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The Infamous Black Bird Southern Oregon History, Revised


Southern Oregon Gold Mines

Methods of Mining circa 1855, James Mason Hutchings
Methods of Mining circa 1855, by James Mason Hutchings.

JACKSON COUNTY
    I am indebted for much valuable information concerning this county to Mr. Silas J. Day, of Jacksonville, whose character and long acquaintance with the neighborhood give ground for confidence in the correctness of his statements, many of which are also confirmed by my personal observation.
    The population of the county is about six thousand six hundred, of whom six hundred are Chinese, principally engaged in mining. The number of white miners, according to the books of the county assessor, is five hundred. The latter receive, when hired, from $2.50 to $3 coin per day. The wages of a Chinese laborer are $1.25 to $1.50 per day, or $35 per month.
    The following is a brief account of the principal mining districts in the county:
    Jacksonville district, including both forks of Jackson Creek and its tributaries, was organized in 1851. The mines hitherto worked have been placers, with some coarse gold.
    Applegate Creek, ten miles in a southerly direction from Jacksonville, is a considerable stream, on which a sawmill has been erected. It is a tributary of Rogue River. The district of this name was organized in 1853. The mining operations on Applegate Creek have been quite extensive. The gold is found mainly on the “bars” of the creek, which for a distance of four miles were very rich. They are now principally worked by Chinese. Water is obtained from a large ditch brought from the creek four miles above the bars, and now owned by Kaspar Kubli.
    Sterlingville district, about eight miles due south from Jacksonville, was organized in 1851. This has been, and is still, a thriving mining camp. The gold in the placers is coarse. The supply of water, however, is limited, as there is no ditch in the district which taps any considerable stream.
    Bunkum district, on the other hand, a southern extension of Sterlingville district, has an abundant supply of water during most of the year, brought in three ditches from the North Fork of Applegate Creek.
    Foots Creek district was organized in 1853. The stream from which it takes its name is a tributary of Rogue River, situated about fifteen miles northwest from Jacksonville. The mines are coarse gold diggings.
    Evans Creek and Pleasant Creek districts are contiguous to each other, about ten miles north of Foots Creek. The coarse gold diggings of these districts are worked principally by the hydraulic process, for which the necessary supply of water is furnished by the streams named in abundance during the rainy season. Both these districts were organized in 1856.
    Forty-Nine Diggings, eight miles southeast from Jacksonville; organized in 1858. The gold is inferior in quality, and worth only about $12 per ounce. Water is supplied by a ditch from Anderson and Wagner creeks.
    The mining laws of all these districts are copied from those of Yreka, in California. The tax on foreign miners (by which only the Chinese are understood) is $10 annually per capita. There is also an annual poll tax of $5 on all mulattoes, Chinamen, and negroes.
    The first discovery of gold in Jackson County is said to have been made in the autumn of 1852, by James Clugage, on Rich Gulch, a tributary of Jackson Creek. Both in the gulch and in the creek large nuggets were, in the earlier days of the mining industry of this neighborhood, frequently found. One piece of solid gold, worth $900, was taken from the latter stream, and many were obtained ranging in value from $10 to $40, and up to $100. These discoveries led to the development of a considerable mining industry, in which, however, no great amount of capital was invested. The claims in the county are, with the exception of the bars and a few quartz claims, mentioned below, generally placer and gravel diggings. The heavy wash gravel ranges from two to twelve and even twenty feet in thickness, and contains a large amount of stones, and even rocks of considerable size. This is especially the case on Jackson Creek. The bedrock is slate or granite--the former predominating. Water is supplied principally by the rains of the wet season, which swell the local streams. There are few mining ditches in the county, and none of great magnitude, the length being generally from one to four miles, and in no case exceeding the latter figure. The mines are therefore directly dependent upon the duration of the season of rains. This lasts usually from December 15 to June 1. The mining season for the year ending June 30, 1869, was, however, here, as elsewhere, a very short one, owing to the extreme dryness of the winter. The season opened about the 10th of January, and was over by the middle of May. When I visited the county, early in August, nothing was doing except by some of the Chinese, who were painfully overhauling the dirt heaps and carrying the earth to water. The average annual product of Jackson County in gold dust for the last five years has been, according to good authority, $210,000. I estimate the product for the year ending June 30, 1868, in spite of the brevity of the season, at $200,000, since the patient labor of the Chinese, of whom there are a considerable number working for themselves, has made up the deficiency of the season. They have produced not less than $75,000 during the year referred to. The product for the calendar year 1868 is practically the same as I have given, since the period of active operations fell wholly within 1869.
    Some very rich quartz ledges have been discovered in this county, and I do not doubt that this, like so many other placer-mining regions, will eventually become the scene of extended deep-mining operations. No quartz veins, however, so far as I could learn, have been worked in Jackson County with capital, perseverance, and judgment adequate to fully prove their values, though in several instances large profits have been realized from operations near the surface.
    One of these instances is presented by the celebrated Gold Hill vein, situated ten miles northwest of Jacksonville, and discovered in January 1859. The ore is white, almost transparent quartz, and, in the pocket first exposed, was highly charged with free gold. Some rock taken from the ledge was so knit together with threads and masses of gold that when broken the pieces would not separate. The vein was worked rudely for a year, and the ore crushed principally in an arrastra. The sum of $400,000 was thus extracted, besides a large amount of extremely valuable specimens, one of which was presented by Maury and Davis, merchants of Jacksonville, to the Washington Monument, and now, I am informed, occupies a place in that structure. But the pocket became exhausted; subsequent operations failed to find paying rock, and the work has been suspended for some years. The property is now owned by a few shareholders, who intend to resume mining at some future time.
    The Fowler lode, at Steamboat City, twenty miles from Jacksonville, is also at present lying idle. This ledge was very rich near the surface, where the rock was considerably disintegrated. The contents of a rich chimney or pocket were extracted, and crushed in arrastras run with horse power. Major J. T. Glenn, one of the owners, says $350,000 were taken out.
    Arrastras were erected at a ledge on Thompson Creek, a tributary of Applegate, to work the ore extracted, but the rock did not pay, and it was finally abandoned. The Shively ledge, on a tributary of Jackson Creek, has had a similar history.
    At present there is but one quartz vein worked in the county. It is being developed by a few men as a prospecting scheme. They carry the quartz about a mile, to the Occidental mill, where they have already had about 100 tons treated, realizing about $1,000, or $10 per ton.
    There are three quartz mills in the county, all driven by steam. The Jewett mill, on the south side of Rogue River, was erected sir years ago in connection with a ledge of the same name. It had eight stamps, and 32 horsepower. The investment was not profitable, professedly because the gold was too fine to be saved, and the mill is now a steam sawmill. A mill similar to the foregoing was put up seven years ago at the forks of Jackson Creek. It cost $8,000, and was intended for custom work, but did not pay, and is now owned by Hopkins & Co. as a sawmill.
    The Occidental mill, on the right fork of Jackson Creek, was built four years ago by a company at a cost of $10,000. It has ten stamps, and 40 horsepower, was made at the Miner’s foundry, San Francisco, and has a daily crushing capacity of 20 tons. The machinery includes two rotary pans.
    The cost of mining materials in this county is not excessive. Lumber is worth at the mill from $18 to $22.50 per thousand feet, according to quality; quicksilver, $1 per pound; blasting powder, 33 cents per pound. Freight is generally shipped from San Francisco to Crescent City, California, and hauled from there in wagons to Jacksonville, at a total expense, including commissions, insurance, etc., of about 5 cents per pound. This enhances the cost of machinery and of some supplies. As a general rule, Jackson County receives no freight overland from Portland or Sacramento.
    There are several good salt springs in the county. One at the headwaters of Evans Creek has been worked with profit for several years past by Messrs. Brown and Fuller. The salt is said to be white and pure, and commands a good price in the local market. Two beds of mineral coal have been discovered in the county. One on Evans Creek, about ten miles from the salt- works, produces a superior coal, which is used by the blacksmiths of the county. It is comparatively free from shale, and is locally known as anthracite. The bed is owned by Mr. R. H. Dunlap, of Ashland. Large quantities of iron ore occur in many places throughout the county, on the surface of the ground. Some specimens from Big Bar, on Rogue River, were analyzed in San Francisco, and found to be quite pure. Cinnabar is reported, but not in paying quantity, from Missouri Gulch, a tributary of Jackson Creek.
Statistics of Mines and Mining in the States and Territories West of the Rocky Mountains, 1870, page 214


