteoric waters, the 
 variety of the materials going to make up the vein-matter is very great. The 
 number of pure minerals, however, which occur in the deposits is very small. 
 The following were noted : 
 
 CERUSSITE, lead carbonate, PbCO,. 
 
 GALENITE, lead sulphide, PbS. 
 
 ANGLESITE, lead sulphate, PbSO,; Pyromorphite, lead phosphate and 
 chloride, 3Pb,P,O.+PbCl,. 
 
 CERARGYRITE, horn-silver, containing chloride, bromide and iodide of 
 silver. 
 
 CALCITE, calc-spar ; BARITE, heavy spar, barium sulphate, BaSO, ; Calamine, 
 silicate of zinc ; Native silver ; Pyrite ; Rhodochrosite, carbonate of manganese ; 
 
26 OCCURRENCE OF THE ORES. 
 
 Psilomelane, hydrous manganese dioxide ; Dechenite, vanadate of lead and zinc, 
 (Pb.Zn) V,O, ; BASIC SULPHATE OF IRON. 
 
 Of these minerals the ones in small capitals only are of common occurrence. 
 Besides the well-defined minerals there are many mixtures of manganese and iron 
 oxides; iron oxide and silica; silica, iron oxide and carbonate of lead, etc., which 
 exist in very large quantity and form the major part of all vein-material. 
 
 The vein-matter may be most conveniently if not naturally divided into ore 
 and gangue. Concerning the position of these, it may be said that the ores occupy 
 almost identically the same relation to the gangue that the whole of the vein- 
 matter does to the limestone. The ore lies immediately under the porphyry, and 
 the gangue below it. The ore does not occupy the whole surface of the current, 
 though it forms a continuous sheet. It is almost always found in strength along 
 the centre, but the gangue always rises to contact along the sides. The thickness 
 also varies greatly. The rule that where the ore is very thick the gangue below 
 is likewise so, and vice versa, does not hold at all, although there is always a large 
 amount of gangue beneath the ore. 
 
 THE GANGUE. 
 
 IRON-ORES. These consist for the most part of hydrous oxides of iron and 
 manganese. The lower half or three quarters of the current is largely composed 
 of these materials. Further up towards the top large quantities of siliceous 
 material occur, especially in the upper current. These mixtures of oxides of iron 
 and manganese are both compact and loose. The loose is found most frequently 
 near the top of the zone of gangue rather than at the centre. It also occurs near 
 the bottom, and frequently forms seams in the limestone and about boulders of 
 that rock. It is a soft wad-like material, but does not powder. It can be easily 
 dug down with a pick and falls in flakes. It contains some sulphuric acid which 
 has most probably been derived from the oxidizing galena. In color it is from 
 dark brown to black, and is slightly mottled. 
 
 The rest of the lower part of the current is occupied by the firmer variety 
 which forms the greater part of the vein-material. It is of a deep blackish-brown 
 color, solid and hard. It has a well-marked jointed structure, and in many ways 
 has, when in large masses, the outward appearance of the stained limestone. In 
 both currents the iron is in such a high state of oxidation that the surveyor uses 
 his compass freely in the mines. All the manganese exists as the dioxide. 
 
 The following analysis represents the average composition of this material. 
 The specimen was taken from the Lower Waterloo. 
 
THE SILICEOUS GANGUE. 27 
 
 Silica 10. 73 
 
 Iron sesquioxide 46.22 
 
 Alumina 0.06 
 
 Manganese dioxide 31.18 
 
 Lime 1.20 
 
 Magnesia 0.68 
 
 Water 9.98 
 
 Phosphorus pentoxide 0.05 
 
 Sulphur trioxide 0.03 
 
 Carbonic acid o. 54 
 
 100.67 
 
 THE SILICEOUS GANGUE. This exists in large bodies and in great variety. 
 It occurs, as a rule, near the ores and both above and below them. Low down in 
 the current it is rare. When above the ore and along the contact it is very pure. 
 It is then often a spongy, white, amorphous material, with hard, cherty cores, and 
 has evidently been deposited from solution. In the Lower Waterloo and Forsaken 
 there is a large sheet of compact rock, now very much disintegrated, but showing 
 a jointed structure and many external features of quartzite. This sheet overlies 
 all the ore of the branch current. It will be mentioned later. 
 
 The siliceous gangue proper belongs below the ore, and occurs in large 
 though ill-defined and by no means regular or continuous bodies. It is much 
 more common under the White porphyry than under the Gray. It is never pure, 
 but has always a high percentage of sesquioxide of iron. In its purest form it 
 exists in local concretionary deposits of a red jasper imbedded in more impure 
 material. It is then much harder and more compact than the rest and has few 
 joints running through it. As long as the percentage of silica is very high the 
 rock is extremely hard, but as the siliceous character becomes less prominent and 
 oxides of iron and carbonate of lead appear in quantity it assumes a regular 
 jointed structure, so that a blow of a hammer will shatter the brittle rock into 
 small angular blocks. The most common variety of this gangue has from 30 to 
 50 per cent of silica, and the rest is made up of sesquioxide of iron, carbonate of 
 lead and a little water. An analysis of this kind of material is given below. The 
 specimen is very rich in silver, but that metal came almost entirely from coatings 
 of cerargyrite deposited from solution along the joints already alluded to. 
 
 Silica 39- 50 
 
 Silver chloride 1.44 
 
 Lead oxide '5-46 
 
 Iron sesquioxide 35-6? 
 
 Lime 0.50 
 
 Carbonic acid 3.44 
 
 Water 3-46 
 
 99-47 
 
28 OCCURRENCE OF THE ORES. 
 
 The percentage of lead carbonate in the analysis given above is seen to be 
 quite large. A full series of this kind of rock running from a quite low percentage 
 in lead, like the one above, to a quite high percentage of that metal occurs in the 
 Morning Star. Very little of it comes under the Gray porphyry, though it is 
 even then occasionally met with. In both the Evening and Morning Star it is 
 abundant under the White porphyry. Where the percentage of lead is low the 
 rock is generally not perfectly homogeneous, but some parts of it contain more 
 lead than others. 
 
 CLAYS. The small quantity of alumina in the vein-material is noticeable. It 
 exists almost exclusively in clays which may be traced to porphyry as a source. 
 All the largest sheets and here they reach considerable proportions lie directly 
 along it, and the very small quantity existing below is in most cases plainly due to 
 infiltration. Along the upper contact clays are, comparatively speaking, scarce- 
 For the most part the White porphyry at contact does not kaolinize, but assumes 
 a hard, dry, siliceous form which in a yet more advanced stage of decomposition 
 easily crumbles to a dry, sandy powder and shows no clay at all. In the upper 
 shaft of the Evening Star and in the Boarding-house shaft there were considerable 
 bodies of clay along the contact. These sheets were highly impure and contained 
 many streaks of manganese oxide and some carbonates of lime and manganese. 
 
 Clay is common along the lower contact. The Gray porphyry is soft and tends 
 to change to clay, and generally several inches, at least, of very pure clay lies above 
 the vein-matter proper. Often it is peculiarly striped and stained by iron and 
 manganese. It is very pure and much of it is of surprising whiteness. It seldom 
 contains appreciable quantities of sulphur. That all these clays have arisen from 
 the decomposition of the porphyry in place there can be no doubt, for there is 
 always a gradual change from the pure structureless clay without to undoubted 
 porphyry within. The thickness of these clay sheets varies from a few inches to 
 two or three feet. 
 
 The remarkable clay called by the miner " Chinese talc" has a different mode 
 of origin. This material conies in the mines both along the contact and below it. 
 The black iron of the Lower Waterloo shows many pockets of it which are 
 entirely isolated and from five to ten feet from the contact. Some of it is stained 
 by manganese and iron, but most of it is pure white. It has a conchoidal fracture 
 and an opalescent or pearly lustre, and is semitransparent on thin edges. On 
 exposure to the air it slowly becomes opaque, especially if impure. Some speci- 
 mens from the Carbonate mine which were soft became opaque on a very short 
 exposure. Two specimens from the Lower Waterloo were analyzed. No. i was 
 the softer. It was stained light green when taken out of the mine. On six 
 months' exposure it became opaque on the surface and had turned to a pinkish 
 color. Within it was still fresh and green. It contained only a faint trace of 
 
THE ORES. 29 
 
 manganese. No. 2 was much harder and more brittle, and remained translucent 
 on thin edges even after half a year's exposure. The following are the analyses: 
 
 (i) W 
 
 Silica 42.94 40. 53 
 
 Alumina 37. n 38.51 
 
 Water 19.48 19.43 
 
 Sulphur trioxide 0.65 0.33 
 
 Lime.. 0.66 1.50 
 
 100.84 100.30 
 
 These analyses show that the composition is variable, though No. I gives the 
 formula Al,Si,O,3H,O very nicely. 
 
 A few minerals which occur in the deposits, most often in the gangue, may be 
 briefly mentioned here. 
 
 CALCITE. This is of course common ; generally it occurs as the ordinary 
 incrustation filling crevices in the waste or lining cavities in the iron. In the 
 large cavities in the gangue beautiful crystallizations are often found. Large and 
 very handsome rhombohedrons on cerussite occur in the Evening Star. Much of 
 it occurred in a cave found in the workings of the Boarding-house shaft. 
 
 BARITE. Heavy spar in small quantities is also very common. Generally it 
 is found scattered through ore as small crystalline aggregates of a pure variety. 
 A more impure kind, of pinkish color, is found in larger masses. 
 
 CALAMINE. This mineral is far more rare than either of the above. It is 
 almost always found in waste, most frequently in the Lower Waterloo, forming 
 the filling of crevices and druses. It occurs in aggregates of fine, slender, needle- 
 like prisms. 
 
 DECHENITE. Dechenite has been found in very small quantity in the Evening 
 Star. It occurs as an incrustation on a siliceous gangue. When thick these 
 coatings are of a deep brick-red color. Surfaces six inches across have been found 
 completely covered with it. It yields no reaction whatever for chlorine, and gives 
 fine reactions for vanadium, lead and zinc before the blowpipe. 
 
 THE ORES. 
 
 There can be no doubt that the lead was all originally deposited in the lime- 
 stone horizon as the sulphide, and that the silver was either deposited along with 
 it as the sulphide, as in ordinary argentiferous galena, or perhaps also with this, 
 but separated out as argentite. Besides these there seems to have been deposited 
 in some places a great deal of iron pyrites, either mixed with varying propor- 
 tions of galena or nearly free from it. The oxidation of these sulphides has pro- 
 ceeded so far that, comparatively speaking, very little galena is now left, and 
 
30 OCCURRENCE OF THE ORES. 
 
 there is not a trace of iron pyrites. The products arising from this decomposi- 
 tion are for the most part carbonate of lead, chlor-bromide of silver (containing 
 also some iodide), sulphate of lead and sulphate of iron. The original sulphides 
 formed a belt along the contact. In most places the change to the oxidized prod- 
 ucts was a gradual one in place. Small amounts of all the metals were carried 
 off in solution by the oxidizing waters. They were to a large extent redeposited 
 in the gangue, and in some cases sufficiently concentrated to form ore out of what 
 would have otherwise been too poor to pay for extraction. 
 
 The galenas occupied the upper portion of the belt of sulphides, and the 
 pyrites, where it occurred in any quantity, formed a belt below. The galena has 
 changed to carbonate of lead, and the pyrites to hydrous basic sulphate of iron. 
 Any galena that was mixed with the pyrites has likewise changed to the sulphate. 
 
 The three sections given (Plate I) illustrate the position of the ore in the de- 
 posits and represent the different zones of ore and gangue. 
 
 Section i is through a portion of the ore-body of the Upper Waterloo. The 
 galena has entirely changed to the carbonate, and the pyrites to the sulphate of 
 iron. The former is represented by the gray-blue band immediately under the 
 White porphyry, and the latter by the yellow band below the blue. The latter 
 zone was not rich enough to pass as ore, and its lower boundary could not be 
 accurately determined, as it was seldom exposed. It is, however, very nearly the 
 same as that given in the section. All the other lines on the plate are from actual 
 measurements. The boundary between the carbonate and sulphate is abrupt and 
 well denned, as is that between the latter and the iron-ore lying below it. 
 
 Section 2 is through a part of the small branch current of the Lower Water- 
 loo. The same description holds here as in the former case. The blue belt is 
 very highly oxidized lead-ore, rich in lead but containing some silica, and by no 
 means as pure as the preceding. The yellow zone, which in this case is fine ore, 
 occupies the same position as in the other section. In this section the current is 
 not very deep, and the stained, impure limestone, is indicated in the lower part by 
 the conventional lining. 
 
 Section 3 is also from the Lower Waterloo, but is from the main ore-current 
 below the junction with the branch. This body of ore never had a zone of 
 pyrites below it, and hence there is no yellow sulphate. The cerussite, which is 
 highly ferruginous, still contains many nodules of galena. The iron immediately 
 below is somewhat soft and contains much manganese dioxide and some sul- 
 phuric acid. It soon changes into the firmer variety. 
 
 No section of the great ore-body of the Evening Star is given, as it was for 
 the most part stoped away, and there was no way of getting an accurate section 
 representing how and as what the ore occurred. 
 
 THE GALENA. There is not much of the galena left in the ore-bodies, though 
 
THE GALENA. 31 
 
 in one or two places it is abundant. It occurs nowhere as continuous and solid 
 bodies. It everywhere shows signs of an advanced state of decomposition into 
 oxidized products, and is divided into nodules by seams or streaks of these. It 
 rarely occurs under the White porphyry, and then in small nodules imbedded in 
 the carbonate of lead, and seldom over a few inches in diameter. It is most abun- 
 dant in certain parts of the Lower Waterloo. No galena is found in the small 
 branch current (Plate II), as oxidation has there been very complete, but in 
 the larger branch and the main current, especially in the former, it is quite 
 abundant. 
 