QUARTZ MINING IN SOUTHERN OREGON.
AN INTERESTING REVIEW--ACTIVE PROSPECTING
AND NEW DISCOVERIES IN MANY QUARTERS.
    Gold-bearing quartz exists in very many localities in Jackson, Josephine and Douglas counties, and the two former have been the scene of considerable mining operations within the last twenty-five years. The first quartz discoveries in Oregon took place in 1859 upon Jackson Creek, when a deposit containing one or two thousand dollars' worth of the precious metal was unearthed by two brothers named Hicks. In the latter part of the same year very rich quartz was found on Gold Hill, close by Table Rock, in the Rogue River Valley, and $150,000 was taken out. This mine as well as the first named, and in fact all those of which we have to speak, was of the sort called a "pocket" lead, where all the gold was found in a very small space in or on the vein, the rest of the quartz being barren or very nearly so. This, the great characteristic of mines of this class, was not recognized at the time of these discoveries, nor has it been fully understood or appreciated yet. This mine, the Gold Hill claim, was owned at first by its discoverer, Graham, with Tom Chavner, John Long, George Ish and James Hayes. Henry Klippel and Col. John Ross afterwards bought in. A large part of the find consisted of "float" (loose pieces of rock), which were in a cavity right over the ledge, or had rolled down a dry gulch. Hundreds of people prospected here immediately, and nearly the whole population gave up every occupation except that of watching the fortunate locators as they picked up choice chunks of quartz with gold visible all through it. Two arrastras were at once put up, and their output amounted for a while to 1,000 ounces of retorted gold each week. Dissatisfied with this, a mill was projected, but it proved unsuccessful, as the pocket was nearly exhausted before the stamps began to drop. The total amount of gold taken out was about $150,000, which was all contained in a portion of the vein twenty feet long, ten feet deep and two feet thick. Hence it was a true pocket vein. All the remaining portion of the lead has been found to be barren. However, it has not been thoroughly prospected as yet in all its accessible parts. Work on it ceased long since.
    Great as was the yield of the Gold Hill vein, it was thrown in the shade by the product of the Fowler mine on Steamboat Creek, a tributary of the Applegate. This vein lies near the California line. Its gold is found disseminated through a larger proportion of rock, but it still possesses the essential character of a pocket vein, although it has been worked as a milling lead. This claim was owned by W. W. Fowler, G. W. Keeler and some others, and was worked for over three years, the rock being put through arrastras. The yield per ton was as high as $2,000, and 1,400 ounces were taken out in a single week. The whole yield is thought to have been over $300,000, which makes this the most productive pocket mine on record, as far as is known.
    In the vicinity of Gold Hill several quartz claims have been worked with success. The principal of these were the Blackwell, the Swinden, the McDonough and the Schumpf veins. On Jackson Creek, very close to the town of Jacksonville, the Holman, the Davenport and other claims were worked, mostly in 1860, the time of the chief excitement in quartz. The Jewett mine, across the Rogue River from Grants Pass, was also worked in the same year and paid many thousand dollars. The above includes the greater number of successful quartz claims in Jackson County, and it has to be observed that the greater part of the work was done upon them in 1860. Subsequent developments have affected little.
    Down in Josephine County some gold quartz has been found. The Enterprise mine on Althouse Creek was worked with profit for several years, the rock yielding about $25 per ton. In 1875 the so-called Oregon Milling Company got possession of the ledge and built a mill at Browntown, near Althouse, but failed to make money. Several quartz ledges lie nearby, none of them having been worked to any extent. In the northern part of Josephine County, near the railroad line, lie several well-known quartz claims, some of them esteemed of value. The Lucky Queen is one of them, but it has thus far belied its name. It is situated on Jump-off Joe Creek, and has been extensively prospected, with great promises of richness. It has a mill of ten stamps. Upon this mine and the Esther, or Browning claim, on Grave Creek, has been done more work than has been put on any other quartz claim in southern Oregon since the exhaustion of the Fowler lead in 1864.
    In various other localities in Jackson and Josephine counties auriferous quartz has been found, notably on Galice Creek, Williams Creek, Foots Creek, Evans Creek, etc. There have been "rushes" to various points, notably to Galice Creek in 1874, where several hundred locations were made on some big ledges 200 or more feet wide. The real history of quartz mining, however, is confined to the years 1860 and 1863, during which time all the most important discoveries were made, and particularly the first-named year. The total gold product of southern Oregon, as far as can be ascertained, includes about $700,000, which was derived from quartz mines, and of this not less than 95 percent has been taken from pocket veins.
    The chief grounds for expecting other and even more extensive developments of auriferous quartz lie in the fact that at least two-thirds of the above sum was taken out of the mines in one year, since which the art of quartz mining has been suffered to languish with only an occasional small discovery to keep it from falling into oblivion. It is not possible that the extensive region could have been entirely exhausted of its mineral wealth in so short a time, and by so unskilled a generation of miners as inhabited it. Quartz mining was then a new and almost untried art, and the resources for this sort of mining were small and precarious. Pocket mining has in some sections become an art by itself, demanding knowledge, skill and care for its proper direction, and when associated with these its pursuit becomes successful in a high degree. The principles of that art are simple. They consist in following the quartz vein to its intersection by a "dike," or other interrupting cause, where generally a deposit of gold is found. So simple is the process, yet made wonderfully complex by the recurrence of numerous "elbows," "faults," "horses" and other recurring causes, that its pursuit requires profound study and attention. Whole communities in California are made up mainly of pocket miners, whose aggregate income forms a large part of the whole gold product of the state.
    All the foregoing is apropos of the fact that prospecting is rife in portions of southern Oregon. Several promising discoveries have been made, the most important being that on the McDonough pocket vein, where several thousand dollars in gold was taken out scarcely a week since, if we may believe newspaper accounts. Even larger discoveries are highly possible, and if prospecting be followed by determined efforts to develop--that is, to examine--the leads, the most flattering results are probable. There is a very large tract of country which deserves to be examined for valuable metals of various sorts, but if the present writer's judgment be not astray, the eastern part of Douglas County presents as good a field as any section of the country for the prospector's craft. Whoever is interested sufficiently in the matter of prospecting is invited to communicate by letter with "Assayer," care of the Oregonian office, whereby information of importance may be obtained.
Democratic Times, Jacksonville, May 29, 1885, page 1


POCKET HUNTING.
HOW PROSPECTORS FOLLOW UP THE INDICATIONS.
    An interesting description of pocket-hunting methods is given in condensed form by a writer in the Grass Valley, Calif. Telegraph. He says: "The usual equipment for active service consists of a pick, shovel and mining pan, with a powerful glass for inspecting the 'colors' of gold. Pocket hunters, as a rule, have their favorite localities and guard them as zealously as a miner would his location. When in search of a 'new find' the expert pocket hunter begins his operations in the small ravines or canyons leading from known veins on the ridges or higher elevations. A pan of dirt is taken from the ravine, carefully washed and panned out, and if no 'colors' are visible the process is repeated at different points and ravines until a prospect is secured.
    "The prospects usually consist of a few colors, which are very carefully examined by the aid of the lens to see whether the gold has an angular appearance, or whether it is smooth, the former being an evidence of its proximity and the latter showing that it has been carried some distance and worn smooth. This system is followed by careful panning, and the point where the gold entered the vein is accurately located. Then its course is followed up the hillside until a vein of quartz is intersected. So expert have these miners become that they have been known to follow the disintegrated particles of the vein in which the pocket exists, and from which small pieces of gold have been strewn in its path to the ravines or gulches below, across several veins that are barren, and finally to the pocket.
    "Invariably the pocket is located by an iron seam in the vein, which is anxiously looked for by the prospector, who proceeds forthwith to dig it out. Absolute certainty seems to be the result of the system used, as they have been known to mark the place carefully and return next day and extract the gold, never failing to get a pocket of more or less value. The presence of iron seems to be a necessity, as it is claimed that no pocket of any consequence has yet been found without its iron seam.
Democratic Times, Jacksonville, March 15, 1894, page 2


GOOD YEAR IN MINING
Jackson County Made Gratifying Progress.
WORK OF SUBSTANTIAL ORDER
Placers Have Held Foremost Place in Gold Output--
Comprehensive Description of District and Its Several Properties.

    ASHLAND, Or., Dec. 27.--Precious metal mining in Jackson County for the year 1900 exhibits gratifying progress, and is of a more substantial character than in any former epoch since gold was first mined in the region. It is not so much involved in perplexity and doubt. Extensive development of a few of the quartz properties with profitable returns and proof of continuity of the veins, with persistence of metalliferous matter carrying good values at the considerable depths attained, has cleared away a mass of misconceptions and errors which has seriously impeded the industry in Southern Oregon during a number of years. There are pocket ledges, so-called, and pocket mining is still carried on to some extent and with profit, but it can no longer be said there are no workable ledges conforming to the requirements of "milling leads." There is in operation close to Ashland one of the deep mines of the state, and there are several within the county whose underground workings are quite extensive with development of ore bodies which maintain them as dividend-payers. In no former year has there been so much work done on ledge prospects and on veins of proven value, and this has been  attended with such results that quartz mining has attained an unquestioned position as a permanent and leading industry of the county. Another feature of advantage to the mining interest is that less money and less effort, relatively speaking, are thrown away on capricious notions of the occurrences of precious metal deposits and hopeless undertakings than in previous years. Work has commonly been done on lodes affording some promise, and with intelligent direction. This is perhaps to be expected in the progress of quartz mining, for each year there are more trained minds and experienced hands, and fewer novices in the working of mines; hence waste work and disappointments are more infrequent and a mining district is more likely to prosper or be abandoned on its own merits.
    The placer mines have held the foremost place as to gold output, but the product of the quartz mines will likely soon be equal (it is nearly so now), if it does not exceed that of the placers. The working of the sands and shallow bars of the streams is small, and the placers of importance comprise the hydraulic diggings, where water is conducted by miles of expensive ditches and flumes to operate giants to tear down huge beds of Neocene gravels and conglomerates, some of which, as the Sterling, are highly auriferous and pay well. The pick-and-shovel miners of early days have nearly disappeared from the creeks, though there are a few who do fairly well in a good season, and the aggregate of their product throughout the county annually amounts to a considerable sum of money. If permitted to class the pocket-hunters with them, their produce exceeds in value that of some of the important farm products of the county. Having pointed out the sources of the gold, the mining man would doubtless desire a description of the country in a general way, to be made acquainted with the character of the rock masses, and some information in detail as to the principal mines and the mineral products.
    South of Ashland are Ashland Butte and its near neighbor, Mount Wagner, two very conspicuous topographic features of the Siskiyou Range or Klamath Mountains. They are some seven miles distant, and the former attains a height of 7662 feet. The trend of the range approximates an east-and-west line, and, except in the vicinity of Ashland, the crest line is mostly in California. It is flanked by spurs of such magnitude in some instances as to make a distinct range, like that north of Mount Wagner, which separates the valleys of Bear Creek and the Applegate. East of Ashland is the Cascade Range, with a northerly and westward trend, which forms the eastern barricade of Bear Creek Valley. From the western slope of this latter range and from the north side of the Siskiyous, the waters are gathered by a series of mountain streams, which are perennial, and conducted to Rogue River. On the south side of the Siskiyous the waters fall into the Klamath River; these are the trunk streams of the region. While the trend of the uplifts are well defined, denudation has been marvelously effective in land sculpture, and the country is essentially mountainous and hilly, with several fine plateaus and rich valleys, relatively small; of the latter the Rogue River or Bear Creek Valley is the largest, and comprises one of the richest agricultural and horticultural areas in Oregon.
    The mountain region, the locality of most of the mines, is attractive and enjoyable to a degree not exceeded, perhaps, in any other section of the West. The forests are magnificent, comprising the best types of the coniferous trees of commercial value, and a variety of smaller growths, inclusive of some vines and plants of particular interest and value. The areas near the summits are often beautiful in their alternation of glade and grove. Groupings of fir and pine, or of fir and hemlock, at the higher altitudes, are often ideal and park-like, and the opens--where there have been no sheep--are bright with beautiful flowers and grasses. The country is bountifully watered, and on the plateau summits there are numerous ice-cold springs of sweet water whose source is probably Shasta, which is generally in grand and majestic view from these points on the Siskiyous, and seemingly only a few miles away.
    The Siskiyous, or Klamath Mountains, comprise extensive areas of the older rocks, in which the auriferous veins commonly occur, and are to certain extent regarded as an extension of the Sierra Nevadas. They merge into the Coast Range westward, with their Cretaceous and Tertiary formations, and are flanked on the north side by these latter formations, which cover much of the area of the county, though there are patches of the older rocks exposed in numerous places. In these patches one is likely to find mines, but they are not confined exclusively to the older formations. Metamorphism is a noticeable feature of rock history, as one goes south and west of Ashland, particularly in the Wagner Butte region. There is a good mining district there, as might be supposed. Further westward is a serpentine belt, covering a large area: the bedrock of the streams being commonly slate, which appears to underlie the serpentine. The mountain mass projecting northward and westward from Wagner Butte is mainly slate, in which there are a few encouraging prospects, but no mine of proven value. In the serpentine belt mentioned there are patches of eruptives or igneous rocks, such as diabuses and bivrites, in which prospects have been found of copper ores carrying some silver and gold values. In this region, too, the prospects of cinnabar appear to be of considerable importance, and on one claim there is extensive development work. There are some huge masses of talc, asbestos is common, and varieties of schists are well represented in places. Immediately to the south and west of Ashland the rock masses are mainly granite and cranodiorite. The Ashland mine is in this formation near town, and there are numerous neighboring prospects, some of which are being extensively developed. Relating to certain specified localities close to Ashland, I quote Professor Diller, a distinguished member of the United States Geological Survey, whose pen has rendered Oregon some valuable services:
    "At Ashland the Cascade Range is separated on the southwest from Siskiyou Mountain, a part of the Klamath group, by Bear Creek Valley, a branch of Rogue River Valley. The topographic features just referred to are composed of four sets of rocks: (1) pre-Cretaceous sedimentary and igneous rocks, (2) Cretaceous conglomerates, sandstones and shales; (3) Miocene conglomerates, sandstones and shales; (4) Miocene and later lavas. Among the pre-Cretaceous rocks of the Ashland region quartz-mica-diorite is one of the most important. It extends from Ashland southward into Siskiyou Mountain. It is the base upon which the Cretaceous strata lie and from which the sands and silts of both the Cretaceous and the Miocene strata were derived. The Cretaceous strata occupy the middle portion of the Bear Creek Valley, and much of the lower slope upon the southwest side . . . and dip eastward beneath the Cascade Range, in all probability connecting with similar rocks of the same age exposed on Crooked River, in Eastern Oregon. The Miocene beds are exposed upon the lower slope of the Cascade Range a short distance northeast of Bear Creek. Although not accurately measured, they must have a thickness of over 500 feet. The Miocene sandstones, like those of the Cretaceous, . . . were derived directly from the disintegration of the adjacent diorite, which formed the shore of the water body originating them. The conglomerate, of which a heavy bed occurs near the base of the Miocene, is made up largely of fragments of older igneous rocks from the Klamath Mountains, and differs from those of the Cascade Range. Mixed with these in the conglomerate, but more particularly in the overlying sandstones, are pebbles of quartz, quartzite, schist, and slate, from among the older rocks of the Klamath Mountains."
    Some of these conglomerates and gravels are auriferous, and a tract north of Ashland has been prospected some. The old Davenport placers were doubtless enriched from them. The Sterling mine is probably in the same formation. Again, Professor Diller says: "The older portion of the Miocene strata contains no trace of the modern volcanic rocks of which the Cascade Range is composed. They dip gently eastward beneath the sheets of lava composing the range." From this and other evidences mentioned he concludes that the Miocene strata of the Ashland district are older than the adjacent portion of the Cascade Range, and that the earliest eruptions in this part of that range took place in a later portion of the Miocene or Pliocene. He further states that the Cascade Range is not underlain by a parallel ridge of pre-Cretaceous rocks. These points are cited as they have an important bearing on the mining geology of the region. In some features they are interesting, too, in relation to the project, said to be afoot, to bore for oil in Bear Creek Valley. Assuming that the animal and vegetables deposits laid down in these Cretaceous and tertiary strata formed carbonaceous shale or other rock rich in hydrocarbons, then the heat produced in the rocks attending the movements and uplifts which created the Cascades and the subsequent disturbances, may be supposed to have been sufficient to have made petroleum from these hydrocarbons. In this connection I may state that some asphaltum has been found in the region, the locality being named of the samples I have examined, which I have no reason to doubt. As asphaltum is a product resulting from the oxidation of the hydrocarbon of petroleum oils, the value of this evidence is manifest, and the oil-boring project is not without a rational basis.
    The Ashland mine whose location has been noticed above is the most important of the quartz properties that is being worked in the county. The underground workings comprise about 6000 feet of shafts, tunnels, drifting, etc. The main shaft is now rapidly approaching the 700-foot level, and it is therefore the deepest mine in Southern Oregon. A 1400-foot tunnel, driven into the north side of the mountain spur which carries the ledge, connects with the shaft at the 250-foot level, which facilitates the ventilation of the mine, and through it the water is carried out. Drifting at the 500-foot and 600-foot levels on both sides of the shaft in fine ore is in progress. The blocking out and exploratory work furnishes all the ore that can be handled with the present milling facilities. This mine has improved greatly with depth, and is a very important factor in supporting confidence in the mining district. At the 600-foot level the vein is "filled," as the miners term it; that is to say, there is ore from wall to wall, a width of seven to eight feet, and so continues. The proportion of free gold in these lower levels is large, and it is an excellent type of a good free-milling lode. Pyrites of iron are practically the only sulphides carried in the ledge. An average of two cars per month of high-grade base ore are shipped to the Tacoma smelter. The concentrates from the mill run in amount from two to five percent, and will perhaps average $45 to $250 per ton. This is known to be correct, as to ores from the upper levels. About 40 men are employed on the mine. Most of the gold product of the Ashland district for the current year came out of this mine. The Shorty-Hope, a neighboring mine which has a 10-stamp mill, is not now in operation. Much work has been done on supposed extensions of the Ashland, but there have been no important discoveries on the lead outside the limits of the Ashland corporation's property.
    The Free Silver, or Barron mine, nine miles southeast of Ashland, on the southwestern slope of the Cascades, has had considerable development, showing a large amount of good ore, and is held to be a very valuable property. A description of this mine has heretofore appeared in The Oregonian. The complex character of the ores will likely require a smelter to save the values, though there is free gold at the greatest depth attained, which is a little over 200 feet. There appears to have been much crushing of the rock material in the vein, which does not seem so well defined as the veins in the Siskiyous. At the 200-foot level it is seven to 12 feet wide. The mineralogy of this mine is more interesting than that of any other known in Southern Oregon. Among the minerals carried in the vein are pyrite, chalcopyrite, galena, native silver, red silver ore, or ruby silver, native gold, sphalerite, and realgar. There is much silver. In the milling tests the concentrates gave $157 gold and 900 ounces silver per ton. The silver in the gold reduces the bullion value to $13 to $14. The Ashland's gold is worth about $15.50, due to the presence of silver, or has been, whereas the placer gold of the county generally will run from $17 to $19.50. Local dealers usually allow $16 per ounce. The Free Silver is the only mine of established value known in the extreme southern section of the Cascades. There are said to be some good prospects up Elk Creek, and numerous locations have been made, but no important properties have been developed.
    The development work on a number of the prospects in the Ashland district is considerable and as a whole encouraging. There have been no sensational "strikes," but there appear to be at least two of the recent discoveries of substantial value to the owners and highly advantageous to the district.
    The mining districts of which Jacksonville and Gold Hill are the commercial centers, though Medford may also be named in the former, are old and have often been described in this and other papers. To the mining man it may be said the metamorphic rocks, such as slates, schists and miners' "porphyries," are well represented in the geologic formations. A peculiar base of granite is a noticeable feature of the Gold Hill rock masses. Both districts are thrifty, and their gold product this year is in excess of that for a number of years past. Explorations in quartz are in progress near Jacksonville, and at several points up the Big Applegate and along its affluents, embracing a large territory of auriferous country. Some of these are yielding money, but no large mines have been developed yet. The placers of the region hold the first place, as heretofore. The Sterling is a large, well-equipped and very productive mine, and holds a place as one of the big placer properties of the Coast. The placer properties generally have been much improved this year, and with their better equipment and promising water supply, will clean off more bedrock this season than in any previous season for years past. About Gold Hill the activities in quartz mining are greater than at any previous period in years, making the camp a prosperous one. There have been some important and very valuable discoveries, notably the Nye ledge, and the gold product inclusive of that of the neighboring placers is greater than that of any year since the bonanza days. In this district Foots Creek, Galls Creek, Sardine Creek and Evans Creek are the important localities of mining operations, both in quartz and placers.
    The writer has been at some pains to collect data by which he could arrive at a fairly close estimate of the gold product of Jackson County for the year 1900. In this work he has been courteously aided by the banks of Medford and Ashland and by a number of mining men. The statements received are for the most part confidential for manifest reasons. The banks of Medford have handled the most gold among the local banks. Some of the mines, like the Ashland, do not dispose of their bullion product through the local banks. The following are the figures obtained, which are submitted as
conservative and a very close approximation of the actual yield of all the mines in the county: Ashland district, $95,000; Gold Hill, $104,000; all districts tributary to Medford and Jacksonville, $155,000; total, $354,000.
    In the Ashland district the product is mostly from quartz. In the Gold Hill district about $55,000 is from quartz mines. Comparing the different sections of the mining areas Gold Hill makes the best showing as to increased product. The Ashland and Gold Hill districts are in a position to greatly increase the output during the next year, as there are several properties just reaching a position to become producers, and I think this will be true, too, of the country in the neighborhood of Jacksonville.
M. F. EGGLESTON.               
Morning Oregonian, Portland, January 2, 1901, page 11


SOUTHERN OREGON MINES.
Gravel Deposits 5 to 50 Feet Deep and Quartz of Great Value.
    A few miles south from Cottage Grove the summit of the Calapooia Range, the line between Lane and Douglas counties and demarcation of Central-Western and Southern Oregon mining sections, is reached. No organized mining districts are known, and localities must be designated by reference to supply points for each as they are found on the line of the railway.
    Roseburg, county seat of Douglas, is situated among, the rolling hills which characterize the greater part of the county, distant south from Portland 198 miles. Here is the United States Local Land Office of Roseburg land district. A portion of Bohemia district laps over the Calapooias into this country, but with this exception but little mining business is done in the northern portion of the county. No mines of importance are tributary to Roseburg.
    Riddles, a growing town on the line of the railroad, 26 miles south of Roseburg, is a point of considerable importance as a supply point for neighboring mines, particularly the placers lying to the east, on Coffee Creek and its tributaries. On Cow, Ash and Bollenbaugh creeks the farmers engage in washing gold out of their lands during the rainy days of winter. For nine months of each year they cultivate their land and for three months they work at the edges for the "gold there is in them." And it is said to be a very profitable business. On Cow Creek, 15 miles from Riddles, several placers, one having a gravel bed 50 feet deep, are being operated by hydraulics under 100-foot head with excellent results.
    Three miles west from Riddles is a group of claims producing nickel. They occur in a range or mountain locally known as "Old Piney," having an altitude of 3500 feet. The formation is an eruptive magnesian rock technically known as saxonite. A series of veins intersect this mass, which covers an area exceeding 1200 acres. Since the formation of the ore veins a subsequent movement has tilted them from their original position and they now lie at a dip of about 20 degrees from horizontal. Apparently the hanging wall has been eroded, leaving great ore bodies exposed as a blanket. The ores are in form of a silicate of nickel and magnesia, averaging about 4½ percent, and the veins vary from 18 inches to 80 feet in width, the gangue being silica in various forms. Cretaceous sandstones, altered slates and serpentine comprise the general structure of the county.
    East of Riddles 35 miles, on the head of Elk Creek, the Rainbow Company has five claims on copper- and gold-bearing veins, of eight, five and 30 feet respectively; the ores going about 10 percent of metal. Elevation, 3500 feet; formation, anderesite, feldsite and schists. Numerous other claims are being developed in that neighborhood.
    Glendale, south from Riddles 35 miles by rail, is near the southern line of Douglas County, which follows the summit of the transverse range of the Rogue River Mountains. The mines tributary to Leland consist chiefly of placers. On Tennessee Gulch, 12 miles northeast, are about a dozen placers, one well equipped, the others on a small scale. On Ball Run, a tributary of Quines Creek, are several, getting coarse gold. Eight miles farther up in the mountains, and on Hogem and Starveout, are numerous others; three hydraulics on Hogem. On Stewart are two fairly extensive hydraulic mines. Six miles farther up, on White Horse Creek, is another group, and 10 miles still farther, cinnabar float has been found on the hillsides and in stream beds. The veins which threw off the float have not been found.
    On Quines Creek, 12 miles northeast from Glendale, is the old Union quartz mine, recently taken over by a California company. The veins lie in contact run parallel, carry free gold and pyrites; formation, diabase and serpentine; elevation, 2500 feet
    On the headwaters of Stewart Creek and above the placers on that stream, is a group of quartz claims known as the Green Mountain. They are reached by wagon road of 22 miles, from Glendale. A considerable amount of work has been done on these mines, and profits realized. The quartz vein is large, carries free gold and sulphurets, has a strike nearly due north and dip 60 degrees east. The hanging wall of slate, footwall of porphyry. A depth of 200 feet has been reached. A small stamp mill is on the property. Elevation, 4500 feet.
    Northwest from Glendale seven miles, on Cow Creek, are the Victory hydraulic placers, with very extensive workings. Four to five giants are kept steadily in operation during the water season. The Southern Pacific railroad passes through this property, and the operations in the mines can be seen from the car windows. The gravel deposits are extensive and from five to 50 feet deep. Just below this are the Fuller, Dewey and Valk placers; and about three miles below the Victory, at what is known as Railroad Camp B, is another hydraulic placer, to be seen from the car windows.
    On the headwaters of Shively Creek, a tributary of the South Umpqua River, some rich placers, producing heavy gold, have recently been discovered, and a hydraulic plant is being installed to work them. Lying near the line, in Josephine County, are the Gold Bug and Benton groups of quartz mines, but telegraph, postal and commercial relations are had with Glendale
    Excellent hotels are maintained at Glendale, and fair commercial establishments. Being in a picturesque, healthful mountain region, the charm of summer resort is added to the attraction of the mines.