 The ore of the Half-way House mine, below the Lower Waterloo, consisted 
 mostly of this mineral, and was very rich, although the bodies were not large. 
 About the first level of the Lower Waterloo shaft (No. 6, Plate II), galena occurs 
 as nodules and broken streaks surrounded by carbonate of lead. Below this 
 point, for 50 to too feet, it is more abundant than at any other place in either 
 mine. Here in some places it is in streaks, alternating with seams of carbonate, 
 and together with this forming a very rich pay-streak two or three feet in thick- 
 ness. The galena streaks are bright at the centre but lustreless on the outside. 
 They are not solid, but in several main streaks and numerous branches which 
 form a network. The decomposition products are deeply iron-stained to a rusty 
 color. The galena in decomposing first loses its metallic color and forms a dark 
 band of greasy lustre, half an inch in breadth ; then, while the streak is still hard, 
 the brown color appears. At the centre of the broadest of the streaks of car- 
 bonate it is softer and granular. The galena in this body was on the whole 
 coarse-grained, but almost every texture could be seen even in different parts of 
 one and the same seam of undecomposed mineral. 
 
 About at the same level as this, but over on the Henriette line, galena is 
 found in great abundance and with very little carbonate of lead. Here it is along 
 the contact, but it does not form a solid streak. It occurs as a series of streaks 
 of the greatest irregularity running through and lying in black iron. In some 
 cases it lies directly along the porphyry, and in some it is entirely surrounded by 
 iron. The streaks are always near the porphyry, however, and the zone in which 
 they occur never extends more than, six or eight feet from it. These streaks are 
 small as well as extremely irregular, but rich in both silver and lead. The iron- 
 ore about it contains no lead and far too little silver to pay. Assays of this iron 
 gave 6 to 20 ounces of silver. The decomposition of the galena was slight, but 
 narrow streaks of cerussite ran through the seams and divided it up into nodules 
 which were both bright and large, many of them weighing 50 or ico pounds. 
 The iron in which they occurred was somewhat soft. It contained much manga 
 nese dioxide and some sulphuric acid. 
 
 Below the junction of the two currents galena is more rare. It is only found 
 
32 OCCURRENCE OF THE ORES. 
 
 as nodules, and these are mostly small and imbedded in large bodies of carbonate 
 of lead. On breaking them open the centres are always bright. Around this 
 core there is a zone of the lustreless sulphide, and then this changes into carbonate 
 so gradually that a division line cannot be recognized between the two. The 
 transition of the galena into cerussite is always plainly shown. 
 
 In the above examples there is every step from nearly solid galena in which 
 the change is just beginning, to the almost completely oxidized bodies in which 
 there is scarcely any galena left. In the branch current of this contact, and also 
 in the Upper Waterloo, we have bodies in which the changes have long been 
 completed. The change is an altogether gradual one from without inward, and 
 there can be little doubt as to the manner in which it is effected. The oxygen 
 dissolved in the waters penetrates the ore and oxidizes the galena to sulphate of 
 lead. The calcium carbonate, held in solution in the water by an excess of car- 
 bonic acid, acts upon the sulphate of lead, forming carbonate of lead and sulphate 
 of calcium. The latter passes off in solution. Alkali carbonates would act on the 
 sulphate of lead in the same manner. 
 
 There are often cavities in the galena, and these are generally lined with 
 large transparent crystals of cerussite. They are then in long prisms capped by 
 the pyramid. 
 
 Galena has been found on several occasions within the Gray porphyry. 
 Sometimes it forms the filling of irregular gashes which run up into the rock from 
 the contact, but which are always very small. On two occasions it was found 
 forming seamlets in it four or five feet above the contact, and running parallel to 
 it. In one case the seam was over a foot thick and mostly carbonate of lead, with 
 galena in large nodules. In the other the seams were only six inches thick, but 
 were nearly solid galena. 
 
 The galena is generally very rich in silver. Under the White porphyry 
 samples were too rare to afford trustworthy estimates of the general run of the 
 original galena of the upper current, but under the Gray porphyry there was an 
 abundance. To give a good idea of the richness of these galenas fifteen speci- 
 mens from various parts of the Lower Waterloo were assayed. The average 
 silver contents was 180.2 ounces per ton of 2000 pounds. The different samples 
 varied greatly in value, the minimum being but 36 ounces and the maximum 490. 
 Four of the fifteen ran less than 75 ounces, and three of them over 300. A small 
 nodule found later gave by assay 1142 ounces, but this was far above any other 
 sample of galena found in either mine. The percentage of silver seems to be in no 
 way connected with the texture of the galena or its crystalline structure. Almost 
 all the galena, coarse or fine, is rich, but both coarse and fine do occur which 
 are, comparatively speaking, very poor in silver. The galena in the Lower 
 Waterloo is not as a rule very pure. Only two of the fifteen assays mentioned 
 
THE PURE CARBONATE OF LEAD 33 
 
 above gave over 75 per cent of lead. Nine of them gave over 70 per cent. The 
 average of the fifteen was about 69 per cent. In the Upper Waterloo the galena is 
 very pure and, as far as could be judged, less rich in silver. The impurities are 
 commonly iron oxide and silica, chiefly the latter. The iron is generally invisible. 
 Only one piece showed tiny specks of pyrites, the only traces of this mineral 
 found among the ores in either mine. 
 
 THE PURE CARBONATE OF LEAD. This is and has always been the chief ore 
 of both mines and under both sheets of porphyry. The purest, largest and best- 
 defined bodies of carbonate of lead occur under the White porphyry. In the 
 Evening Star they had been removed before the fall of 1882, but in the Morning 
 Star they were well developed but not stoped out. In the upper levels of the 
 Forsaken and Lower Waterloo there is another body of large extent, though 
 neither so thick nor so pure, but very completely oxidized. The ores of the lower 
 levels and elsewhere are still less pure, and contain the galenas already mentioned 
 as well as iron oxide and other gangue. The purest carbonate of lead bodies con- 
 tain little else than pure, granular cerussite crystals, often so loosely put together 
 that thev easily crumble between the fingers, especially when damp. Some of it 
 is more firmly cemented and, especially when dry, quite firm and hard. The 
 grains out of which the purest bodies are formed are about the size of coarse sand 
 and resemble it superficially. They consist of very imperfect crystalline gran- 
 ules, among which, by the aid of a strong magnifier, a more or less perfect prism 
 may occasionally be recognized. They are of course very brittle, and, whatever 
 the color of the body be, the powder is white. It is for this reason that a pick 
 always leaves a white mark in this ore. 
 
 In the color of the pure cerussite ore there is great variety. Rarely it is an 
 almost pure white. Brown, grayish brown and gray are the most frequent 
 colors, but grayish blue is also common. Sometimes it is a light cream-color, 
 sometimes almost black. The coloring-matter is mostly oxide of iron, more 
 rarely oxide of manganese, and only forms a small percentage in the composition 
 of the ore. The color bears no relation to the silver contents, and rarely to the 
 percentage of lead. The bodies of the Upper Waterloo frequently show a pecu- 
 liar banded structure, very faint and delicate, and entirely in the coloring-matter. 
 These bands can be plainly seen by candle-light, but can hardly be recognized on 
 the surface. They consist of bands of slightly different color, and, though gently 
 wavy, always run strictly parallel to the dip of the body. Almost all the purest 
 cerussite ore shows this banding. 
 
 The percentage of lead in these ores is almost that of normal cerussite. Two 
 analyses were made, one from the ore of the Upper and one from that of the 
 Lower Waterloo. The first was grayish white in color, the second bluish gray. 
 
34 OCCURRENCE OF THE ORES. 
 
 (i) (2) 
 
 Gangue 0.42 4.43 
 
 Leadoxide 83.27 77.70 
 
 Silver chloride '. 0.03 0.12 
 
 Lime 0.80 
 
 Carbonic acid 16.30 14.56 
 
 Sulphur trioxide 0.32 0.28 
 
 Phosphorus pentoxide 1 . 22 
 
 Chlorine trace 
 
 Moisture 0.50 
 
 100.34 99.61 
 
 These two analyses represent the purest ore found under the White and 
 Gray porphyries respectively. The first is almost pure cerussite. The second 
 shows, besides gangue, a considerable percentage of pyromorphite (nearly 8 per 
 cent). 
 
 These pure carbonates are very fine ores on account of the high percentage 
 of lead ; for, since they are very desirable to the smelter, a high price per pound is 
 paid for the lead in them, and a low charge deducted for treatment. They are, 
 however, poor in silver. Wherever the ore is purest and oxidation has been most 
 complete the amount of silver is found to be the least. In the Upper Waterloo 
 the pure cerussite ore with only a few per cent of gangue normally runs not more 
 than 20 ounces in silver, and on an average even less. A good idea may be 
 gained of the amount of silver in these high-grade lead-ores by referring to the 
 ore sales. From 19 shipments (or between 900 and icoo tons) of ore running over 
 50 per cent of lead by assay, the average was but 15.03 ounces per ton, or 0.0516 
 per cent, of silver. When this ore is rich it occurs in pockets in the poor bodies, 
 and the silver is always visible as grains and scales of the chlor-bromide. 
 
 THE IMPURE CARBONATE OF LEAD. The pure heavy carbonate of lead ore 
 just described forms a large part of the ore of both contacts. The more impure 
 ores of carbonate of lead are likewise abundant. These may consist of a mixture 
 of pure carbonate of lead with a visible gangue, yet too finely mixed to admit of 
 their being sloped separately. As examples of this class we have streaks of cerus- 
 site alternating with narrow streaks of iron oxide or sulphate, or some siliceous 
 gangue, or seams of it running up into and mixing with the porphyry. But 
 besides these, which differ in no way from the large bodies, there are the HARD 
 CARBONATES of the miner. This name has a rather broad significance, and may 
 be used to indicate any sort of hard rock that carries silica and iron sesquioxide, 
 with enough carbonate of lead and silver to make it pay as ore. 
 
 In describing the siliceous gangue it was shown that lead occurs in that 
 material. Whenever the percentage of lead is high, 20 to 30 per cent, we have a 
 hard carbonate. A perfect series of such material is found, from the hard jasper- 
 like rock with little or no lead, on the one hand, to the pure lead carbonates, on 
 
THE IMPURE CARBONATE OF LEAD. 35 
 
 the other. As the name implies, these ores are hard. The ones containing much 
 iron and silica are very hard and scratch glass easily. As the percentage of lead 
 increases they become softer, but are always hard as long as they contain any 
 appreciable amount of silica. Excepting the poorest of them they are perfectly 
 homogeneous in texture and uniform in color. The color varies through almost 
 every shade of brown, red and gray. 
 
 Hard carbonates do not occur in extensive sheets along the contact like other 
 ores, but rather as thick, massive bodies of small area which underlie pure car- 
 bonate and extend down into waste. When the percentage of lead is quite high, 
 say 40 per cent or more, there are frequently streaks or veinlets of pure, soft 
 cerussite running through it. The richest variety of this class of ore that is, the 
 richest in lead is of a light gray color and contains little iron. It is extremely 
 solid and heavy and will contain from 80 to 90 per cent of carbonate of lead, the 
 remainder being mainly silica. Another very pure variety has very little silica 
 but much iron. This variety is deep red in color and not nearly as hard as the 
 more siliceous. The composition of such an ore is given below in analysis No. i. 
 For the other analysis I am indebted to Dr. LeRoy W. McCay of the Scientific 
 School, Princeton. It shows the composition of a fair average specimen of hard 
 carbonate in all but the silver. The latter metal is present far in excess of the 
 
 average. 
 
 (i) (a) 
 
 Silica 2.82 18.84 
 
 Silver chloride 0.16 1.30 
 
 Lead oxide 66.98 54.89 
 
 Iron sesquioxide I 4- 2 3 11.38 
 
 Lime trace i. 78 
 
 Carbonic acid i3-7 10.83 
 
 Sulphur trioxide -55 
 
 Water.. 1.52 1.61 
 
 99.33 100.65 
 
 No. 2 is deep brownish-red in color and very hard. It has a perfect jointed 
 structure which divides the rock into small rectangular blocks. Though this 
 jointed structure is very common, it is seldom as perfect as this. It is on these 
 joints that the cerargyrite which makes the ore so rich occurs. 
 
 Several thousand tons of such ores have been taken out by the present man 
 agement, much of which was stored in old cribs and drifts, and the rest in place 
 through the old works of the former company. In some cases almost the entire 
 filling of an old drift would be shipped as ore, after passing through the hands of 
 the ore-sorters, and would realize as much as $20 to $30 a ton above all expenses. 
 
 The average amount of silver in these ores is much larger in proportion to 
 the amount of lead present than it is in the pure cerussites. It is seldom that a 
 hard carbonate assaying 30 or 40 per cent of lead carries less than as many ounces 
 
36 OCCURRENCE OF THE ORES. 
 
 of silver. A large amount of the silver ore has often been deposited along the 
 crevices in.it by percolating waters. Such is generally visible in scales. 
 
 The question now arises as to the source of the carbonate of lead in these 
 siliceous ores. That the water dissolves some lead and redeposits it below admits 
 of no doubt, for the incrustations of cerussite along joints and cleavage planes are 
 very common. But it cannot be supposed that this solution and redeposition has 
 been so extensive as to account for much more than a trace of the lead in the 
 hard carbonates. The only way they can have arisen is by the oxidation of 
 impure galenas. A perfect and complete series of these ores, from impure ones 
 not assaying over 20 per cent to the purest gray varieties running 60 to 65 per 
 cent lead, was collected, all of which contain bright particles of galena undergo- 
 ing decomposition. In all of these the various stages between the undecomposed 
 galena and the thoroughly oxidized carbonate may be seen. It cannot be doubted 
 that these hard carbonates have arisen from impure masses of galena just as the 
 more pure carbonates of lead have arisen from bodies of more pure galena. 
 