JOSEPHINE COUNTY.
Hundreds of Miles of Placers Ramify the Mountain Ranges.
    A detailed description of the mining industry of Josephine County would be like reporting the resources of a commonwealth. There are hundreds upon hundreds of miles of placer mines ramifying the mountain ranges. Some of them are of marvelous formation, of vast depth, and a few are being operated on a large scale and with modern, contrivances. What follows in the way of description, like what precedes it, is greatly abbreviated, and is in no case consciously exaggerated. Very much is omitted.
    The exalted bed of an ancient and mighty river, now filled with prodigious deposits of fossils. auriferous gravels and sand, covered with rich soil and the vegetation of centuries climaxed in trees 200 feet high, and paralleled in part by a great mineralized zone, which has been barely touched, is one of the mysteries of this wonderful country. Strength for the ordinary avocation of life falters in the presence of the work which is to despoil the gravel hills and rob the mountains of their golden stores.
    Mount Reuben, terminating in a summit somewhat higher than the surrounding elevations, is a part of the general uplift where the Rogue River Range intersects or joins the Coast Range. It is situated just south of the line between Douglas and Josephine. Romantic history here also has its wonderful tales to tell, including the discovery of the Gold Bug mines.
    Mount Reuben: This locality is as one just discovered. The genuine quartz prospector was late in coming, but found a virgin country for exploration. The mountain is seamed with veins, and the results so far attained are satisfactory and encouraging.
     The Gold Bug group, before referred to, lies on the western slope of the hill, 18  miles by wagon road from Glendale. The general formation of the county here is hornblende andesite. The veins of quartz are from 16 to 25 feet wide, strike west of south, and lie in chloritic chutes intersecting the general formation.
Veins Neither Pockety Nor Blankety.
    The ores are free gold, with sulphurets carrying values. The savings on battery and plates are about 75 percent of assay returns; the sulphurets are saved by vanners in the usual way. The veins have gouge on well-defined walls and dip vertically about 70 degrees from horizontal. The Gold Bug vein has been opened to a vertical depth of 700 feet, the vein increasing in strength and value to the deep. Conditions here and at other mines in Southern Oregon prove that the veins are neither "blankets" nor "pockety." There is a five-stamp mill on this property and a cyanide plant being installed for treatment of the sulphurets. Altitude of mines, 3000 feet.
    The Benton group lies one-half mile due west of the Gold Bug at an elevation of 2600 feet. A serpentine dike traverses the country here, and this group lies in a magnesium trap. Workings nearly 500 feet deep, walls well defined, dipping uniformly 70 degrees east
    The California group joins the Gold Bug on the east in the same character of formation, and has a two-stamp mill.
    Farther around the mountain, to the southeast, some two miles from the Benton, is the Ajax of four claims; formation schists and porphyry. Two parallel veins of quartz, about 400 feet apart and from two to 18 feet wide, return gold averaging $6 per ton. A two-stamp mill is on the property.
    From the Ajax west of south three miles is the Copperstain, a group of four claims. Here an incline shaft follows the vein 320 feet A. Tremain mill is to be supplanted by the orthodox stamp.
    Adjoining the Copperstain on the southwest is the John Lewis property, consisting of a group of claims which are being developed systematically.
    Adjoining the Gold Bug on the northwest is the Ramsey group of six claims. A tunnel cuts the principal vein at a depth of 500 feet. It is well defined and shows 11 feet of ore. An upraise is being made to the surface. The ore is similar in character to that of other mines in the district.
    Across Whisky Creek, which runs at the base of Reuben and on the eastern slope of the opposite mountain, are four claims, known as the Palmer and Kramer. A cross-cut tunnel cuts the vein 200 feet deep. This vein is strong, has four feet of high-grade ore carrying free gold and tellurine.
    On the northeast slope of Reuben three miles from the Gold Bug, and on the wagon road from Glendale, is the New Hope group of seven claims. The formation is porphyry and schists. The veins run northeast, and are intersected by an iron dike nearly at right angles. This locality is intersected by veins running at various courses and from one to 16 feet in width, approximating stock-weeks [sic]. A cross-cut tunnel is to open the principal ore chute at a depth of 210 feet.
    The foregoing details arc summarized to show that this very newly discovered quartz zone is receiving active attention. Many unmentioned prospects in this mountain are being exploited.
    Leland, another point on the Southern Pacific railroad, 276 miles south from Portland, is the departure point for the upper or northern portion of the immense placer fields of Josephine County, and some important quartz mines are being operated in the adjacent county.
    Ten miles east from Leland, by good road, is a quartz mine generally known as the Greenback. The property consists of seven contiguous claims, which are latterly known as the Victor, Jr. They lie in a spur of St. Peters Mountain. The general formation is metamorphic trap. The strike of the veins is nearly due east and west. A serpentine belt or dike, striking north and south, intersects this entire section, and the veins abutting it, as against a wall, cease entirely. The veins are in true fissures, averaging three and a half feet, dip 40 degrees north, at an elevation of 2800 feet. The depth attained on the Greenback vein is 700 feet; ores free and in sulphurets. A 15-stamp mill is kept in full operation, and 25 stamps are to be added. The property is reputed to be paying handsomely with ores averaging $18 per ton. Telephone connection with Leland.
    In this locality, many other properties are being developed, several giving excellent promise of future mines. A two-stamp mill at the foot of the mountain does sample and custom work.
    Placer claims of various areas, depths, deposits and methods of working are tributary to Leland, but rely on Grants Pass for large supplies and local bank facilities. Grave Creek and Wolf Creek, flowing from the north and east, unite near Leland. The beds and banks of these streams above and below the point of junction and the beds and banks of their tributary streams and gulches form an almost continuous chain of placer mines. In the aggregate these auriferous gravel beds cover a large area of country. A short description of one modern plant must suffice.
    The Columbia Mines Company, an Oregon corporation, has an extensive property and up-to-date plant thereon, on Grave Creek, eight miles from Leland by wagon road of easy grade--a delightful summer drive. This plant has, it is claimed, the largest hydraulic gravel elevator ever constructed A halftone cut from a photograph of this elevator, with description of its construction and operation, appears on another page of this paper. It is locally called the Hampton elevator, Professor Hampton having, in its construction, made improvements on the original device of another by adjustment of numerous parts on closely calculated scientific principles.
    The holdings of this company cover an area of about 2500 acres. Water is supplied the giants and elevator through 22 miles of ditches, all four feet wide on the bottom, seven on the top and three feet deep. When the plant is in full operation 4000 inches of water are brought to the mine under head, or pressure, of from 1 foot to 1000 feet, as the various needs require. The impact of a stream of water under a pressure of 700 feet through a six-inch nozzle is terrific. It is very like that of a solid bar of iron moving almost like a cannon shot. When such a stream is diverted upward through a  pipe constructed properly, everything that will enter the pipe must pass through it and to a height determinable by the calculations of the engineer.
    The ground is piped in the usual way into sluices fitted with riffles, where the gold is saved. The tailings--rocks, gravel and earth--fall from the tail of the sluice into the pit at the base of the elevator, where the uprushing stream of the elevator forces all the mass up the pipe to the desired elevation for "dumping."
    A small stream of water drives a Pelton wheel and dynamo, which furnish arc and incandescent lights to the workings, office and residence and quarters for employees. Telephone lines connect the office with distant points on the ditches and surrounding camps and with Portland. It is an ideal plant.
    Eight miles above the plant of the Columbia Mines Company is an ancient channel following, or lying in, the summit of a low range of foothills. This old channel is the bed of a prehistoric river, and now lies at an elevation of nearly 200 feet above the bed of Grave Creek. It has been traced at this point for nearly a mile, and its gravels are being washed in a small way.
Grants Pass.
    This city is the county seat of Josephine, and the commercial and financial center of this great mining country, which extends into Del Norte County, Northern California. Its location is beautiful and healthful. The streets are wide, and business blocks are of brick and stone. It has strong banking institutions, heavy commercial houses, splendid hotel accommodations, and well-stocked livery stables. It is favored with good newspapers, and the Oregon Mining Journal, a weekly publication devoted to the interests of that industry, and the oldest journal of its kind in the state, is published here. A Mining and Commercial Club has a strong and active organization with permanent rooms in this city.
    A 5-stamp custom quartz mill is located here. The elevation above sea level is about 1000 feet.
Gold in Timber-Clad Hills.
    Placers and quartz mines extend from within a mile of the town into the mountains and gorges of the Rogue River, Coast and Siskiyou ranges, all clothed with fir, cedar, pine and oak. The product of the placers has been enormous in the past and continues to be very large; the exact amount is not ascertainable.
    Quartz mining has received scant attention until very recently. Heavy plant growth has been a hindrance, though available timber is of great importance to a mine when opened. The discovery of one quartz mine serves as a fingerboard on the road to others; so the opening of mines aids the prospector in his search for others in the same locality. Somewhere in these hills lie the veins that fed the rough, quartz-bearing dust into the placers.
    West from Grants Pass, 25 miles by wagon road, and rising abruptly from the south bank of Rogue River, is Peavine Mountain. Apparently this mountain at one time joined Mount Reuben as a range or chain, and the accumulated waters cut through this formation, carving out the canyon through which Rogue River now gets its outlet to the sea. Intersecting Peavine on its eastern slope, in a nearly north and south course, and continuing on through the mountainous country, is an immense lode or zone, something over 300 feet wide, made up of a series of highly mineralized veins, lying parallel, carrying gold, silver, copper. Iron and various other metals. This lode was first discovered where the Rogue River had cut it to a depth of over 1000 feet. From this point it has been traced south 20 miles, and north 15 miles, to and beyond the Victory placers on Cow Creek, and through the Cow Creek range. It is surprising that very little exploration has been made upon this remarkable lode. Only one company is now actively and earnestly at work on it, and this is being done at a point on Rogue River. It is generally known as the the Yank ledge.
Prehistoric River.
    A great river surpassing Rogue River 50-fold or more once flowed northward through this country. It was a mile or more in width, and has been traced at interval of its course. Rogue River has cut through it at the mouth of Galice Creek, and from this point northerly for a distance of 25 miles or more this old channel holds its course through the mountains, and cut across by the present streams of Rogue River, Grave Creek and Cow Creek. The northern end so far as traced passes into the placers of the Victory Company on Cow Creek in Douglas County. South from the mouth of Galice Creek the old riverbed passes through the Briggs Creek placer district, on across the lower Illinois River to the Waldo placers on the west fork of the Illinois, a distance of 45 miles. In its southerly course it has been cut across by Briggs Creek, Illinois River, Josephine Creek and the west fork or the Illinois. On its course south this old stream appears again in Northern California. Wherever encountered the gravelly bed of this prehistoric stream has been found rich in gold, and considerable quantities of platinum have been found in it. A very small portion of the bed of this ancient river has been opened in Oregon. The general elevation of its bed above those of the present streams is about 400 feet, and where modern streams have cut it their beds or banks have been  rich in gold.
    Peavine Mountain has many quartz veins; several projects being opened; ores, free-milling gold. The output of some of these claims is being reduced by the old arrastras--mule power.
Copper Vein Nearly a Mile Long.
    A copper vein, 15 miles northwest from Grants Pass, 15 feet wide and 5000 feet long, is being prospected; and in the southwest portion of the county is an extensive section of country which extends into California.
    The ancient placer towns of Waldo, Kerby, Althouse and Browntown are in this locality. Energetic work is in progress here on big copper prospects, all of which carry well in gold. Croppings appear in nearly every hill, and the surface showings are excellent. This country is reached from Grants Pass by daily stage through Kerby and Waldo to Crescent City, Cal. A daily stage also connects Kerby with Browntown, a distance of 13 miles. Telephone lines connect Grants Pass with Waldo, Selma, Kerby, Shelby Creek and Crescent City.
    South from Grants Pass is Williams Valley, a garden spot of orchards, alfalfa fields and flowers, 10 miles by three miles. It is surrounded by imposing mountains. Looking up from the valley one sees holes ranged in the mountainsides above like pigeonholes in a concave desk, apparently almost in reach. These are mouths of tunnels, opening to quartz veins of copper and gold. The ores are of high grade and extensive operations are being pushed. Three of these mines have a 5-stamp mill each, and another mine is procuring a mill. The formation is limestone and porphyry.
    A wonderfully beautiful and massive mountain of purest marble overlooks this valley. This hill has all the variegated marbles in colors and tints, and from purest white to onyx-like black. It is unappropriated and almost untouched.
    On Baldy Mountain, southeast, and four miles from Grants Pass, is the Jewett quartz mine of free gold, and calaverite, in large vein. It has a 5-stamp mill.