 THE BASIC IRON SULPHATE. The most peculiar material in the mines is the 
 hydrous basic ferric sulphate which so frequently underlies the lead-ore in both 
 the upper and lower workings. Though this substance is only sometimes very 
 fine ore, it is grouped with the ores because it is often rich and always contains 
 some lead and silver. It forms sheets which, with remarkable persistence, extend 
 beneath the cerussite ores in certain parts of the mines. Its position is shown in 
 sections i and 2, Plate I, and is represented by the yellow color. In color it is a 
 pure light-yellow ochre and has a great resemblance to yellow clay. It is never 
 plastic except when wet. Usually it is dry and firm and has a perfect jointed 
 structure, due probably to pressure. It consists of iron sesquioxide combined 
 with sulphuric acid, has much water and varying amounts of sulphate of lead. 
 When subjected to intense heat it loses all its water and most of its sulphuric 
 acid combined with the iron. The following is an analysis of a specimen of this 
 material : 
 
 Lead sulphate ; 29. 18 
 
 Silica trace 
 
 Iron sesquioxide 40. 22 
 
 Alumina HI 
 
 Sulphur trioxide 18.02 
 
 Water II.2O 
 
 Silver chloride 0.27 
 
 100.00 
 
 This sample contains more lead sulphate than the average. The percentage 
 of lead being low, the value of this material depends largely on the amount of 
 silver it contains. In the Upper Waterloo large bodies of it occur under the pure 
 lead ore which contain on an average only a few ounces, and are therefore too 
 
THE CHLORIDE OF SILVER. 37 
 
 poor to mine. In the upper contact this substance is rarely rich, except when it 
 contains chloride of silver in visible form. In the Lower Waterloo and Forsaken 
 it is abundant in certain places, chiefly under the cerussite ore of the branch cur- 
 rent. Here it always runs well in silver (from 20 to 100 ounces), and makes an 
 excellent ore. The silver is never visible in this body. It has most probably 
 arisen from the galena, which has given rise to the sulphate. 
 
 The fact that this material, wherever it occurs, is always perfectly pure, well- 
 defined and abruptly bounded by the other vein-material indicates without a 
 doubt that it has all arisen in the same way, and differently from any of the rest 
 of the vein-material about it. Although the soft black iron which often lies below 
 both this and the other ores contains some sulphuric acid, this is not often in 
 large quantity and some of the iron contains none. Moreover, the iron contains 
 no lead and, even when under very rich ore, not enough silver to pay. 
 
 The manner in which it is believed to have been formed has already been 
 stated ; namely, by the oxidation of a belt of pyrites mixed with more or less galena 
 (seldom over 15 or 20 per cent) which formerly occupied this position and formed 
 a layer with the more pure galena above it. This easily oxidized mineral, sub- 
 jected for a great length of time to agencies which have almost completely 
 oxidized the last traces of galena in the ore above it, has completely succumbed 
 and been brought to its highest state of oxidation. Not a trace of pyrites has 
 ever been seen in it. Small nodules of galena of great richness in silver have 
 occasionally been found in it. These nodules assay from 60 to 70 per cent in 
 lead and average as high as 450 to 500 oz. in silver. They are seldom entirely 
 bright at the centre, but even there have begun to decompose along the cleavage 
 planes. 
 
 THE CHLORIDE OF SILVER. The great difference in silver contents between 
 the carbonate of lead and the galena is very striking. The amount of silver in a 
 thoroughly oxidized carbonate of lead is never normally above 40 or 50 ounces. 
 Even when no richer than this the silver may often be seen as tiny grains and 
 scales of chloride scattered among the granules. The average richness of the 
 carbonate of lead has already been shown to be much less than this. 
 
 The galena, on the other hand, is (as has already been stated) much richer 
 and averages at least the half of one per cent silver. From ten samples of ore 
 assayed, five of bright large galena nodules and five of the .thoroughly oxidized 
 carbonate of lead around them, it was found that in proportion to the lead present 
 in each there was over six times as much silver in the galenas as in the cerussites. 
 
 It is easy to explain where the silver missing from the carbonates has gone. 
 All the iron about the ore-bodies contains silver. All the porphyry along the 
 contact contains it. And it is not merely the material about the ore. The lime- 
 stone and the vein-matter deep down in the current often contain traces of silver. 
 
38 OCCURRENCE OF THE ORES. 
 
 Assays of these materials yield from one to four ounces. Scarcely any vein-mat- 
 ter can be obtained that does not run one or two ounces, and much of it runs 
 higher. In some places the amount of silver deposited is much more considerable 
 and then ores arise, it may be out of what before was far too poor to be such. In 
 these ores the silver-bearing mineral can always be recognized. In both mines it 
 is invariably the same in color, light greenish yellow. It is soft and sectile, and 
 feels like lead between the teeth. Exposed to the light it does not change color 
 in the least. Qualitative tests show it to contain chlorine, bromine and iodine, all 
 in considerable quantity. It occurs as scales or plates and as single crystalline 
 grains, or aggregates of such grains, and as rough crystalline coatings on the 
 walls of crevices and joints in the various vein-materials ; also as scales and grains 
 more or less thickly scattered through granular carbonate of lead, and as highly 
 crystalline lumps forming the lining of druses and hollows in that mineral, just as 
 cerussite crystallizes in the hollow gafena nodules. Though generally highly 
 crystalline, the grains are small and have to be examined with a magnifying-glass. 
 
 The most common ore formed by the deposition of cerargyrite is low-grade 
 and siliceous. It is the hard, siliceous gangue, with numerous joints and crevices 
 which, interlacing and extending all through the rock, allow the mine-waters to 
 trickle through them or stand in them. The chloride is deposited along these 
 joints. As long as this is visible it is sloped down and sent to the surface, where 
 it is carefully sorted. Of course this is not done when the base itself is pay-ore. 
 Chloride seldom enriches the iron sufficiently to make it pay. When the yellow 
 sulphate of iron is firm and has crevices running through it, it also frequently 
 shows chloride of silver. The pure carbonates of lead frequently have it, and it 
 has occasionally been found in lumps of decomposing galena. 
 
 The most remarkable deposit of ore arising from the deposition of cerargy- 
 rite occurs in the White porphyry on the Evening Star. This body was struck 
 by the main shaft between 20 and 30 feet above the contact. The gangue is noth- 
 ing but porphyry. This is in a state of extreme decomposition here, and there is a 
 deep stain of iron oxide along all the joints which divide the rock into lumps of 
 but a few inches in diameter. The silver is mostly invisible, but shows here and 
 there through the stained portion as tiny specks of chloride. The amount of lead 
 present is very low and it is often altogether wanting. This body is very irregular, 
 but in many places it is 8 or 10 feet thick and three or four times as broad. The 
 ore could only be distinguished from the waste by assay. Just below this point a 
 large dike of Gray porphyry has broken up and reaches almost to the White. 
 It seems not improbable that the disturbances accompanying this eruption may 
 have shattered the White porphyry and allowed the solutions bearing the metals 
 a limited access to this rock. 
 
 Rich pockets of ore always owe their richness to the chloride of silver that 
 
THE UPPER CURRENT. 39 
 
 has been concentrated there. They generally occur in the pure carbonate of 
 lead. Specimens of the latter metal are frequently found, which run from 5 to 10 
 per cent of silver, but there is seldom over a few pounds of such ore found at one 
 place. Lumps of this cerargyrite weighing a few ounces have frequently been 
 met with. Only one or two lumps weighing over a pound have ever been found. 
 Such pockets are always small, and it is rarely that many tons of ore averaging 
 over loo ounces are found at one place. 
 
 THE ORES IN POSITION. 
 
 There has been so much ore removed from the current under the White 
 porphyry that it is difficult to give a good idea of the ore in the current taken as 
 a whole. Its thickness in different parts and its richness may be shown from the 
 size of the stopes and their thickness, from the appearance of the streaks of ore 
 found in the old workings and by referring to the ore sales, but with regard to the 
 ores forming the different parts of the body, their relative size and their position 
 very little information can be given. Under the Gray porphyry as clear a view 
 as could be desired is obtained of the ores standing, in all parts of the current. 
 
 THE UPPER CURRENT. 
 
 This current reached its greatest thickness in the Evening Star. The thick- 
 ness of the ore at the centre of the current was, as already stated, very great. At 
 the centre and north-western side the ore varied from 30 to 60 feet in thickness 
 and contained so little waste that there was often great trouble in getting material 
 with which to fill the cribs. From the centre the ore rapidly thinned towards 
 the south-eastern side, till at the upper shaft it was very thin, and a little beyond 
 it ceased altogether. The bottom of the ore-body was extremely irregular and 
 ended in a series of branchlets, streaks and isolated bodies running through or 
 lying in the gangue below. Much of the ore at the bottom was very siliceous, 
 hard carbonate of lead ; some of it low-grade ore consisting of iron impregnated 
 with cerargyrite. The top of the current was more regular, being against the 
 porphyry. It must not be thought that the porphyry was a perfectly smooth 
 sheet. On the contrary, it was very irregular, but the irregularities were all 
 local. The sheet taken as a whole is smooth enough, but it has innumerable 
 hollows and gashes, many of them of considerable size. These were generally 
 filled with ore or silica. 
 
 The quality of the Evening Star ores is shown by the sales to have been very 
 fine. The percentage of lead is low when compared with the Morning Star ores ; 
 
40 . OCCURRENCE OF THE ORES. 
 
 but in silver they run much higher. In Part II., a table is given showing the pro- 
 duction of ore for both mines and their average richness for August, September 
 and October 1882. This table shows the stated differences very plainly. The 
 average of the Evening Star for the year before would have been considerably 
 higher in both silver and lead. The silver for that time averaged from 50 to 60 
 oz. per ton ; the lead was still far lower than the average in the Morning Star 
 portion of the same current, which is also higher in lead than the average of the 
 Lower Waterloo ores. In the Evening Star the top of the main body was richer 
 than the bottom, especially in lead. 
 
 The ore-body thinned as it approached the Morning Star boundary, and 
 entered that claim a much thinner body, though the area occupied by ore was 
 just as large. In some places along the centre it was still very thick, sometimes 
 20 or 30 feet. At other places along the sides of the current some barren spots 
 occurred, but the continuity of the ore was never broken. The percentage of 
 lead in the ores begins to increase and the silver, though still high, begins to 
 decrease in amount. The ground in this part of the property was stoped by the 
 old Company ; but the nature of the ores can be inferred from the streaks over- 
 looked which are every now and then discovered. There seems to have been 
 along the contact some very pure carbonate of lead which ran very well in silver, 
 from 25 1040 oz. The contact was very irregular and had along it much spongy 
 silica, some of which was quite pure and some mixed with ore. Below the pure 
 streak of "sand" carbonate there was much very highly siliceous ore containing 
 scarcely a trace of iron. The ore passed on towards the Upper Waterloo shaft, 
 No. i, Plate II, where there was very pure cerussite along the contact and a 
 great deal of hard carbonate, now often containing iron, below. More of this 
 hard ore occurred in this part of the property than any where else in either mine. 
 Beyond this the rest of the current was still standing last fall. The hard car- 
 bonates cease and streaks of basic sulphate of iron begin to appear under the ore 
 just beyond the last-mentioned shaft. The pay-streak was weak at first, but 
 rapidly strengthened and developed into a fine body of large area of which 
 section i, Plate I, is typical. The blue of this section shows the lead-ore, which 
 assays from 68 to 75 per cent lead and averages as high as 70 to 72 per cent. It 
 lies immediately below the porphyry. The section shows neither the thinnest 
 nor the thickest part of the body, but represents a fair average. The yellow 
 band represents the yellow sulphate of iron. This material contains, intimately 
 mixed with it, from 10 to 30 per cent of anglesite, and sometimes a little car- 
 bonate of lead. In silver it generally runs from 4 to 6 oz. In section i this 
 material is seen to reach the contact at one place, cutting off the cerussite. It 
 runs on beyond this point for 30 or 40 feet, maintaining a thickness of loto 14 feet, 
 and then thins out and disappears, ordinary iron taking its place. These sul- 
 
THE LOWER CURRENT. 41 
 
 phates, being of so low a grade, are left in the mine as waste, or if they have to be 
 removed they are sent up for the dressing dump. 
 
 This body of ore, though of so low a grade in silver, is remarkable for the 
 rich pockets that occur in it. These are both large and small. The small ones 
 often contain little nuggets of chloride of silver. There are only one or two of 
 the larger pockets, and they do not contain excessively rich ore. They are from 
 20 to 30 feet through each way, and vary from 50 to 300 ounces in silver, with an 
 average of 75 to 100 ounces. The yellow sulphate below these pockets is also 
 pay-ore. Whether this rich ore has arisen from a concentration of the silver 
 from the poorer ores around it, or whether it comes from galena richer than the 
 rest, it is hard to decide. The fact that in the Lower Waterloo galena samples 
 taken from the same drift, and from what was once the same body, differ greatly 
 in their silver contents shows that the last is certainly possible. 
 
 Before leaving this current it may be worth while to describe a dike of Gray 
 porphyry which breaks up in this part of the mine on the northern side of the 
 current. This dike rises to the contact and spreads out along it. The ore thins 
 as it approaches it and ends, at some places, in direct contact with it. The only 
 drift that cuts through this dike shows it to rise up with a thickness of 8 or 10 
 feet at this point. It lies in a sheet along the White porphyry above, in some 
 places 30 or 40 feet wide. At the western end an upraise shows it to have a thick- 
 ness of about 25 feet. No ores were found beyond this dike, but when the drift 
 stopped there was limestone in the face of it. The dike showed the character- 
 istic structure of the Gray porphyry. It was in a highly decomposed condition, 
 soft and changing into clay just as the decomposition goes on in the lower work- 
 ings. All about it the White porphyry decomposes to the dry siliceous product, 
 often showing specks of white mica which has been so frequently mentioned. 
 
 THE LOWER CURRENT. 
 
 The smaller branch current under the Gray porphyry begins at the lower 
 north-west corner of the Evening Star claim, and runs with a north-easterly 
 course till it joins the larger one. The area occupied by pay-ore in this current 
 is remarkably large, though the ore is never very thick, being seldom more than 
 six or less than two feet through. 
 
 In the Evening Star there" is very little carbonate of lead. Almost all the ore 
 is the basic sulphate of iron mixed with anglesite. The carbonate of lead is not 
 continuous, but occurs in narrow pure streaks of small extent, generally along the 
 contact and always underlaid by the other ore. Sometimes small lenticular 
 strips of carbonate of lead occur imbedded in the sulphates but parallel to the 
 contact. The thickness of the pay-ore in this part of the current is variable. 
 
42 OCCURRENCE OF THE ORES. 
 
 Four feet is a good average. Along the sides of the current the ore is very 
 irregular and ends in deep gashes running into the waste, from which it is easily 
 distinguished by the color. Below the ore there is sometimes much ferro-siliceous 
 gangue, very hard, but more commonly only the black iron-ore. 
 
 After passing the Morning Star line the ore in the current weakens some- 
 what and, along the lower south-eastern side especially, is very thin. At the same 
 time the carbonate of lead becomes relatively more abundant, until at about a line 
 drawn across the current through the Old Forsaken shaft, No. 8, Plate II, there is 
 a continuous seam of " sand " over one of the yellow ore. Though here only a 
 foot thick, the two bands are remarkably well separated from one another, 
 as analysis No. (2), page 34, and that on page 36 show very well. The two speci- 
 mens from which the analyses were made lay within six inches of each other in 
 the mine, and were both taken from a specimen of only a few pounds' weight, of 
 which the lower half was the sulphate and the upper the carbonate. 
 
 From this point the ore begins to thicken and rapidly develops into a fine 
 body which extends without change almost to the Old Waterloo shaft. This 
 body has a continuous streak of lead carbonate above it, and one of the yellow ore 
 below. On the north-west side of the current the ore is the strongest all the way 
 along, and the carbonate of lead streak is thinner than the sulphate, the ratio 
 being about i : 2. On the lower south-eastern side the pay-streak is not so strong, 
 and the carbonate of lead is relatively much thicker. Section 2, Plate I, shows a 
 section of this body running along the centre of the current. The carbonate of 
 lead streak is seen to be very much the thicker of the two here, but further up 
 towards the north-western side this is not the case. . 
 
 Above this body of ore there is a siliceous sheet, soft, loose and resembling 
 moist sand more than anything else. Further from the ore it is harder, and has a 
 jointed structure which divides it into small, angular blocks but a few inches in 
 thickness. This firmer material resembles a softened and disintegrated quartzite. 
 It varies from 2 to 10 feet in thickness, and when penetrated soft Gray porphyry 
 is found beyond. The lead carbonate mixes with this sandy material. At the 
 bottom of the streak it is as a rule pure, as shown by the analysis, page 34. 
 Towards the top it gradually becomes more impure and merges into this soft 
 siliceous layer, so that in most cases no boundary can be distinguished. 
 
 Though averaging much lower in lead than the Upper Waterloo ores, the 
 carbonate of lead is richer in silver in proportion to its lead contents. It assays 
 from 15 to 30 ounces in silver and from 30 to 50 per cent of lead. Below this 
 streak the yellow sulphate is very pure and always good ore. It is low in lead, 
 but is richer in silver than the carbonate. Assays show it to vary greatly in 
 value. From 20 to 80 ounces per ton in silver and from i to 20 per cent in lead 
 are the usual amounts of these metals in this ore ; the average is from 40 to 50 
 
THE LOWER CURRENT. 43 
 
 ounces and from 5 to 15 per cent. Most silver is found, as a rule, where there is 
 most sulphate of lead, though this is not always the case. No specimen showing 
 visible chloride was ever observed in this current. 
 
 This ore-body begins to diminish in breadth and thickness about 50 feet 
 before the Old Waterloo is reached. The yellow ore diminishes most rapidly 
 and opposite this shaft appears only in isolated patches, mostly below, sometimes 
 above, the carbonate of lead. Up to this point the dip of the Gray porphyry has 
 been quite gradual, but here the line is reached where the entire sheet assumes a 
 much steeper dip (from 30 to 35). The crest of this bend is marked by the 
 Lower and Old Waterloo shafts, both of which are situated upon it. The ore 
 passes over this bend and still continues a pay-streak, though much changed in 
 nature. Both the siliceous sheet above and the sulphate below have disappeared, 
 and the ore now consists of narrow streaks of granular carbonate of lead, with a 
 great deal of highly siliceous and very hard ore below so hard that it barely 
 pays to mine it, although it yields $10 to $15 net per ton from the smelter. 
 
 The other branch current and the main current below their juncture are very 
 different. The ores of the northern branch current are principally galenas. 
 They do not occur in large, continuous bodies as do the ores in all other places, 
 but form a series or string of small bodies which are, however, very rich. The 
 ore in this part of the mine overlies black iron-ore except in the case of a single 
 pocket of large size, where a seam of yellow ore, very thin but exceedingly rich, 
 occurred. Above the lower shaft, No. 6, where the dip is not so great, the ore is 
 in larger bodies than just after the steep dip is begun. At one place the ore 
 occurred as small irregular seams of galena, seldom as much as a foot thick, 
 scattered along the contact, and in black iron-ore through a zone reaching 6 to 8 
 feet from the porphyry. Everything has to be stoped in such a body, and the 
 galena separated from the iron by careful sorting. The largest of these bodies 
 always contains much carbonate of lead, as already sufficiently mentioned under 
 the head of Galenas. 
 
 Below the juncture of the two currents the ore-bodies are larger and" more 
 completely oxidized. They also run much less in silver than the galenas. Section 
 3, Plate I, is taken along the strike through the ore in this part of the mine. It is 
 at a point only a short distance below the juncture of the smaller current. It 
 consists of a low-grade carbonate of lead of average quality in silver. The 
 impurities, which are abundant, are mainly ferruginous. Galena occurs only as 
 nodules, and now forms but a small portion of its bulk. This body begins about 
 75 feet from the Henrietta line and extends southward to the other side of the 
 current. Toward the east it stops suddenly on the crest of a very steep dip 
 taken by the porphyry at an angle of at least 70. It continues at this rate for 
 about 20 feet, and then resumes its regular dip. The ore begins again 30 or 40 
 
44 OCCURRENCE OF THE ORES. 
 
 feet beyond, and has continued from this point on as far as exploration has been 
 pushed, a distance of about ico feet. The grade of the ore has improved a little 
 also, and the average of silver is higher than has been struck anywhere else in the 
 current except in the galena ores already mentioned. 
 
 The difference between the degree of oxidation of the two branches is very 
 striking. The fact that the ores of the one are completely oxidized while those 
 of the other are not nearly so, and that below the junction the ores, though 
 further from the surface, are more completely oxidized than the ores in the large 
 branch, shows undoubtedly that the smaller current has for some reason been the 
 course of greater quantities of meteoric waters. As 'the smaller current cuts 
 across the dip of the stratum and makes a sharp angle with the outcrop, all the 
 waters entering at the outcrop and following the contact between the outcrop of 
 the current and its junction with the main channel would go down to it, while the 
 other current, being perpendicular to the outcrop 'and following the dip of the 
 porphyry, would be the recipient of comparatively little. That water did pass 
 along both currents many channels washed out along the contact prove. 
 
 THE DEPOSITION OF THE VEIN-MATERIALS. 
 
 There can be little doubt as to the way in which the vein-matter was 
 deposited. The evidence tending to show that " the process of deposition of the 
 vein-materials was a chemical interchange, or actual replacement of the rock mass in 
 which they were deposited" seems the more indisputable the more one sees of the 
 deposits. The great changes due to extreme oxidation and the action of large 
 quantities of surface-waters for such a long period of time render it impossible to 
 trace step by step the way in which the replacement was accomplished, but that 
 it did take place there is sufficient proof. 
 
 During September and October, 1882, the upper shaft of the Evening Star 
 was sunk, from 8 feet below the contact, 100 feet towards the Gray porphyry 
 sheet. It was mentioned above that this shaft strikes the south-eastern edge 
 of the main upper current. The ore here was not very thick, much of the area 
 had no pay-ore, but there was from 4 to 8 feet of vein-matter along the contact 
 about the shaft. On sinking the shaft, limestone was entered at the very start; 
 namely, at 8 feet below the porphyry. It was stained and much altered, coarse- 
 grained but firm, although not nearly as solid as the normal blue limestone. This 
 limestone continued only 10 feet, and at 18 feet below the contact iron was again 
 entered. Both the upper and lower sides of the limestone layer were parallel to 
 the dip of the formation, and the bedding-planes, which were well marked, were 
 likewise parallel to it. The iron below was of the common soft variety and con- 
 
THE DEPOSITION OF THE VEIN-MATERIALS. 45 
 
 tained sulphates. It had no limestone in it. This streak lasted but 7 feet, and like 
 all the others, above and below, was parallel to the dip of the formation. Lime- 
 stone was again entered at 25 feet below the contact. This layer was so softened 
 and disintegrated that it had lost all coherency and was very loose and crumbly. 
 The bedding-planes were completely obliterated. It is met with in other parts of 
 the mine, and the miners have the special name "lime-sand" for it. At 35 feet 
 another layer of iron appeared, and continued without interruption for over 40 
 feet. This iron was firmer than the other layer, but still contained some sulphuric 
 acid. At about 50 feet it contained from 5 to 20 per cent of lead, and here and 
 there nodules of galena poor in silver. This lead bearing material occupied a 
 zone parallel to the dip of the beds. At about 80 feet " boulders" of limestone 
 began to appear, imbedded in the vein-matter. These isolated lumps showed, 
 when large, the bedding-planes in position and having the regular dip. They 
 became more and more frequent, until at 100 feet solid limestone was reached, 
 the purest struck anywhere on either mine. At this depth the sinking was 
 temporarily stopped. 
 
 It would be hard to account for these layers of limestone and " boulders" all 
 in position if a pre-existing cave were assumed. They can only be satisfactorily 
 accounted for by supposing the iron to be in the position of former layers of lime- 
 stone, which allowed an easier passage for the flowing waters, and that along 
 these courses the vein-matter was deposited by replacement. 
 
 All the iron which lies near the ores or along evident water-courses, although 
 containing much more iron and manganese as oxides, has always a considerable 
 though variable amount of basic sulphates. The yellow ore which underlies the 
 lead carbonates in some places, and which is supposed to have been formerly iron 
 pyrites with a little galena, consists, as has been already stated, altogether of 
 basic sulphate. It would seem that if the conditions, when these sulphides were 
 decomposing, favored the formation of basic sulphates, the latter compounds would 
 have existed in large quantity in the iron lower down, provided this had formerly 
 consisted of the sulphides of iron and manganese. The analysis given on page 27 
 shows that the more pure variety of iron is almost free from sulphur. The main 
 mass of the vein-matter, in fact, contains little of this element. Further, although the 
 iron often reaches a thickness of 60 to 100 feet, a trace of pyrites has in no case been 
 discovered in it. It seems more probable, therefore, that the iron and manganese 
 were deposited by the ordinary reactions between mineralized waters and lime- 
 stone, the solution depositing its protoxides of iron and manganese and replacing 
 them by calcium and magnesium oxides. The iron and manganese now forming 
 the main body of the currents would accordingly have been deposited as the car- 
 bonates. From these the hydrous oxides as they now exist would be formed by 
 the oxidizing waters. The silica must have been deposited by the replacement of 
 
46 OCCURRENCE OF THE ORES. 
 
 limestone by that substance, molecule for molecule. That the lead and silver and 
 some of the iron were deposited as the sulphides there can be no doubt. The 
 proofs of this have, however, been given under the description of the different 
 ores. 
 
 SOURCE OF THE VEIN-MATERIAL. As to the source of the vein-material, 
 no careful study of the question was attempted, as neither time nor data could be 
 found. The White porphyry, of which an analysis is given on page 21, showed 
 no traces of lead or silver, but also showed scarcely a trace of sulphur, though the 
 rock at one time certainly contained much iron pyrites. Although it seems 
 strange that such immense quantities of vein-matter could be derived from a sheet 
 of porphyry, in this case not more than 1000 feet thick and on an average not more 
 than 200 or 300 feet thick, it is hard to account for the formation of the currents 
 in any other way. There is absolutely no proof, as far as could be ascertained, 
 that the vein-matter came from below ; and though development has been exten- 
 sive throughout the camp, none of the alleged " feeders" have been struck. 
 
 The only theory regarding the formation of the deposits that is founded on a 
 careful, thorough and protracted study of the deposits of the whole camp is that 
 given by Emmons in his abstract of his main Government Report. It is only 
 through such a protracted examination of the deposits, involving not only a 
 careful inspection of all the mines but a great number of delicate chemical analyses, 
 that any trustworthy conclusions can be reached. The data from which his 
 theory is deduced are not yet published, but his published conclusions account 
 most satisfactorily for all the phenomena of the deposits developed in the Morning 
 and Evening Star mines. 
 