    Placers exist on Jump-off Joe, Louse and Jones Creek The Dry Diggings are within three miles of Grants Pass, and cover 100 acres. There are extensive placers in the Williams Valley country, and on Oscar Creek, the latter noted for big nuggets.
    Two properties merit special mention as typical of the formation and methods of operation in this county, one lying east and the other west of Grants Pass. On Louse Creek, eight miles northeast by good road, is a group of placer and quartz claims known as the Granite Hill property, where 500 acres have been covered under one title. The entire tract is covered by splendid timber, and to murder those trees, even in the pursuit of gold, seems a sacrilege and a crime. The elevation of the tract is 2200 feet. The middle, north and south forks of the creek converge at one point, and the placer claims are laid here, extending up each fork and below the junction. Just below this junction a movement of the earth, or slide, from the adjacent mountain on the north, long ago, filled the former channel of the stream, forming a huge basin which has been filled with gravel and subsequent soil to a depth of 50 feet, so that an area of 60 acres has been formed in what formerly was a mountain gorge. Prospect shafts sunk at various points show the gravels rich in gold, reputed to average 75 cents per yard of the entire deposit.
    To open this bed of gravel and gain a tailings dump in the canyon below, a tunnel which will tap the bedrock under the gravel at its lowest point is being run. It requires 1400 feet of tunneling, which will be utilized by placing sluice boxes firmly on its bottom, this conveying away the washings of the gravel deposits above to the canyon below. The body of the slide is of material too compact to be removed. The total pay gravel area of this property is fully 250 acres, the average depth being 25 feet. A few acres of the upper deposit have been worked profitably, 6½ acres returning $60,000 in dust.
    An excellent feature here is the absence of large boulders. Water for the hydraulic pipes and giants is brought eight miles by ditch, which are to be, or ought to be, enlarged.
    Five quartz veins cut the mountainsides above the placers. They are from one to 15 feet wide and carry free-milling ore. The ores from these claims was formerly worked by four arrastras. The mules, being of the slow-gaited variety, were turned out, the arrastras abandoned and a 5-stamp mill now reduces the product of the mines, which have been opened in some 1200 feet of workings. The owners are R. A. Booth. J. O. Booth and C. L. Magnum, of Grants Pass.
    Several lesser properties lie below on this creek, one of which is using the Ruble elevator.
Galice Creek and Blue Gravel Placers.
    Here [the] chronic geologist and practical miner can find mental and bodily sustenance; the one in these marvelous mines, the other at manager Harvey's unpretentious but ample board. The property lies on Galice Creek, 25 miles northwest from Grants Pass. The deposit lies in a section of the bed of the ancient river before mentioned, which parallels Galice Creek at this point. The bed of the old stream, which is the bedrock of the placers, is about 450 feet higher than the bed of the present stream. This bedrock consists principally of shales and slates, with occasional thin strata of sandstone, all with strata upturned and in places much contorted and twisted. On extensive areas of this old riverbed, recently made clean by the placer washings, the polishing, rippling action of prehistoric waters is distinctly visible. At one place a sheer fall in the old river of 20 feet appears, disclosed by recent removal of the filling of gravel and sand, which had hidden it for centuries. The width of this channel is supposed to be from one-half mile to one mile; but at this point, though thousands of feet have been uncovered, the western rim has not been reached. The workings have been carried on from the east side--nearest Galice Creek--and the bedrock, or riverbed, is still "pitching into the hill," indicating that the center of the channel has not been reached. This old channel was filled with the gravels, rocks and sands of long ago, and with them the gold. It is a marvelous deposit, in places exceeding 200 feet in depth. Its course is due magnetic north. The placer claims laid along it, and now owned by one company, extend for a continuous distance of four miles. The general elevation is 1500 feet. Of these mining claims 950 acres have been patented and 600 acres are held under the usual possessory title. Seven small tributaries of Galice Creek have cut through this deposit and down through the bed of the older stream, enriching Galice Creek with the gold which made men rich and that creek famous in the early days of placer mining here.
    At 12 points along the eastern rim of this old channel, and within the four miles mentioned, the several original owners worked into the deposit, and the amount of gold obtained was very great, but the depth of the banks became so great that operations with divided supplies of water became impracticable. More water was indispensable, but various owners could never agree on means of getting it so titles finally were concentrated in J. R. Harvey and his Chicago associates. During the year past Mr. Harvey has improved the water supply and consolidated the workings so that three giants with 6-inch nozzles and under a head of 500 feet are thundering day and night against walls of auriferous gravels and sand over 175 feet deep, and which persistently stand vertical till knocked down in slabs of 10,000 tons each. It is a thrilling, awe-inspiring sight to look from the verge of a vertical wall of 200 feet, down upon the human atoms as they direct the hill-destroying streams below. The giants are set on the bedrock and the water applied at the base of the bank, and as the lower stratum is washed out the upper ground breaks for want of support and slides into the pit to be washed away.
    These great beds are composed chiefly of gravel from two to three inches in diameter, graduating into pebbles, grit and sand, lying in alternating layers or masses of quartz sand very compact, but not cemented. The deposit is practically free from boulders, cement and clay, a remarkable condition. A peculiar feature of this deposit consists of numerous large boulders distributed irregularly through the mass and of perfect form but so completely decomposed as to crumble at the touch and dissolve in the water more easily than does the material which surrounds them. Manifestly, it was a sluggish stream that made this deposit.
    The gold runs from fine dust to nuggets of $50--occasionally pieces are found which weigh $100. An abundance of timber of great height has grown upon and covered this deposit, and a saw mill comprises part of the plant. Water is supplied through 20 miles of ditches 5 feet wide at the bottom, 7½ feet at the top and 3½ feet deep. The climate is the ideal one of Southern Oregon.
    The Big Yank ledge, mentioned elsewhere, at this point parallels the old channel and its deposit, lying to the west at a distance of less than one-fourth of a mile.
    The Dry Diggings hydraulic placers, three miles east of Grants Pass, have been operated for 30 years with scant supplies of water and during short seasons. The property covers 400 acres and is noted for production of coarse gold and big nuggets. Preparations are being made to increase the water supply by pumping into reservoirs from the adjacent stream, and to enlarge the ditches. A mammoth vein was uncovered by these placer workings and lay unappropriated until November last. It is 200 feet wide, evenly mineralized, and preliminary tests show an average of $5 per ton in free gold and pyrites. A mill run is to be made of ore taken entirely across the vein. Its strike is nearly due north, dip not definitely ascertained.
----
JACKSON COUNTY.
Work Near Gold Hill Retarded by Insufficient Water Supply.
    Gold Hill is a growing town on the Rogue River, 313 miles south from Portland by rail. It is immediately surrounded by a rolling country, the foothills of the mountain ranges. It is ably represented by a good weekly newspaper. Two quartz mills are maintained here for custom work. There are two well-stocked livery stables. The hotels, three in number, are not quite good enough to meet the demands. Miners, like other experienced men, prefer comfortable quarters and pretty good food. Even in rude cabins the American gold miner usually manages to have good provisions, and on  necessity is a good cook. One of these, on placing before his guests a splendid dinner of bean soup, brook trout, grouse, potatoes, lettuce, tomatoes, biscuits and ideal coffee, all elegantly prepared in the ample fireplace of his log cabin and served smoking hot, declared that "it is better to have good food on one's table than napkins and silverware." Good hotels are useful adjuncts to all important mining camps.
    Development of placers tributary to Gold Hill has been retarded by insufficient water supply; and this district has suffered somewhat from ill-founded repute that the quartz veins are "pockety." The pocket hunter is no true miner. Vegetation and soil cover the hills wherein lie the quartz veins. The pocket hunter methodically "potholes" the hillsides. He digs a system of holes in the soil to the rock and pans the dirt, noting the presence and quantity of gold dust taken from each hole. Finding by this means a channel or flow of gold in the soil, he follows it, potholing as he goes, until he locates or reaches the source in the quartz vein upon the hillside. He sinks on the vein here and often secures several hundred dollars' worth of very rich free gold quartz, which he crushes in a mortar or in a dolly, and pans out the gold; or takes it to the custom mill for reduction. It is a fascinating business. But when depth is attained, compelling the use of candles for light, or windlass for hoisting, the work becomes slow and tiresome. Nothing but the biggest of prospects holds him. Ores yielding less than $100 to the ton do not pay for this style of mining. Twenty-dollar ore is useless to him, so if the rich streak from which erosion fed the hillside doesn't hold out, or the vein "pinches," as all pay bodies do, this anomalous miner goes to another point on the same or a neighboring hill for renewal of prospecting for pockets. A great deal of this kind of mining has been done in this section, and men do well at it, make big wages often. But the reports of surface pockets have gone abroad, and tended to divert the real quartz prospector to other fields. However, late working to depths show that the veins continue with ores of high grade for milling. As to quartz mining, this section is as a new country, and unprospected.
    On Sardine Creek for several miles are a series of placer claims, all worked when water can be had. One of these is a farm of 360 acres, patented as such, which the owner cultivates in summer and hydraulics in winter.
    The Lucky Bart quartz group of six claims is on this creek, the mouth of which is within a mile of Gold Hill. A five-stamp mill is on this group, which is in a formation of diorite and slate, elevation 2600 feet, ores free gold and sulphurets. There are many quartz prospects on this stream.
    On Wards Creek are hydraulic placers, and the Gold Chloride quartz claim, a late discovery, being developed; ore mills an average of $30 per ton, altitude 2600 feet, formation slate and porphyry. On Pleasant Creek are some placers reputed as among the best in the state. The Cameron claims of 1500 acres are operated at several points by giants; depth of gravel banks 30 feet.
    On Kanes Creek adjoining the town of Gold Hill, the placers extend up the stream continuously for four miles, but there is scarcity of water. Above the placers on either hillside are numerous quartz prospects. The Braden group covers 800 acres, has five parallel veins, striking easterly, dipping about 30 degrees south. One vein strikes across the course of the others, dips westerly 40 degrees, vein 10 feet wide, all pay ore. Formation of the locality granite, diorite, porphyry and slate; elevation 1800 feet. A 10-stamp mill is running on the ore. One mile farther up the stream is the Roaring Gimlet group of three claims. It has been very productive, and continues to supply free-milling ore to a custom mill in the vicinity. The vein lies between a slate-hanging and porphyry footwall; pay streak two feet wide, strikes easterly, dip nearly vertical.
Little Work Netted $30,000.
    On Galls Creek placers are being worked in a small way for three miles. The water supply is scant. Some of the best quartz claims in the district are on this stream. The principal ones are the Kubli property of 12 claims, three parallel veins, all being worked. A three-stamp mill is being replaced by a modern five-stamper. On the hill opposite is the Bill Nye group, a large producer; veins nearly vertical, strike northeasterly, ores worked in custom mill at Gold Hill. There are numerous prospects here, and one, the Bliss claim, is reputed to have produced over $30,000 from a shaft of 42 feet and a drift of 30 feet
    On the west fork of Foots Creek for six miles, and on the east fork for eight miles there are continuous placer claims, several of which are operated extensively by hydraulic. There are thousands of acres of unappropriated placer lands on these streams. Water is scarce. Mayhap the dredger men will find opportunity here.
    On the Main Creek is the Horseshoe group of two quartz claims, with a five-stamp mill. The Dixie Queen, south from the Horseshoe, with similar formation, has its ores worked at a custom mill. The ore is reputed to produce gold at $100 per ton. These are types of some 40 prospects in that vicinity.
    East from Gold Hill two and a half miles is the locally famous Blackwell quartz property of 320 acres. There are seven ledges, three being worked. Depth can only be attained here by sinking. Veins nearly vertical, formation slates and porphyry. The Tolo, of six claims, adjoins the Blackwell on the north. These lie in a granite belt and carry free gold. These workings are well supplied with steam hoist and power drills.
    On Nigger Baby Hill, three miles north of the town, is a recent discovery of an 18-inch vein, carrying $40 gold per ton.
    There are a great number of prospects, making promise of permanent mines, on which development is being prosecuted. They are too numerous for detail.
    Some 10 miles north from the town a large body of cinnabar has recently been exposed. The vein is 500 feet wide, and ores from it discharge globules of pure quicksilver. It is now being opened by a strong force of men. And on Elk Creek, 25 miles north of Gold Hill, is an entirely new district of large veins of low-grade ores. A Huntington mill has been taken to it, to be followed by a five-stamp mill. It is in the foothills of the Cascade Range at an elevation of 4000 feet.
    Deposits of copper, coal, asbestos and mica exist in the county at the headwaters of Evans Creek. The extent of these is not known, but all are being opened. It is known as the Meadows district.
    The immense power of Rogue River can be utilized to great advantage in this locality, and the gravel elevator and dredger may soon come to obviate the extensive use of water and overcome the flat-lying gravel beds, which exist at some points. The quartz prospects are most favorable. Well-directed work will make a great country of Gold Hill district.
    From Medford northeast 25 miles, and from Gold Hill 18 miles, in a spur of the Rogue River Range, are two groups of claims on a cinnabar deposit. Development is in progress. On one group of six claims the Rogue River Quicksilver Mining Company has a shaft 6x7 feet sunk to a depth of 56 feet, showing a vein of ore 6 to 14 inches. The other group of five claims lies adjoining the first named. A shaft has been sunk here 112 feet in ore formation like the other. In this shaft the vein is 11 feet wide at the bottom, has a northerly strike and a dip nearly vertical.
Jacksonville Has Produced Millions.
    Jacksonville, county seat of Jackson County, is the pioneer town of the Southern Oregon district. It began as a frontier mining camp in the winter of 1851-52. Its founders and dwellers were types of the best brain and brawn of America. Others came, but Americans dominated. Their courage and strength and their gold aided mightily in the then new and forward movement of the world. They poured millions into the then almost empty chest of commerce. Oregon and California roused a lethargic world. Since those days civilization and science, with seven-league boots, have climbed to heights never dared before.
    Contemplation of these things dwarfs consideration of present details to insignificance. Yet science, built upon what the delvers disclose, comes to give reward and help to renew the harvest of gold and rejected rocks may become "the headstones of the corner."
    The placers have not all been worked out; the veins in the hills have remained untouched, scarcely looked for. A great many small gulches are being worked in a limited way; scarcity of water again. Their number is too great to specialize. The principal ones are on Frost Creek, six miles from Jacksonville, Poormans Creek, five miles, and several others that were once large producers. On Upper Applegate are two hydraulics and numerous small mines.
    The Sterling placers are a type of the greater mines. They are on Sterling Creek, eight miles by splendid wagon road of easy grade, from Jacksonville. Great quantities of coarse gold came from them in the early days, gotten by the simplest methods. But the water supply was limited to the rainy season, and with each passing year there was a marked decrease of rainfall, until now it is not more than one-half its early annual supply. So, with failing water and deepening gravel banks, the old-timers slowly gave way. Nearly all the original claims finally passed into the hands of the Sterling Mining Company, a Portland corporation. This corporation has two stockholders, V. Cook and Henry E. Ankeny, the latter being practically president, board of directors, manager and superintendent, the rest of the company trustingly leaving everything to him. It is an ideal board, and necessarily everything moves satisfactorily and to the great profit of the stockholders.
    These placers cover some 1500 acres, which extend for 5½ miles along Sterling Creek. The deposit of gravel is from two to 100 feet deep. The  hillsides are piped for gold. The property is splendidly equipped with piping, giants, flumes, ditches and sluices. When in full operation, four No. 4 giants utilize 4000 inches of water, brought chiefly from the Siskiyou Mountains, by a system of ditches constructed for the purpose. The largest, or Siskiyou, ditch, is three feet wide on the bottom, 6½ on top, 3½ deep and 28 miles long. Other ditches bring water from other sources. One, six miles long, carries 500 inches of water; another of the same length, 1500 inches, and another, five miles long, carries 500 inches.
    The bedrock consists of strata of shales, porphyry, sandstone, in streaks, and occasional points of granite, all tumbled and distorted, small kidneys and stringers of barren quartz cutting through and interlacing the whole. These mines present curious and interesting features, not possible to relate here, in variety of gravels, including cinnabar, and of bedrock.
Fossil Remains in Deep Workings.
    Fossil remains in abundance and great variety are encountered in the deep workings as the giants break down the bank in huge slabs. Among the remains thus exposed was one of a mastodon's tusk measuring 26½ inches in circumference and 11½ feet long. Nine years ago nearly an entire skeleton of one of these monsters was distinctly exposed, imprinted in the massive banks; the backbone, ribs, joints, shoulder blades, leg bones, all save the head. They were much decomposed, but perfect in outline and position. Tusks and bones of these mammoths have been encountered yearly during the last 10 years. Last season a six-foot tusk was uncovered. Imprints of fossil shells and of leaves, etc. are of common occurrence.
    A post office and excellent school near it are maintained on the grounds of the company. Gardens and small farms in the vicinity supply vegetables, fruit, eggs, milk and meat to the community engaged in getting the gold.
    There is a group of gold quartz claims covering 240 acres of patented ground 1½ miles west of Jacksonville, at an elevation of 2600 feet. There are five parallel veins opened, one to a depth of 200 feet. The strongest vein is 24 feet between walls, all regarded as pay ore, the best values being in a six-foot stratum. A five-stamp mill is on the property, crushing ore. Values in concentrates run high. The strike is northwest and dip 70 degrees west. The formation is slate and diorite.
    On Forest Creek, 10 miles northwest from Jacksonville, are several quartz properties in various stages of development. The Mountain Belle has been worked almost continuously for several years, reducing the ores in a Huntington mill.
    On the same stream the Winningham and Pentz has been operated for three years, using a five-stamp mill.
    On Applegate, west from Jacksonville, 10 miles, a custom mill has been running for several years, reducing and testing ores mined in that locality. There are no deep or extensive workings here, but the miners are sticking to their prospects.
    Jacksonville is well supplied with commercial houses and a solid banking institution. The hotels are fair, the livery stables good. It is splendidly represented by a newspaper issued in weekly and semi-weekly editions.
Mines in the Vicinity of Ashland.
    This city, situated on the Southern Pacific Railway, 341 miles from Portland, is the southernmost point of supply for Oregon mines. The climate is matchless, and the location of the city superb. Its most excellent hotel is of advantage to mining men, as well as are its good livery stables, prosperous banks and ably conducted newspapers. Its site at the foot of the Siskiyous is at an elevation of 1940 feet. Ashland Butte, to the south, is 7662 feet high, and Wagner Butte, west of south, reaches an altitude of 7245 feet. The Siskiyou Range rises immediately to the south of the city, and the railway's grade commences its ascent of the mountain before passing from the city limits.
    A quartz mine named the Ashland is reached by a good wagon road of three miles, running southwest from the city. The mine is in a mountain ridge buttressing Wagner Butte, in granite formation; the hanging wall is granite, foot wall diorite; elevation 3500 feet. The workings are through a shaft and tunnel levels to a depth of 800 feet, the deepest workings in the county. The vein is from four to 10 feet wide; strike northerly, dip west about 65 degrees. The gangue is quartz, carrying free gold and sulphurets. It has a 10-stamp mill located in Ashland, which, by amalgamation and concentration, saves 90 percent of the assay values, a good mill record.
    The Shorty Hope mine lies about one-half mile west from the Ashland. It is a typical, fissure vein of large size, cutting all formations. Its strike is northwest, dip nearly vertical. It probably intersects the Ashland vein at a point south from the Ashland workings. The quartz is free milling. The elevation about 2500 feet The mine is well equipped and has a 10-stamp mill, driven by water power. Above the Shorty Hope are a great many good prospects in various stages of development.
    Farther west and south, 12 miles from Ashland, on the headwaters of Little Applegate Creek is an area of cinnabar prospects. Here a large serpentine belt which intersects a portion of Josephine County, passing into northern California, is encountered. It is underlaid by slate. The cinnabar occurs in an area of altered locks lying east of the serpentine and embraces 8 or 10 square miles. One prospect here has been somewhat extensively developed. This is the most extensive exploitation for cinnabar in the Siskiyou Range.
    Farther west in the Siskiyous, on the headwaters of the several tributaries of the Applegate, is a "likely country" of auriferous rocks and gravel, little explored.
    Up Ashland Creek three and one-half miles south of the town is the Reeder quartz claims, recently opened and in course of development. The formation, character of ore, strike and dip is similar to the Ashland vein, save that the proportion of free gold is less, the values, which are high, lying in the pyrites. It is supposed to be an extension of the Ashland vein system.
Quartz Lode on Mount Reuben.
    Still farther south by trail over Ashland Butte--unsurpassed for scenic grandeur and beauty--a few miles south of its summit there is a strong ledge, somewhat developed, showing stibnite--sulphide of antimony--carrying a fair amount of gold. A few miles below this on the head of Grouse and Beaver creeks, are some old placers, worked in the early '50s, from which millions of gold were taken. This locality was never abandoned, but has been worked continuously to the present time. Additional rich and extensive gravel beds have recently been discovered and equipped with hydraulic plants. A striking feature of this general locality is the recent discovery of a strong and remarkably rich quartz lode on the top of Mount Reuben. Nearly $30,000 was taken from it in gold of the form very like the product of the placers below, and which was worked by mortar and pan. Recent prospecting disclosed the fact that a series of auriferous veins intersect this mountain. The marvel is that the early placer miners on Beaver and Grouse Creeks never searched the mountain above them for the source of the gold they were getting. Probably it was the old story--they knew little of quartz and had no machinery from the faraway shops with which to work it. The country is abundantly supplied with water, timber, game, and scenic points indescribable, and it is blessed with an ideal climate. The country is accessible from Ashland by wagon road ending in a trail over the butte or by a ten-mile mountain trail due west from Coles, a railway station at the boundary line between Oregon and California.
    From Ashland, up Bear Creek Valley, nine miles in a southeast course, by good road, is the Free Silver, or Barron, mine, lying in the high foothills of the western slope of the Cascade Range. This mine is of peculiar interest from the fact that in rock formation and character of mineral deposits it has a marked resemblance to certain localities in Colorado. Mineralogically the Barron mine is most interesting. It carries 16 or more different elements. Free gold, and free silver, and ruby silver are abundant. The ores generally are base and embrace the tellurides, realgar, sphalerite, galena, iron pyrites, etc. It is a smelting proposition.
    Locally this section is called the "Cripple Creek" of Southern Oregon, because of the presence in quantity of the telluride ores, not found elsewhere in the county. This mine carries a large amount of silver, greater than any other in this region. Many contiguous locations of claims have been made, but as yet they are merely "prospects." The general formation is eruptive; the elevation about 2000 feet.
    In the Cascade Range near Ashland are many deposits of mineral paints, kaolin and clays convertible into finest China porcelain wares. Mineral springs, carrying medicinal waters, are numerous in the vicinity of Oregon's southernmost city.
----
ALL THE COMFORTS OF LIFE
In No Part of Oregon Is Mining Work a Hardship.
    In this very greatly condensed review descriptions of many great mining properties from which information, general and technical, could be derived have necessarily been omitted. They have been barely referred to by name. Localities of great extent and promise have often been but vaguely mentioned.
    The mineral-bearing areas of Oregon are extensive, rugged and mountainous, and until the coming of the railway almost inaccessible to machinery. Nearly all the early placer miners departed with their gold. They were succeeded by wheat growers, horse, sheep and cattle raisers, lumbermen, fishermen, horticulturists and traders. The matchless forests, the wonderful valleys and the almost limitless prairies and plains, and the rivers, aswarm with royal chinook, gave place and employment to all these, and there ever was room for more. The few remaining miners, aided occasionally by newly arrived prospectors, have proven the existence of great ore bodies in each of the localities which have been mentioned, and that thousands of miles of payable placers still remain in gulches and creek beds. American genius, with new contrivances, wonderful machinery and modern metallurgy, is come to their aid, and the harvest of gold in the future ought to be great--greater than that of the best of the early years.
    The field is vast, but the laborers are few, widely dispersed and isolated. Fill this field, open these mines, and there will be a home market for Oregon fruits.
    A most striking characteristic of the miners in Oregon must impress deeply every man who goes into the camps of the various districts. With scarcely an exception the best house in town is the schoolhouse. Where two or three families are gathered together there is a schoolhouse in the midst of them. Is it habit, trait, loyalty or love for his kind, or all these? Truly, it is American. By the time the third family of five children arrives, a volunteer committee, with the proverbial "old miner" as its head, is arranging for the construction of that inevitable and indispensable schoolhouse. The committee may have homes in shacks, but that schoolhouse must be comfortable, and is often ornamental.
     Thanks are due by every reader of this to the miners and managers who have given freedom to properties and information and aid for its preparation. Their generous assistance, always cordial, has been invaluable, the regret being that a bare tithe of the truth can be told.
    The American miner is intelligent, earnest, brave and patriotic. His success is not promoted by the failures of others. He can well declare: "I am a true laborer; I earn that I eat, get that I wear, owe no man hate, envy no man's happiness, glad of other men's good."