PART SECOND. 
 
 METHODS OF EXTRACTING THE ORES. 
 
THE SHAFTS. 
 
 There are two general methods of taking ore out of the mines in use at 
 Leadville; one by means of an incline starting from the surface and running 
 into the hill along the mineral zone, the other by means of a shaft sunk perpendic- 
 ularly until the ore is struck. The latter method is used on the Morning and 
 Evening Star properties, though often in combination with the former; that is, 
 with an incline following the ore from the bottom of a shaft along the contact, 
 through which the ore and waste are conveyed to the shaft by the hoisting-engine. 
 
 It has been stated in a preceding chapter that the Morning Star mine has four 
 shafts at present supplied with engines, and that the Evening Star has likewise 
 four, of which one is used by the two mines in common. The reason for such a 
 number of shafts is obvious. The ore occurs in two separate bodies under differ- 
 ent layers of porphyry, and, as far as present developments show, widely removed 
 from each other horizontally. Hence the ore of each mine could only be taken 
 out through one large shaft by running long and expensive drifts and by handling 
 the ore a great number of times. It is also more convenient tb have several shafts 
 on each body of ore, because the very slight dip of the porphyry soon carries the 
 workings a long way horizontally from the shaft, giving rise to the same difficul- 
 ties mentioned above. On the other hand, the distance of the ore below the sur- 
 face is so short, varying from 80 to 400 feet, that the cost of sinking is not very 
 great, while a number of shafts allows less work for each, and they can be small 
 and supplied with light machinery. 
 
 On the Morning Star all the shafts, with one exception, were sunk to contact 
 before the consolidation, and that one was nearly completed, so that the present 
 company has not, until lately, found another necessary. On the Evening Star the 
 main shaft was already sunk to contact when the property was bought in 1879. 
 The upper shaft was sunk later by the present company, and the Raworth shaft 
 by the side of the main shaft when the latter proved inadequate for raising the ore 
 of the main ore-body. 
 
 All these shafts are small. They are rectangular in shape and have two com- 
 partments, one for a ladder-way, the other for hoisting. In the Lower Waterloo 
 the ladder-way has been converted into a pumping-compartment. In the new 
 McHarg shaft of the Morning Star there will be a large pumping-compartment, 
 
EXTRACTING THE ORES. 
 
 but no ladder-way, 
 shafts : 
 
 The following tables will show the dimensions of the various 
 
 SHAFTS ON THE MORNING STAR. 
 
 NAME OF SHAFT. 
 
 No. 
 
 Depth to Con- 
 tact. 
 
 Dimensions of Lad- 
 der-way. 
 
 Dimensions of Hoist- 
 ing-Compartment. 
 
 Size of Shaft in the 
 clear. 
 
 
 I 
 
 460 
 
 4x5 
 
 *, X 5 
 
 c x O 2 
 
 Main Shaft 
 
 2 
 
 265 
 
 3.8 x 4 
 
 4x4 
 
 4X8 
 
 Old Waterloo 
 
 5 
 
 135 
 
 3.4 x 3.5 
 
 3-5 x 3-5 
 
 3.c x 7 
 
 
 6 
 
 140 
 
 3-3 x 3-3 
 
 3.3 x 3.3 
 
 3.3x7 
 
 McHarg Shaft 
 
 
 
 4.5x5 
 
 4x5 
 
 5 X O 
 
 
 
 
 
 
 
 SHAFTS ON THE EVENING STAR. 
 
 NAME OP SHAFT. 
 
 No. 
 
 Depth to Con- 
 tact. 
 
 Dimensions of Lad- 
 der-way. 
 
 Dimensions of Hoist- 
 ing-Compartment. 
 
 Size of Shaft in the 
 clear. 
 
 Main Shaft 
 
 10 
 
 116 
 
 3-7 x 4 
 
 4x4 
 
 4x8 
 
 Upper Shaft 
 
 II 
 
 4OO 
 
 3.2 x 3.2 
 
 4.2X4.4 
 
 a 2 X 7 
 
 
 
 
 3.7 x 4 
 
 4x4 
 
 4x8 
 
 
 7 
 
 81 
 
 3.2 x 3.3 
 
 3.2 X 4.6 
 
 32X7 
 
 
 
 
 
 
 
 COST OF SINKING THE SHAFTS. There were no records kept of the cost of 
 sinking the old shafts. The new McHarg shaft has reached a depth of 300 feet 
 (May i, 1883), of which White porphyry occupied the first 18*0 feet, and iron and 
 limestone the remaining distance. The cost of sinking this 300 feet, including 
 putting the timbers in place, was not quite $18 per foot. The cost of the timber 
 and framing brings the total cost of the shaft completed to $23.50 per foot. 
 
 METHODS OF TIMBERING THE SHAFTS. The soft nature of the ground, and 
 its tendency to swell or cave, render substantial timbering necessary ; and even 
 when the larger timbers are used they often bend in and distort the lining. The 
 ordinary methods of timbering shafts, which are in use wherever timber is cheap, 
 are adopted here. All the shafts are timbered with regular cribs, resting one 
 upon the other. The logs used vary in size, but average 10 to 12 inches in diame- 
 ter. They are usually sawed on the face only, the other three sides being left 
 round, but the bark is always removed. The timbers of the new McHarg shaft of 
 the Morning Star are better made than any others on the property. They are 
 shown in Fig. 4, Plate V. They are sawed on all four sides, and are 9 by 10 
 inches through. The lo-inch face stands vertically. The tenons on the ends are 
 9 inches long, and the shoulders 2 inches each, so that each set timbers one foot of 
 shaft. The shaft is to be 9 feet by 4 feet 6 inches in the clear, so that the longer 
 timbers have the former distance between the tenons, and the shorter the latter. 
 
 The timbers are put in in the following manner : when a convenient depth 
 
CLOSING THE LEVELS. 51 
 
 has been reached below the lowest timbers 8 or 10 feet on an average, but vary- 
 ing according to the nature of the ground notches are cut into the sides at each 
 end, and cross-pieces, prolonged beyond the tenon, as in b, Fig. 4, Plate V, are 
 fitted into them horizontally. Then the sets are built upon these until those 
 above are reached. Every other set is wedged in place firmly by blocks or 
 wedges driven back of it, and any large spaces behind are filled with blocks. 
 Fig. i, Plate VI, represents a section of shaft showing the way the long cross- 
 piece is put in. The shaft is divided into two compartments by heavy planking 
 put across and held in place by 3- or 4-inch scantling, which is spiked to the tim- 
 bers. Four-inch planking at least should be used for this purpose, as anything 
 thinner is apt to be bent in and broken, needs constant repairing, and may cause 
 accidents by catching the bucket as it ascends. The new shaft is to have 6-inch 
 division planking. 
 
 When a shaft reaches the contact a drift is always run from that point. If 
 there is but this one level the timbers are supported on four heavy posts, although 
 the method of timbering and the pressure of the ground against the cribs pre- 
 vent very much weight from settling upon them. Each pair of these posts rises 
 from a sill and is surmounted by a cap. They are similar to the square sets to be 
 described later on. If there is a sump it is timbered like the shaft, these cribs 
 starting below the sets at the bottom of the drift. When the level is above the 
 bottom the arrangement may be the same, except that the posts then set a little 
 further out so that they may rest upon firm ground. Sometimes the cribbing 
 does not stop, but runs all the way down. A place is then cut in the side and a 
 frame put in for the landing at the first level. The height of these sets varies ; 
 where there is no incline they are generally 6 feet high. 
 
 CLOSING THE LEVELS. When an upper level is not in use it is closed by a 
 door. The door most commonly used, and by far the simplest and most conven- 
 ient, is arranged as follows : two strong hinges hold it to the edge of the sill of 
 the set at the shaft, and, as the length of the door is made greater than the height 
 of the set, the top rests against the side of the cap towards the shaft when the 
 level is closed, and is held there by a counterpoise. When the level is in use the 
 door is thrown back against the opposite side of the compartment, and its weight 
 is then sufficient to keep it there. The bottom formed by such a door has a 
 slope of about 60, and the bucket, on striking it, slides into the drift. The face of 
 the door has longitudinal strips of boiler-plate riveted on it to keep the bucket 
 from tearing the wood. Where an incline is used and a truck has to be run 
 under the shaft, as at the first level of the Morning Star main shaft, the door is 
 made shorter, so that it just reaches across the shaft and rests horizontally on a 
 support fastened to the other side. The truck then runs up on a track which 
 is spiked on the back of this door. 
 
EXTRACTING THE ORES. 
 
 THE DRIFTS. 
 
 Drifting commences from the contact. The drifts are either horizontal, i.e 
 drifts which run along the strike, or inclines which follow the dip of the por- 
 phyry. A level drift does not change its height on running into a shaft. The set 
 in the shaft is the same height as the rest. When there is an incline with a track 
 the first few sets from the shaft are higher, and gradually run down to the normal 
 height of the drift, so that a more gradual turn for^the rope may be obtained. 
 Owing to the loose nature of the ground and its great tendency to cave, the drift 
 timbers have to be very substantial, and, although they are obtained at reasonable 
 prices, they form, after the labor and smelting accounts, the largest item of ex- 
 pense. The lumber and timber used is all pine, the only tree that grows in great 
 abundance about Leadville. 
 
 COST OF TIMBER. The timber is bought as round logs, and contracts are 
 made for its delivery at the mines. The following were the prices paid by the 
 Evening Star mine for logs delivered during October and November, 1882 : 
 
 Logs 10 feet long and 10 inches in diameter at small end $o 60 
 
 " 12 " 14 135 
 
 " 14 " 14 " I 50 
 
 14 " 16 " I 80 
 
 The Morning Star was having delivered about the same time the following 
 sizes : .] 
 
 Logs 12 feet long and 10 inches in diameter at small end $o 75 
 
 " 14 10 080 
 
 " 16 " 10 " 090 
 
 The annexed table of prices from a contract of the latter mine made in No- 
 vember, 1 88 1, is more complete: 
 
 Logs 14 feet long and 12 inches in diameter at small end $ 40 
 
 14 14 75 
 
 14 16 85 
 
 12 12 .'. 30 
 
 12 14 50 
 
 12 16 60 
 
 16 16 2 10 
 
 12 8 030 
 
 14 6 030 
 
 14 10 090 
 
 14 8 050 
 
 Lagging 16 feet long and 4 to 6 inches in diameter o 25 
 
 All the logs brought to the mine for delivery must be sound and good accord- 
 ing to contract. They must also be full length. They are carefully inspected 
 
THE CAPS. 53 
 
 before unloading, and any logs crooked, unsound, short, or in any way failing to 
 comply with the terms of contract are rejected. A certain time is set during 
 which the logs are to be delivered, and generally a given number has to be 
 brought each week. Weekly payments of 75 per cent are made for logs deliv- 
 ered and the balance is paid when the contract is fulfilled. All the mining, 
 timbers are made from these logs. 
 
 TIMBERING DRIFTS. 
 
 In timbering drifts the ordinary set is used, consisting of a sill, posts, cap and 
 braces. Besides these, wedges are used to hold them in place, and lagging to hold 
 up the loose dirt. A brief description of these pieces may be advisable, as they 
 have to be carefully made. 
 
 THE POSTS. These are made of various sizes. Heavy or light ones are used 
 according to the nature of the ground and the amount of use the drift will be 
 put to, but the same sized timbers are used throughout. Generally the logs are 
 sawed on the face only, and are left round on the other three sides. A tenon of 
 2 inches is made at the top, with shoulders on the front and the two sides. The 
 front shoulder is always 2 inches deep;, the side shoulders only about i, but 
 vary according to the size of the log, as the tenon has the fixed width and the 
 space left over on either side forms the lateral shoulders. Thus if a 1 2-inch post 
 were to be made from a 14^-inch log, the tenon would be just 12 inches across and 
 ij inches would be left for each side shoulHer. The faces of the tenon are care- 
 fully squared, and the top made square, with the front face of the post. The 
 bottom of the post has no tenon, but is sawed off square. The length varies 
 according to the use to which the drift is to be put. For an ordinary track-drift 
 the posts are 6 feet 4^ inches long over all. A post is shown, drawn to scale, in b, 
 Fig. i, Plate V. It is made from squared timber, as is sometimes done, but does 
 not differ from the round posts in any other way. 
 
 THE SILLS. These are not, as a rule, as heavy as the posts ; they are often 
 sawed square, and always on the upper and lower sides. They are usually 8 
 inches thick and 12 inches wide when made for a 1 2-inch post. They have a 
 9-inch tenon at each end, with one shoulder of 2^ inches on the upper side. The 
 posts rest upon these tenons, and the faces come close against the shoulders. 
 The length between the tenons is generally 4 feet. Fig. 2, Plate V, shows a sill. 
 
 THE CAPS. The caps are made of logs corresponding to the posts in size. 
 When the latter are not square, neither are the caps, but are then sawed only on 
 the lower side. They have a tenon at each end which is 9 inches long on the 
 under side. On this side the collar is 2 inches deep. When this tenon rests on 
 the top of the post, the shoulder of the cap comes against the tenon of the post 
 
54 EXTRACTING THE ORES. 
 
 and the face of the cap rests against the front shoulder of the post. There are 
 shoulders on the sides of the cap also, but these are, like those on the post, 
 seldom over i inch deep. They start 2 inches back of the lower shoulder ; that 
 is, 1 1 inches from the end of the cap. The length of the cap, like that of the 
 sill, varies greatly. Usually it is 5 feet 10 inches over all ; that is, 4 feet in the 
 clear, a, Fig. i, Plate V, represents a cap. It is turned lower side up to give a 
 better view of the tenon. 
 