Morning Oregonian, Portland, January 1, 1902, pages 35-36

MINING IN SOUTHERN OREGON
By Dennis H. Stovall
Photographs by the Author
    The story of the discovery of gold in Oregon is nearly parallel to that of the mad rush to California in '49. The first nugget that betrayed the presence of the royal metal was uncovered on Josephine Creek, southern Oregon, May 2, 1851. The discovery was made by a party of wandering miners from California who had crossed the Siskiyou Range and were trying their luck in the Oregon country. Gold was next found on Canyon Creek, near Josephine. The third discovery was made at Waldo, of the same district, which was called Sailor Diggings. This name was given the camp because of its discovery by a band of sailors, who had heard of the rich gold fields in Oregon and deserted their ship while at anchor near Crescent City.
Southern Oregon gold, August 1906 Sunset magazine
    Early in 1852, less than one year from the time of the original discovery, gold seekers swarmed every gulch and creek in southern Oregon. Busy camps sprang up in a night at Kerbyville, Althouse, Waldo, Galice and Jacksonville. With rocker and pan millions were cradled from the auriferous gravel bars. Following the era of rocker, shovel and sluice, the placer bars and channels of southern Oregon were in due time equipped with hydraulic mining apparatus. The first giant thundered its shaft of white on Jack Layton's mine, Applegate river, 1862. Others soon followed, and in a few years this region contained the largest number of hydraulic mines of any section of similar area in America, and this distinction is still the proud boast of the surface miners of the most productive mining district.
    Southern Oregon is peculiarly adapted to hydraulic placer mining. Every stream and gulch contains gold. Even in the valleys, where the soil is rich, there is gold, and the farmer and the miner work side by side. Owing to the abundance of the auriferous gold deposits, the many streams, the mild winters, the heavy rains, the non-restricting mining laws, the placer miner has many advantages in this section that are denied him elsewhere. Beds of ancient channels are found along the rivers and streams. The gravel of these old diggings comprise the diggings of the placer mines. These channels lie on bedrock to a depth of from eight to two hundred feet. On the bottom, next the bedrock, are the boulders, the nuggets and coarse gold. Above this is the finer gravel and pipe clays, lying in strata of blue and gray. Still above this is the layer, or capping of red clay, which carries its values in fine or flour gold.
Southern Oregon hydraulic mine, August 1906 Sunset magazine
    To build and develop each of the scores of big hydraulic mines that operate in southern Oregon, no little capital, skill and labor was required. Several hundred miles of ditches and flumes were constructed, to bring the water down from the nearest streams. Some of the mines go ten, twenty and even thirty miles for their water, in order to get it in the greatest possible quantity. It is stored in huge reservoirs or bulkheads three hundred or four hundred feet above the diggings, on a mountainside or prominence. Huge pipes, like so many steam boilers riveted end to end, lead down to the diggings from the reservoir, and forking, branch off in smaller pipes to the giants.
    As the amount of mining done is dependent upon the water supply—other things being equal—that miner who has the best supply for the longest season is owner of the best property. The hydraulic placer season is covered only by the wet or winter months, beginning in November and closing in April or May. A few of the larger properties operate through June and July. The dry season is utilized in making the annual cleanup, and in overhauling and repairing the ditches, flumes and pipe lines. Once started, the giants never cease their roar from the beginning to the end of the season. Night and day they hurl their avalanche, ceasing only when the north wind puffs warm, and the snows disappear from the peaks of the Cascades.
    One giant washes down more gravel in an hour than the pioneer, with his shovel and rocker, could do in weeks. It costs from one and one-half to five cents a cubic yard to mine a mountain by the hydraulic method in southern Oregon—after the first cost of equipping the property. It is usually considered that a giant mines $100 in gold each day it is operated. This is a very conservative estimate, as there are a number of mines that uncover $200 every day with each giant. A crew of only fifteen men is sufficient for both the day and night shifts of the largest properties. The mines produce from $6,000 to $60,000 each for a season, the size of the cleanup depending upon the number of giants employed, and upon the general capacity of the property, as well as upon the value of the ground. But on an average, the placer channels of southern Oregon carry from ten to thirty cents a cubic yard, thus leaving a good margin of profit. Placer mining, like any business, must be conducted on business principles to be successful, and in southern Oregon the operator has everything in his favor.
    But all southern Oregon's gold comes not alone from placer channels. And while this section of the state has some of the richest quartz mines of the West, ledge mining is in its infancy here. Because of the great amount of gold on the surface, the genuine prospector was long in coming. At present there are over one hundred and fifty quartz mines being operated or developed here and more than thrice that number of claims and prospects. Where there is such vast acreage of placer ground and surface diggings, there must also be deep-setting ledges whence the gold of the wash channels came. So the development and operation of recent years has demonstrated that southern Oregon has vast bodies of free-milling and base ore in its mineralized mountains.
    There are some twenty-five mines equipped with mills and reduction plants in southern Oregon. These mills represent a total of two hundred stamps. Many of them increased their batteries this season, because of the excellent showing of the ore bodies. The Greenback, with its two mills, one of ten and the other forty stamps, is the largest southern Oregon quartz property. Three hundred and fifty people, supported entirely by the mine, live in the town of Greenback, on Grave Creek. Granite Hill mine and camp, with its population of two hundred, is another of the larger mines of this district, and is located near Grants Pass. Other camps and flourishing mining centers are Gold Hill, Takilma, Galice and Jacksonville.
Granite Hill Mine, August 1906 Sunset magazine
    One of the big advantages in quartz development and mining in this section is its cheap natural power. This has been secured by harnessing Rogue River, a wild, turbulent stream, which flows across the southern end of the state. This power is already distributed, by electric wire, to all the principal mines and camps. It is used, not alone in mining, but for every conceivable purpose. The biggest power plant yet built on Rogue River is that of the Condor Water and Power Company at Gold Ray. A concrete dam has here been built across the Rogue, lifting the water twenty feet, and developing ten thousand horsepower. At Dry Diggings, the Golden Drift Mining Company has built a similar dam and has utilized the power to drive a monster set of pumps with which the hydraulic giants are operated day and night the entire season.
    The Greenback, Granite Hill, Opp, Braden, Homestake and Bill Nye mines all use electric power, generated by the power dams on Rogue River. There are already more than three hundred miles of electric wire power line in southern Oregon, and more lines are being strung. Electricity is not only more convenient, but is a far more economical power than steam. It is more regular, is no trouble to generate, is always ready, and can be conveyed to the deepest levels of a mine without loss, or without causing the great discomfort of extreme and smothering heat. This proves a decided advantage in all properties that require much pumping from the lower levels, to prevent flooding. The use of electricity for power also saves the fine timber on the mining claims, leaving it to a better purpose than that of being cut into short lengths for cordwood.
    Thousands of acres of rich dredging ground on the Applegate, Illinois and Rogue rivers have been bonded by the Oroville and other prominent dredging companies of the West for development and operation. On Foots Creek, a tributary to the Rogue, the dredger of Champlin & Co. has been successfully operating for the past three years. This dredger is operated by electricity, and is one of the largest and best of all the great fleet of gold ships of the Pacific Coast. It has a capacity of two thousand yards daily, and has ground enough to keep busy, day and night, for twenty years. This dredger makes a weekly cleanup of from $1,500 to $3,000.
    Southern Oregon has a rich and extensive copper belt, located at the lower end of Josephine County in the Waldo district. The great Iron Mountain and Siskiyou copper sections of Northern California, only a few miles farther south, are a part of this same belt. This copper area is twenty-five miles wide by sixty miles long, and embraces a half score well-developed properties. At Takilma, near Waldo, is located the Takilma Smelter, Oregon's only copper reduction plant. It was built and is operated by the Takilma Smelting Company of Colorado, and the Waldo Smelting and Mining Company of California, both companies owning properties in the district. The smelter has a capacity of two hundred tons daily. During the summer season, the Takilma Company employs a freight train of one hun
dred and twenty-five horses and mules to haul over the forty-five miles of mountain road from the smelter to Grants Pass, and to carry out coke for the operation of the plant. Large crews are employed in the Queen of Bronze, Cowboy and Lyttle mines, the properties that supply the smelter with ore. After the present summer, the method of hauling matte and coke by wagon will be a thing past, as a railroad is being built, connecting the smelter with the Southern Pacific at Grants Pass.
Sunset Magazine,
August 1906, page 139