 COLLAR- AND FOOT-BRACES. These are made of sawed timber. They are 8 
 by 10 inches thick, and of varying length. They are sent down the mine in long 
 pieces and cut of the length required when the set is put together. The collar- 
 brace rests on the lateral shoulders of the posts and against those of the caps. 
 The foot-braces lie on the floor of the drift between the posts. 
 
 Fig. 3, Plate V, shows three sets of drift timbers of about the usual strength 
 for an ordinary track-drift. From this figure it may be seen how the various 
 timbers fit upon one another. It must be remembered that in the ground the 
 space between the sills is filled in, and that the foot-braces, which do not lie on 
 any shoulders, rest upon this filling. 
 
 As accessories to the set Wedges and Lagging may be mentioned. 
 
 WEDGES. Wedges hold the timbers in place until pressure sets upon them. 
 They are made from any suitable material. Waste lumber or logs are sawed into 
 blocks 1 6 to 1 8 inches long and these ripped into pieces about 4 inches square. 
 Such a piece is then sawed from one end edge diagonally across to the other, 
 thus forming two wedges. 
 
 LAGGING. This is only used where the ground is loose enough to cave. It is 
 generally required over the caps and often behind the posts. It may be of any 
 light material, but is most commonly round sticks 3 to 5 inches in diameter. 
 These are of any convenient length, frequently about that of two sets. The ends 
 of the pieces are cut obliquely on opposite faces so that they form parallel sur- 
 faces. They then fit end to end and make a tight joint. Any other light material, 
 like slabs, may be used for lagging. Everything used in drift-timbering has now 
 been mentioned. 
 
 Certain precautions should be used in making these timbers and putting them 
 together. The following are the most important: (i) In making the various 
 timbers, care should be taken that they fit perfectly when put together. The 
 tenons and shoulders should be made accurately to measurements and carefully 
 squared. The centre-lines should be plainly marked on the inside faces so that 
 they may be used in putting up the set. (2) In ordinary drifts the sets should 
 stand perfectly vertical. The sill should be placed with the utmost care, as the 
 strength and durability of the set depend greatly upon this. A trench is dug for 
 it, and the sill then set in with the upper face perfectly horizontal, and, in a level 
 
COST OF DRIFT-TIMBERS. 
 
 55 
 
 drift, on a level with the preceding sill. If the drift has a slight inclination, say of 
 2 inches per set, the sill is given this difference of level. In preparing this trench, 
 especially where the ground is not very hard, the center should be dug lower 
 than the ends, so that the middle of the sill cannot touch. The pressure of the 
 roof, exerted through the posts, presses the ends of the sill into the ground, and, 
 when the ends sink, if the middle meets with resistance it will spring up and the 
 sill will be broken, just as a stick is broken across the knee. Neglect of this pre- 
 caution constantly results in the breaking of sills, this being one of the most com- 
 mon ways in which they are destroyed. The necessity for removing the ground 
 that would bear at the center applies also in placing the posts and caps. Fig. 2, 
 Plate VI, shows typically how the ground should bear on a set in a drift. (3) 
 The lagging should be neither too strong nor too close together. Soft ground 
 will often swell for a time after it is exposed with irresistible force. If the lag- 
 ging be too close this will easily break it, while if it be further apart the soft 
 ground will be forced into the interstices and the pressure will thus be relieved. 
 It is for this reason, also, that round logs are often preferred to square ones in 
 timbering winzes which pass through vein matter. Where the ground is not soft 
 and plastic, but dry and very crumbly, close lagging may be advisable. The 
 harm resulting from using too strong lagging is also apparent. As long as the 
 pressure is not excessive the lagging should hold up the ground. But, since all 
 the pressure on it is conveyed to the sets, if the lagging be very strong this may 
 be sufficient to crush them. It is, however, better for the lagging to bend or 
 break, as it costs much less than the sets. 
 
 COST OF SETS. The cost of the various pieces of a set, framed and ready 
 to be put up is given below. The posts are ordinary ones of 1 2-inch tenon ; that 
 is, made from a 14-inch log. Sets three feet apart from centre to centre. 
 
 
 Timber. 
 
 Framing. 
 
 Sawing. 
 
 Total. 
 
 One sill 
 
 $0 67 
 
 $0 18 
 
 $O IO 
 
 $ 95 
 
 
 I 50 
 
 22 
 
 IO 
 
 i 82 
 
 
 68 
 
 4O 
 
 05 
 
 I 13 
 
 Two collar- brace c 
 
 ao 
 
 
 
 30 
 
 
 3O 
 
 
 
 30 
 
 
 
 
 
 
 Total , 
 
 $3 45 
 
 $0 80 
 
 $o 25 
 
 $4 50 
 
 
 
 
 
 
 The distance of the sets apart varies according to the nature of the ground. 
 Sometimes they are not more than 2\ feet from centre to centre, sometimes they 
 are as much as 5 feet. The average is about 3 feet, which would make the cost of 
 the framed timbers $1.50 per running foot of drift. This estimate is exclusive of 
 wedges, lagging, and the cost of putting the sets in place, which would bring the 
 cost very nearly up to $2 per foot. 
 
56 EXTRACTING THE ORES. 
 
 THE STOPES. 
 
 * 
 
 The pressure on the sets is often enormous. It may arise from two causes, 
 swelling of the ground, owing to access of air, or an actual caving or settling of 
 the roof. The latter is far the more powerful source of pressure, and is more 
 common than the other, especially under the White porphyry. When a large 
 body of ore is being stoped along a drift the whole region settles. The caps are 
 often crushed to splinters on the posts and broken in the middle, while the sills 
 spring up at the center and thus almost close the drift. To support the roof in the 
 slopes the most substantial methods of timbering have to be employed. The stope 
 supports are simple. They are stulls and head-blocks, cribbing and square sets. 
 
 STULLS AND HEAD-BLOCKS. These are employed as temporary supports to 
 hold the roof during sloping until more permanent ones can be made. They may 
 be permanenl only where Ihe stope is very small and the spaces between them 
 are at least partially filled with waste. The stull is merely a post or log, and is 
 made 10 or 12 inches shorter than Ihe dislance belween Ihe walls where il is to 
 be used. The head-block is a block sawed on two opposite faces, and about i foot 
 thick by 16 inches broad and 2 feet long. In selling Ihem up a smooth place is 
 made on Ihe floor for Ihe slull, and on Ihe roof for Ihe block. The stull is then 
 put up and the block put over it. Wedges are driven above the block until Ihe 
 stull is held in position. Pressure soon setlles upon it, and it is then held lighlly. 
 The slull is always pul in al right angles to the roof. Fig 4, Plale VI, shows a 
 slull in posilion. The wedge used lo hold it up in Ihe firsl place is driven from 
 Ihe lower side. 
 
 CRIBBING. Cribs are Ihe mosl common slope supports in the Evening and 
 Morning Star mines, and, though Ihe mosl expensive, are by far Ihe mosl sub- 
 slanlial and safe supports. Where Ihe ore-body is very large Ihey are almosl 
 indispensable. Cribs are generally reclangular in shape. When large, each crib 
 or set consisls of five logs, Iwo large ones, notched at the middle and each end on 
 both sides, and three shorter ones, notched only at Ihe ends. Two long logs are 
 laid down, and Ihree short ones are placed across Ihem, Ihe nolches filling inlo 
 each olher ; Ihen Iwo more long ones, and so on up, sel above sel, unlil Ihe roof 
 is reached. If Ihe plalform on which Ihey resl be nol horizontal, an extra log is 
 put under the lower side as in the figure. The size of the logs varies, but com- 
 monly a lo-lo 12-inch log is employed. 
 
 The cribs are carried lo Ihe roof, and Ihe compartmenls in them are carefully 
 filled as full as possible with waste, as Ihis helps lo keep Ihe cribs in shape and to 
 support the pressure. Il is also well, if Ihe cribs are very high, to fill the spaces 
 between the logs with small timber, as Ihis will receive a part of Ihe pressure when 
 
SQUARE SETS. 57 
 
 the cribs settle and remove that much from the ends of the logs. Some of the 
 cribs of the Evening Star are between 70 and 80 feet high, and they are found to 
 be the only thing that will support the roof in such places. Fig. 3, Plate VI, 
 shows the form of a set of cribs. The foundation and roof have been smoothed 
 off, and the cribbing is built up vertically although the floor slants. The compart- 
 ments are completely filled with waste. 
 
 SQUARE SETS. This form of stope timber is seldom used in either mine, es- 
 pecially in the Morning Star. The square sets used here differ from those in use on 
 the Comstock Lode and described by J. D. Hague, and are apparently not so 
 good a form. They differ in no essential way from the ordinary drift set already 
 described, only the post has a shoulder on the fourth side for an additional collar- 
 brace. One set is placed directly upon the other, the cap of the lower forming the 
 sill of the one above. Where the ore-body is large and regular this form of 
 support is not now used. Where it is very irregular and narrow, but runs some 
 distance vertically, it is always used. In stoping, if square sets are to be used, a 
 face is started as wide as a set, and extending from the top to the bottom of the 
 ore, and this is run forward through the block like a great high drift. But if 
 cribbing is to be used in a large body they start at the bottom, dig under the 
 body and prepare a foundation of proper shape and size, and then work up, stop- 
 ing overhand and taking out a pillar. The cribbing is built up as fast as the ore 
 is taken down, and any waste is utilized for filling up the cribs. In such places it 
 is often difficult to get waste for this purpose. 
 
 For making all these timbers each mine is provided with a saw-mill and 
 framing-rooms. In both cases they are connected with a shaft-house, and the 
 same boiler supplies the steam for the hoister and the engine which runs the saws. 
 Only plain sawing, cutting into lengths and making wedges is done by machinery; 
 all the rest of the framing is done by hand. As soon as the timbers are sawed 
 they are taken to the framing-room, framed and stored in piles of pieces of the 
 same kind and size, ready for use. From here they are distributed to the various 
 shafts of the mine as needed. The crib is either notched on top with an adze or is 
 sent below of the desired length and notched when used. The log-yards are just 
 above the saw-mills, so that the logs are easily obtained. A team brings them to 
 the mill and distributes the framed timbers. 
 
 The cost of drift timbers has already been given. Cribs cost according to the 
 size and length of the logs from which they are made. Any pieces cut off the 
 regular length are made into wedges or head-blocks, and the expenses of framing 
 them are small. The timber for one crib of two 14-foot logs and three ro-foot 
 logs, all 10 inches in diameter at the small end, will cost $3.60. Good lagging 
 costs about \\ cents the running foot. Wedges cost, ready made, a little over i 
 cent apiece, head-blocks about 10 cents, and stulls 6 cents the running foot. 
 
5 8 EXTRACTING THE ORES. 
 
 SHAFT-HOUSES. 
 
 Although the arrangement of several shaft-houses on both mines is more com- 
 pact, that of the Lower Waterloo has other and more important advantages, and, 
 though not so large, it is in many ways better than any of the others. It is more 
 complete and has machinery superior to that of any shaft on Carbonate Hill, and 
 the arrangement of the dumps is also very good. It has therefore been selected 
 for description. 
 
 MACHINERY. The hoisting-engine was made by J. W. Jackson, of Denver. 
 It is a powerful one and capable of much more work than it is now required to 
 do. The spool is 4 feet in diameter. It is worked by friction gearing, as are 
 most of the hoisters of the camp. The large friction-wheel attached to the spool is 
 6 feet in diameter and works against a 2-foot paper-tired wheel. The axle of the 
 wheel rests in eccentric sockets, so that by turning the latter one way the large 
 friction-wheel is thrown against the small, while by turning the other way it is 
 thrown against the break-block. The spool rests on a solid wooden frame which 
 is on a massive masonry foundation. The rope is a i-inch steel wire cable. It 
 passes to the sheve over a small pulley which revolves on a bar along which it can 
 slide, keeping on a line with the sheve and the point where the rope binds on the 
 spool. The sheve is 4 feet in diameter, and is supported on a strong framework 
 over the hoisting-compartment, which is carefully braced on the side towards the 
 hoister. 
 
 There is a fine air-compressor on the same floor. It was made by Sargeant & 
 Cullingworth, of New York. It was put in for running a pump at the bottom of 
 the incline and for using air-drills, but so far has been used exclusively for the 
 former purpose. This air-pump conveys the water to a sump at the foot of the 
 shaft; from here a steam-pump of peculiar and not very satisfactory pattern raises 
 the water to the surface, a distance of about 200 feet. The steam is supplied by 
 two boilers. At present one of these is able to do all the necessary work, so they 
 are run alternately, being changed every few weeks. The engineer attends to 
 the engine and to firing the boilers. No firemen are employed at any of the 
 shafts. 
 
 The water for the boilers is obtained directly from the city mains, which run 
 immediately under the shaft-house. A large tank holds a reserve, and is filled at 
 will by turning on the tap. The pressure in the main is considerable, and all the 
 lower shafts get their water in this way. The upper shafts, Nos. i, 2, 3, 9, 10 and 
 n, Plate II, are too high up, so each mine has to have a small steam-pump which 
 supplies it with water daily. The water is of excellent quality, containing little 
 or no carbonate of lime. 
 
HOISTING-FLOOR. 59 
 
 HOISTING-FLOOR. The position of this shaft-house, like all the others, is 
 with its greatest length running up and down the hill, in order that the ore-bins 
 may be some distance above the ground, and that a good dump may be obtained. 
 For this reason, also, the hoisting-floor is made higher than the floor of the engine- 
 room. In this shaft-house it is only six feet higher. The shaft terminates at this 
 floor, and everything is hoisted to it. The shaft has two compartments ; one is 
 used for pumping, and the other for hoisting. A bucket, not a cage, is used. 
 The hoisting-compartment rises 8 inches above the floor all around. The front 
 and back of it have a triangular piece surmounting this, which is 10 inches higher 
 at the middle than at the sides. Two heavy doors, hinged to the sides, rest upon 
 these pieces. A rope from each of the doors passes over a pulley about 8 feet 
 above it, and then both ropes pass to one side and join together ; this single rope 
 passes through a third pulley and has a counterpoise attached to it. Hence when 
 one door is pulled open or shut the other is too, and at the same time they work 
 very easily. The doors are always kept closed when the bucket is down. Be- 
 hind the shaft the floor is covered with boiler-plate. From this one track leads to 
 the ore-bins and waste-dump, and another to the " wash" dumps, on which any- 
 thing hoisted too poor to pay, but rich enough to make ore by dressing, is 
 thrown. 
 
 The bucket used for hoisting has a capacity of 6 to 8 cubic feet. Some- 
 times it is of wood, especially where there is no incline, but here and at the 
 Morning Star main shaft it is iron. Iron buckets are made of J-inch boiler-plate, 
 with the seams strongly riveted. They are cylindrical at this shaft, and their 
 length and breadth are about equal. At the other shaft they are shaped like an 
 oil barrel, and are about the size of one. The wooden buckets are of this shape, 
 made of hard wood and bound with -inch wrought-iron bands. When hoisted, 
 the bucket strikes against the doors and throws them open. It is stopped about 8 
 feet above the floor. The dumper then closes the doors and fastens a hook, which 
 is suspended by a rope from a point above and behind the shaft, to a ring at the 
 bottom of the bucket. The engineer lowers, and the rope pulls the bucket back 
 and overturns it into the car, which stands in position against the back of the 
 shaft. It is then hoisted to its former position, the rope unhooked, the doors 
 opened and the bucket again lowered into the shaft. 
 
 The car used is almost exactly like that described by J. D. Hague as used on 
 the Comstock Lode, the only essential difference being in the turn-table, which at 
 Leadville consists of three plates, the upper two of which are hinged together 
 and turn on the third. The door at the end is the same in both cases : hinged at 
 the top, and controlled by a lever in front. These cars are made at the mines, of 
 2-inch pine plank. They are lined with boiler-plate and firmly braced on the 
 outside with bands of the same material. 
 
60 EXTRACTING THE ORES. 
 
 ORE-BINS. The ore-bins are at some distance from the shaft, and a covered 
 passage leads to them. This gives the height above the surface requisite for a 
 sorting-floor and ore-bins below it from which the wagons are loaded. At this 
 shaft the bins are only four in number, two with grates and two without. The 
 grates terminate over a sorting-floor which is 6 feet above the bins. Those with- 
 out grates receive ore on the lower floor immediately, and only such ore as is not to 
 be sorted is thrown into them. The gratings are 4 feet wide, and consist of thirty 
 X ii-inch wrought-iron bars standing on edge. They have an inclination of about 
 60, and stop about \\ feet above the sorting-floor. Below them the floor is guarded 
 with boiler-plate to prevent wear. When the ore is thrown on these grates, all the 
 fine, which is mostly granular carbonate of lead, passes between the bars to the 
 lower floor, while the lumps capable of being hand-sorted fall on the sorting-floor. 
 The sorter goes over all this, throwing the ore into the bins, and the gangue on 
 the waste-dump. The waste-dump is directly beyond the ore-house. It receives 
 only such waste as is very low in silver and lead. Any waste running over 10 or 
 12 per cent of lead is thrown on a separate dump to await dressing. 
 
 The other large shaft-houses are provided with ordinary Colorado hoisters 
 and no other machinery. The Upper Waterloo and Morning Star main shaft- 
 houses are much larger than the Lower Waterloo, and the ore-bins are differently 
 and not so well arranged. These bins are arranged in a row along the hill so that 
 they run across the lower end of the shaft-house, forming a sort of letter T. 
 The car containing ore is run to the crest of the bins and then turned on a piece 
 of boiler-plate to a track at right angles running along the edge of the bins. 
 These bins are ten in number, five with gratings and five without. The car not 
 only has to be turned twice every time the ore is brought up, but, unless the hill 
 is very steep, the hoisting-floor has to be raised very high above the ground to 
 afford sufficient dump. The Morning Star shaft has its floor about 20 feet above 
 the ground. 
 
 All the shaft-houses have sorting-floors, and ore-sorters are constantly em- 
 ployed in taking out the gangue. Sorting not only lessens the amount of ore 
 smelted, but as the percentage of lead is increased the price paid per ton for 
 smelting is lessened, and the price received for the lead is greater per pound. An 
 example will show this more plainly. Suppose 56 tons of ore mixed with waste 
 averages before sorting 29 per cent lead and 35 ounces silver. If sent to the 
 smelter it would sell as follows : 
 
 Received for lead, at :J cents per pound $406 oo 
 
 " " silver, at $1.07 per ounce 2097 20 
 
 $2503 20 
 Paid for smelting, at $14 per ton 784 oo 
 
 Received from smelter $1719 20 
 
JDXIFTS. 6 1 
 
 If the ore had been sorted and brought down to 50 tons, assaying 32 per cent 
 lead and 38 ounces silver : 
 
 Received for lead, at i cents per pound $480 oo 
 
 ' silver, at $1.07 per ounce 2033 oo 
 
 $2513 oo 
 Paid for smelting, at $13 per ton , 650 oo 
 
 Received from smelter $1863 oo 
 
 The practice of putting all the waste raised that is capable of making ore by 
 dressing on separate dumps is now in use at all the shaft-houses on the Morning 
 and Evening Star, and both mines now have large quantities of this material on 
 hand. The third-class dump of the Upper Waterloo gave, by assay from a num- 
 ber of samples carefully taken, from 27 to 30 per cent of lead and from 4 to 6 
 ounces of silver per ton. This dump is higher in lead and lower in silver than 
 any of the others. 
 
 Bancroft UbrS$ 
 
 UNDERGROUND WORKINGS. 
 
 DRIFTS. All the shafts worked either strike the ore or come very near it. 
 As soon as contact is reached development is begun by running exploring drifts 
 along the contact. They are either horizontal or have a decided dip. Such drifts 
 may be divided into two classes; (i) regular highways which collect all the 
 material to be hoisted and convey it towards the shaft, and (2) numerous branches 
 of these which run off developing the ground, each serving at most as the out- 
 let for only a limited territory. The former are the larger, more carefully made 
 and better timbered. They are always supplied with a tramway along which the 
 ore and waste is conveyed in cars or in buckets set upon trucks. The latter, 
 being comparatively little used, are less strongly timbered, and where the ground 
 is good, as in the Lower Waterloo, sometimes not at all. They have no tramway 
 and are not necessarily smooth like the former. The vein-matter taken out 
 through them is conveyed to the nearest track-drift in wheelbarrows. If a shaft 
 or level has no incline up which the ore is drawn by the hoister, only the ore on 
 or above that level is taken out by it, as the dip is too steep to move the ore up 
 hill by hand. If there is such an incline the ore may be taken out for an indefinite 
 distance below. The Morning Star main shaft, No. 2, Plate III, and the Lower 
 Waterloo shaft, No. 6, Plate III, are the only ones that have such inclines. In 
 both cases the incline serves as a main outlet, and side-drifts run out from it hori- 
 zontally. Cross-drifts are again run from these, dividing the ground up into 
 blocks and fully exploring it. The Morning Star incline is the better of the two. 
 It begins at the point where the shaft strikes the contact and, following the con- 
 
62 EXTRACTING THE ORES. 
 
 tact, runs to the end of the property. It is not shown on the section. This 
 incline is perfectly straight and substantially timbered with 1 2-inch sets (i4-inch 
 logs). A single track runs down it. The first 15 feet from the shaft is horizontal, 
 though the sets are higher, so that the top keeps the regular slope of the incline. 
 The set in the shaft has a lo-inch drum at the top. When a bucket is to be sent 
 from the surface down the incline it is lowered to the level. The trammer has a 
 low truck at the foot of the shaft to receive it. A chain just of the right length is 
 fastened to the front of the truck. The trammer receives the bucket, guides it to 
 its proper position on the truck, sees that it rests with its ears across the drift, 
 and hooks the chain over the rim. He then pulls the truck over the crest of the 
 incline and jumps on. The engineer, having merely paused at the level long 
 enough for the bucket to be properly adjusted, now lowers it to its destination. 
 On hoisting, the trammer comes upon the truck and loosens the chain just after 
 the crest is reached, thus leaving the bucket free to go up without stopping. The 
 rope used is hemp, which is much better for this purpose than wire. It bends 
 over the drum in the set at the foot of the shaft, and over rollers at any point 
 along the incline where the slope changes. At various points on either side of 
 this incline horizontal drifts have been run, and from these smaller drifts. All the 
 ore is brought to the incline through these, and there transferred to the bucket. 
 Some of these drifts on the south side are outlets of quite extensive workings, and 
 are provided with tramways and cars. 
 
 The arrangement at the Lower Waterloo is much less convenient, and develop- 
 ing work only is pushed on down this incline. It is intended to take out the ore 
 through the new McHarg shaft, which will strike this contact below the present 
 workings. A level drift runs from the second level of the shaft out 200 feet to 
 the south-east till contact is reached, and here a very steep incline begins, so steep 
 that it is not safe for a man to ride down it. A special truck and bucket have 
 been devised for use on this incline, the rope being fastened to the truck. 
 
 The Evening Star upper shaft has also an incline, but with a very moderate 
 slope, and the ore about it was hauled to the shaft by a donkey kept underground 
 for this purpose. All the other shafts and levels work only the ground at or 
 above their own level, and long horizontal drifts run from these to collect the ores 
 from the contact. 
 
 CHUTES. In a stope the ore is thrown or wheeled to the nearest track-drift 
 below to be taken out. Instead of throwing it on the floor of the drift, where it 
 would be greatly in the way and from whence it would have to be shovelled into 
 the cars, the ordinary chute is used when possible. These extend either from 
 some accessible point in the stope to the track-drift below or, more commonly, 
 from a drift which in turn leads to the stope. Chutes are from 3 to 6 feet wide at 
 the top and \\ feet at the bottom, and are about i foot deep. They run from the 
 
STOPING THE ORE. 63 
 
 bottom of the upper drift to the side of the lower, and protrude enough for the 
 car or bucket to be pushed under them. A sliding door at the bottom closes 
 them so that the contents will not fall out. If two drifts cross one above the other 
 a chute may be run from the bottom of one to the top of the other at the point of 
 crossing. The Upper Waterloo has an excellent double chute of this kind. It 
 runs from a track-drift which is the outlet of a great deal of pure carbonate of 
 lead to the main double-track drift running from the second level of the shaft. 
 At the place where they cross a broad chute is run from each side of the upper 
 drift into the top of the lower. As the drifts are close together the chutes are 
 short, but being very broad they hold a great deal. At the end of each chute 
 there are two doors, one over each track. One chute is used exclusively to re- 
 ceive ore, the other waste. It is often desirable to have a double chute where the 
 drifts do not cross, so that ore and waste may be sent down and yet never go into 
 the same receptacle. For this end a very broad chute is made with two doors at 
 the lower end, and a middle partition which runs nearly to the top. On this par- 
 tition a door is hinged which swings from one side to the other. Thus when one 
 side is in use the other side is closed. If the chute starts from the bottom of a 
 drift instead of the side, the door is hinged to the bottom along the middle line of 
 the chute. 
 
 WINZES. In the Evening Star the ore-bodies were so thick that the main 
 drift for conveying the ore to the shaft would be 20 and even 60 to 80 feet below 
 the contact. In such cases winzes are sunk from the upper workings to the 
 lower, down which the ore is thrown. To avoid accidents winzes are generally 
 made at the ends or sides of drifts. They are timbered with cribs just like shafts, 
 only the logs are lighter. They are tightly lined with planking running up and 
 down to prevent the rocks from destroying the timbers. 
 
 STOPING THE ORE. When new ground has been thoroughly developed the 
 ore, if in considerable quantity, is left standing in reserve until the management is 
 ready to take it out. In the mean time everything is prepared so that it may be 
 removed in the cheapest and most expeditious manner. They generally begin to 
 slope on the lower side of one or more blocks, and work upward along the con- 
 tact. The manner of sloping varies slightly according to the nature of the body. 
 If the ore is damp and soft, like the ores of the Forsaken and Old Waterloo, it is 
 picked down only. When the ore is badly mixed with waste, picking is also done 
 as much as possible. Where the ore is hard, or where it is quite solid but un- 
 mixed with waste, it is blasted out. The highly siliceous ores are the hardest to 
 stope, as they are very hard to drill and often break with a short fracture. The 
 thick bodies of granular carbonate of lead are also blasted down. In the Upper 
 Waterloo the holes were bored in this ore in a few minutes with long iron augers, 
 and a shot put in. The ore was thus brought down much faster than a man could 
 
64 EXTRACTING THE ORES. 
 
 pick it. The augers were used instead of drills, as the powder made by the drill 
 packed before it and made the progress very slow, while with the auger a i-inch 
 hole 2 feet in depth could be bored in a few minutes. As the ore is stoped it is 
 separated from the waste as much as possible and sent up to the bins, where it is 
 again sorted by daylight. As much of the waste as can be stowed is kept down 
 the mine; the rest is sent up and thrown on the dump. Anything fit for dressing 
 which has to be stoped is sent up for the third-class dump. 
 
 The method of putting in the slope-supports is very simple when the ore -body 
 is not exceedingly thick ; that is, when it is less than six or eight feet thick, as 
 are most of the bodies of the Morning Star mine. In such a body stulls are put 
 in for temporary support as the work progresses, and as soon as there is room 
 these are replaced by cribs for permanent support. The waste is stowed in these 
 cribs. Where the body is much thicker and stulls cannot be used, square sets or, 
 much more commonly, high cribs are put in at once. The way these are put in 
 has already been described. 
 
 ASSAYING THE ORJES. The variety of the ores, their differences in value, and 
 the fact that many of the products, though alike in all other respects, are some- 
 times ore and sometimes waste, have already been shown in the former chapters. 
 Unless the percentage of lead in the ore is very high, or the silver is visible in it 
 as the chloride, the most experienced miner cannot depend on looks alone to dis- 
 tinguish it from waste. The only trustworthy way of distinguishing the ores is 
 by assay. The importance of having frequent assays made to tell what is ore and 
 what is waste cannot be overestimated. The old Morning Star Company did not 
 pursue this course, and as a consequence passed by large quantities of ore, and, 
 worse than this, stowed away large quantities of it because it looked like waste, 
 when in reality it would at that time have paid them handsome profits. To keep 
 track of the ores each mine is furnished with an assay office, an assayer and his 
 assistant. Every "shift boss" is required to collect frequent samples from wher- 
 ever development is progressing and from wherever his men are stoping, so that 
 he may never miss any ore. If there is any doubt about the value of any material, 
 even when the quantity would not exceed a ton, an assay is made to decide upon 
 it. The superintendent and time-keeper also sample where they think necessary, 
 and to the latter officer belongs the duty of recording the samples and distributing 
 the returns of the assayer. The ore-sorters also send in doubtful samples to 
 assist them in sorting. Consequently there is little danger of passing over an 
 ore or of mixing it with much waste. By a few assays from one place the miner 
 can soon learn to tell ore from gangue at that place. 
 
 Each assay office has, on an average, from 40 to 50 of these assays a day. Of 
 course great accuracy is not required, as it is only desired to distinguish ore from 
 waste. One assay of each sample is made. Both the lead and silver are deter- 
 
SCALE OF PRICES. 65 
 
 mined. The lead assay is made first, and if the button shows over 10 per cent of 
 lead it is cupelled for the silver; if less than this, a scorification is made. Where 
 the per cent of lead is low there is no sulphur, and it is found that the lead collects 
 almost all the silver when there is not much of the latter metal present. There is 
 considerable loss only where there is a great deal of silver, and in such a case 
 enough can always be collected to show that the ore will pay. The best furnace 
 for these assays is the soft-coal furnace with two muffles, one above the other. 
 Such a furnace when hot will allow seven to nine crucibles to run in the upper 
 muffle, while twelve scorifiers run in the lower. The heat can be easily regulated, 
 and the same furnace is excellently adapted for control assays. 
 
 SELLING THE ORES. 
 
 The ores are not treated by the companies, but are sold to the various smel- 
 ters about Leadville and to Grant's smelting works at Denver. The Leadville 
 smelting works are situated along California and Big Evans Gulches, where 
 water for the engines and furnaces and an approach for the railway, as well as fine 
 positions for furnaces and ore- floors, are afforded. The ore is hauled from the 
 shaft-houses to these works in wagons. This is done by a contractor who agrees 
 to haul all the ore taken out at a certain rate per ton (from $0.70 to $1.00). The 
 two mines have a weigh-house, and all the ore shipped is weighed there as well as 
 at the smelters. 
 
 The ore is sold in lots of about 50 tons each. They seldom vary 5 tons from this 
 amount. Each lot is sampled at the smelting works, and the ore is sold on the 
 assay of this sample. When reduced to a final half-pint the sample is divided into 
 three portions and sealed up in bottles or paper sacks. One of these goes to the 
 mine assayer and one to the smelter. The third is kept for a referee in case of 
 dispute. Each assayer makes three scorification assays for silver and duplicate 
 assays for lead. On all ordinary lots running from 10 to 40 ounces the assayers should 
 agree within a half-ounce. Their lead assays should come within less than per 
 cent of each other. When the assays are satisfactory the mean between the two 
 returns is taken as the basis on which the ore is sold. 
 
 SCALE OF PRICES. It is highly desirable to the smelter to have ores rich in 
 lead to mix with those poor in that metal, and a scale of prices based on the 
 amount of lead in the ore is the result. Thus, if the ore contains very little lead 
 a very low price is usually paid per pound for it, and a high price is charged 
 for smelting. If, on the other hand, the ore contains much lead a higher price 
 per pound is paid for it, and a low charge is made for smelting it. The price 
 paid for silver is always six cents an ounce less than the market value, whatever 
 
66 EXTRACTING THE ORES. 
 
 the richness of the ore. The following is a copy of an ore contract. It shows the 
 form of the contract and the scale of prices. The italics occupy blank spaces in 
 the printed form and are filled in when the contract is made. 
 
 ORE CONTRACT. 
 
 THIS AGREEMENT, made this fifteenth day of July, 1882, between The Morning Star Consolidated Mining 
 
 Company, party of the first part, by W. S. WARD, General Manager, and 
 
 Smelting Co., party of the second part, WITNESSETH : 
 
 1st. That said Morning Star Consolidated Mining Company, by its General Manager aforesaid, in con- 
 sideration of payments hereafter mentioned, to be made by said second party to said first party, has agreed 
 and does hereby promise and agree to and with said second party to sell and deliver at the works of 
 said second party in Leadville, three fourths (}) of the output of said Morning Star Consolidated mine, tons 
 of ore from its mines, the delivery thereof to begin on the fifteenth day of August, 1882, and to continue 
 (unavoidable delays and accidents excepted) until the first day of February, 1883. And the amounts de- 
 livered each day (Sundays excepted) to approximate three fourths of the product of said mine for each day, it 
 being the intent hereof to sell and deliver to said second party only three fourths of product of said mine 
 during the time which will be required to produce and deliver the said ore hereby agreed to be sold to said 
 second party. 
 
 2d. In consideration of the foregoing, the said Smelting Co., party of the 
 
 second part, agree* to pay for the said ore, to the said first party, at the following rates : 
 
 For Silver, New York quotation at time of settlement, less six (6) cents per ounce. 
 
 FOR ORE CONTAINING: 
 
 Up to and including 20 per cent Lead 25 cents per unit,* less $16 per ton 
 
 Over 20 " " 25 " " 25 " " 15 " 
 
 " 25 " " 30 " " 30 " " 14 " 
 
 " 30 " " 35 " " SO " " 13 " 
 
 - 35 " " 40 " " 35 " " 12 " 
 
 " 40 " " 45 " " 40 " rt // " 
 
 " 45 " " 50 " " 40 " " 11 
 
 " 50 " " 55 " " 42 " " 10 " 
 
 " 55 " " 60 " " 45 " " 10 " 
 
 60 " " 65 " " 50 " " 10 " 
 
 " 65 " " .. " " 50 " " 9 " 
 
 All Gold over one half ounce per ton to be paid for at the rate of twenty dollars ($20.) per ounce for entire 
 gold contents. 
 
 All assays, whether Gold, Silver or Lead, to be reported to the tenth of the unit. 
 
 All expenses of hauling in excess seventy cents per ton to be paid by said party of the second part, and 
 all payments to be made in lawful money, upon request of said first party, whenever fifty tons or less shall 
 have been delivered, sampled and assayed. 
 
 AH ores shall be sampled and assayed without unnecessary delay, and in case of disagreement as to 
 values, as shown by the assays of the respective parties hereto, the umpire or third sample, shall be referred 
 
 to for assay, and his determination of the value from such sample shall be 
 
 final, and fix the value of said ores so sampled, which values so fixed shall thereupon be paid for said ores 
 by said second party to said first party, and the expense incurred for said umpire assay to be paid for by 
 losing party. Moisture determinations to be made incase of dispute on the water-bath. 
 
 It is understood and agreed that if for any reasonable cause the said first party should be unable to 
 produce the amount of ore herein contracted to be sold, then, as to such part not produced, this contract 
 shall be void. 
 
 Signed j 
 
 *The unit is one per cent of a ton; that is, 20 pounds. 
 
VALUE OF THE ORES. 
 
 6 7 
 
 Since February i, 1883, the following very advantageous terms have been 
 made by both mines with one of the smelting companies : For silver, 6 cents 
 an ounce less than the New York quotation at the time of settlement. For 
 lead, 45 cents per unit when the New York price is above 5 cents per pound, 
 40 per unit when it is between 4^ and 5 cents, and 35 cents per unit when it is 
 below 4^ cents per pound. From this value thus obtained the smelter deducts $9 
 a ton as a charge for treatment. 
 
 VALUE OF THE ORES. The ore-books, recording the ore-sales, do not state the 
 amounts of silver and lead in the ores, though they give all the data for obtaining 
 them. To obtain these, tedious calculations have to be made for each lot. To 
 give a general idea of the average richness of the ores of the two mines the follow- 
 ing table was prepared. It shows the number of net tons of ore shipped from 
 each mine, and the silver and lead in them, for each of the three months, August, 
 September and October, 1882 : 
 
 TABLE SHOWING PRODUCTION OF EVENING STAR. 
 
 
 Net Tons. 
 
 Oz. Ag. 
 
 Tons Lead. 
 
 Av. Oz. 
 per ton. 
 
 Per cent Pb. 
 per ton. 
 
 
 2,828.089 
 
 115,725.3 
 
 574.589 
 
 40.92 
 
 20.31 
 
 
 2 228. ^m 
 
 88 278.2 
 
 302.636 
 
 39.65 
 
 13.58 
 
 
 1,258.871 
 
 46,117.4 
 
 140.215 
 
 36.63 
 
 11.14 
 
 
 
 
 
 
 
 Total 
 
 5,315.475 
 
 250,120 9 
 
 1,017.440 
 
 
 
 
 
 
 
 
 
 TABLE SHOWING PRODUCTION OF MORNING STAR. 
 
 
 Net Tons. 
 
 Oz. Ag. 
 
 Tons Lead. 
 
 Av. Oz. 
 per ton. 
 
 Per cent Pb. 
 per ton. 
 
 
 1,749.029 
 
 43,014.0 
 
 678.848 
 
 24-53 
 
 38.8 
 
 September 
 
 1,070.921 
 
 23.753.4 
 
 473-057 
 
 22.27 
 
 44-2 
 
 
 1,975 006 
 
 52.238.0 
 
 691.968 
 
 26.45 
 
 35-o 
 
 
 
 
 
 
 
 Total 
 
 4,794.956 
 
 119,005.4 
 
 1,843.873 
 
 
 
 
 
 
 
 
 
 These tables show prominently the high average of the Morning Star ores in 
 lead. The Evening Star ores never averaged as high as the former in this metal, 
 but are lower in lead for the three months given than they were before the large 
 body was stoped. The fact that the Evening Star ores are much richer in silver 
 than those of the Morning Star is also prominently brought out. The variations in 
 value of the various lots is, comparatively speaking, small. Thus in the Morning 
 Star sales for the three months only 8 lots out of the 98 went over 40 ounces per 
 ton, and the highest was 46 ounces. The lowest ran 8 ounces, with 4 lots below 
 10 ounces. 
 
 In lead the variation was great, the limits being 65 per cent on the one hand 
 
68 EXTRACTING THE ORES. 
 
 and 14^ percent on the other. There were 16 lots below 25 per cent, 18 lots above 
 50, and 6 above 60 per cent. 
 
 The Evening Star shows no greater variations. From the 125 lots sold, 8 went 
 over 60 ounces, with a maximum of 75 ounces. But 3 lots ran below 25 ounces, 
 and the lowest was 23^ ounces. The lead was always very low; only 13 lots 
 assayed over 25 per cent, and the highest was but 31^. Of the 17 lots which ran 
 below 10 per cent lead, 13 were sold during the month of October. The exceed- 
 ingly low minimum was 6 per cent, the lowest of any shipment of either mine 
 noticed on the books. 
 
 In order to show the expenses of mining and the items of greatest expense, the 
 following table, showing the expenditures of the Evening Star mine up to Oct. i, 
 1882, is given. The total represents the amount received from the smelter for the 
 ores. The value of the silver and lead produced by the mine would, of course, be 
 far greater. 
 
 TABLE. 
 
 Cash on hand $4,82409 
 
 Labor 386,059 01 
 
 Improvement 20,844 85 
 
 Machinery 17,268 53 
 
 Iron, steel, etc 33,603 81 
 
 General supplies and expenses 4,049 18 
 
 General transportation 272 86 
 
 Assaying materials 3,324 48 
 
 Horse feed 3,957 09 
 
 Legal service and surveys 3,293 99 
 
 Office expenses 1,568 18 
 
 Ore transportation 42, 333 1 1 
 
 Timber 41,998 29 
 
 Fuel 12,434 18 
 
 Insurance 479 15 
 
 Telegraph and telephone 723 97 
 
 Leadville Water Co 1,894 25 
 
 Tax 47762 
 
 New York office as net earnings 1,410,592 20 
 
 Total received from sale of ores $1,989,998 84 
 
 THE END. 
 
PL. I 
 
 SECTION 1. 
 
 White 
 Porphyry 
 
 Gray 
 Porpliyry 
 
 GraiuJar 
 Lead ( ' : i rl>< 1 1 1 ; 1 1 1 
 
 Basic Iron. 
 Sulphate 
 
 Jxaru. Ore 
 
 Blue 
 Limestone 
 
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Pl.V. 
 
 Fig. 2 
 
 Fig. 3. 
 
PI. VI. 
 
 Fig.l. 
 
 Ffq.2. 
 
 Fig.3, 
 
 Fig. 4. 
 
 Scale: 1+