The Art of Prospecting in Southern Oregon
Written for the Northwest Mining Journal by
Dennis H. Stovall, Grants Pass, Ore.

    Two professional prospectors came here from the state of Washington, entered the Williams Creek district, and cleaned up $30,000 in three weeks. The ground on which these men did their work had been prospected time and again; it is one of the oldest mining districts in Oregon. But these men found gold where others had failed; it was because they knew their business.
    The two boys have only sunk a few shallow prospect holes, and the gold they have taken out is only the rich stuff contained in the oxidized portion of the vein. They have really struck a system of quartz veins, and the conjunction of these ledges forms the rich bunches from which the main bulk of the gold is taken. Besides the large amount of metal already taken from the discovery, all of which has been mortared out by hand, there yet remains fully $75,000 in sight.
    The Southern Oregon Mining District, which extends from the California line on the south to the Calapooia Mountains on the north, and from the foothills of the Cascades on the east to the Pacific Ocean on the west, covering an area of 5,000 square miles. Much of this country is quite mountainous, some of its summits reaching 5,000 feet above sea level. But between these spurs and ranges rest beautiful valleys and vales, all abundantly watered by the numerous rivers and creeks that are fed by the everlasting snows of the higher levels. Gold is found everywhere in the district. Here the farmer and the miner work side by side. Though some of the districts have been scratched over for the past sixty years, there still remain many sections that have not been prospected at all.
    The geological formations are chiefly metamorphic slate and quartzite in the southern part and slate, serpentine and conglomerate in the north. Denudation has been very extensive in all the region, cutting canyons 2,000 feet deep and carving out valleys and mountains from what appears to have been an elevated plateau.
    This is an easy country to prospect. The winters are mild, and the abundance of water and timber makes it possible for the gold-hunter to remain on the trail at all times of the year. The method most used by prospectors in this district is that of "tracing."
    When a favorable spot is found, the prospector halts and strikes camp beside a stream. He follows the stream and pans the dirt, washing each pan down carefully and scanning the remaining residue for colors of gold. If a little string of yellow flows in the corner of the pan, close behind the black sand, the prospector smiles. The little string of yellow is colors of gold, and the black sand to which it closely clings is its inseparable companion. He pans again, near about, then pans again, and if the colors grow better with each pan, the prospector smiles yet more happily, for then he knows he is on a trace, to follow which correctly will lead him to the treasure.
    Frequently during the panning the prospector pours the minute dust-like particles into the depths of his palm and examines them critically. He knows at once whether all of those colors came from the same source. No two colors of gold are alike to him. And that is why the old-timers say "prospecting is an art"--it requires years to learn some of these things.
    When a ledge is struck, or the outcrop of a ledge, the miner's first work is to ascertain its value. He will dig an open cut to a depth of three or four feet, and chip fragments of quartz from the vein. These are as finely powdered as possible and panned out. It frequently happens that the ledge is some distance from water, and the powdered quartz must be carried through the undergrowth and over the hills, a mile or more, to the nearest stream.
    The amount of colors left in the residue will indicate the quantity of free gold carried in the vein. But it will do no more than that. It will not tell the whole story. Sometimes very rich quartz will not pan at all, the values being hidden in rebellious sulphides.
    To ascertain the value of base quartz, and where there is no assay office within a radius of many miles, the prospector becomes at once his own assayer. He pulverizes the quartz into a dust, and adds to it one-third as much gunpowder as there is pulverized ore. The whole is then mixed with water and made a thick paste. He shapes it into the form of a cone, and places it on a flat rock to dry. When dry the point of the cone is fired with a match, and the mass sputters and burns away till there is naught left but a small black and charred metallic button. A little polishing and scraping will satisfy the prospector as to the identity of the metal.

Northwest Mining Journal, August 1908, page 3



Gold Mining in Southern Oregon
By Arthur M. Geary
    The miner is again a factor in the material progress of Southern Oregon. The prospector, with his peculiar glint of eye and bulging pockets, is often seen on the streets of Medford and Ashland, where he comes for supplies or in search of financial backing in the promulgation of his projects. But boding more towards the development of the mineral wealth of the region than the presence of the prospector, who has always been somewhat in evidence in Southern Oregon, the eastern capitalist has become interested. Mining promoters whisper the names of noted mining men who are backing them in development of their properties. R. A. Towne and other New York capitalists have invested a million dollars in the improvement of the Blue Ledge copper mine, situated 35 miles from Medford. As soon as Hill builds his proposed railroad lines to tap the different districts, large quantities of eastern money will undoubtedly be spent in the development of other properties as well.
    The initiated know that Southern Oregon and the tributary district of Northern California have had a mining history. Men are yet alive who witnessed and took part in the mad struggle for gold which ensued in the '50s. The fact that on New Year's Day, 1852, the population of the Rogue River Valley numbered 28, and four months later totaled 1000, bears eloquent testimony of the genuineness of the gold rush in Southern Oregon. That $30,000,000 of gold was sent out of Jackson County between 1851 and 1883 testifies that the gold discovery in Southern Oregon was no false Eldorado.
    The mining of gold was a tremendous factor in the rapid settlement and development of Southern Oregon. Previous to 1852 trappers on fur-hunting expeditions and groups of travelers passing between California and Southern Oregon brought tales to the settlements of the meadows where grass grew as high as a mule's back, of the seeming fertility of soil, and of the superb climate. But the fear of the thieving Rogue River, Shasta and Klamath Indians, with their occasional massacre of the unwary traveler, struck terror into the hearts of the immigrants and caused them to choose homes in the safer precincts of the Willamette Valley.
    In the spring of 1851 there were only three habitations of white men in the Rogue River Valley. These were at Perkins', Long's and Evans' ferries on the Rogue River--Perkins' ferry being near the present site of Grants Pass. In the summer of '51 Governor Gaines, aroused to action by the reports of numerous murders and robberies committed by the Southern Oregon Indians, obtained federal aid in punishing them. United States soldiers and volunteers waged a short but effective campaign against the Rogue River chiefs known as Sam and Joe. In midsummer, following the campaign, a treaty was drawn, after which a few men took up donation claims in the region. [Geary seems here to be confabulating memories of the unwritten 1850 treaty with those of the 1853 Rogue River Indian War.] The first to arrive was Judge Alonzo A. Skinner, who had been appointed Indian Agent. He took a claim near Table Rock. [Other sources place his home between the sites of Central Point and Medford.] The Rogue River Valley, however, was too isolated to invite settlement for agricultural purposes. It necessitated the call of gold to attract white men into this dangerous and lonely valley.
    The discoverers of gold in Southern Oregon were James Cluggage and Poole. During the winter of 1851-52 they had driven their string of mules up Jackson Creek to fatten and condition them for packing in the spring. These men chose Jackson Creek for their pasture ground because it was off the beaten track. At this time Californians from Yreka were scouring the country in search of horse thieves, and it was safer for two men with a string of mules to be encamped in a secluded spot, as pursuers were nearly as lawless as [the] pursued. While encamped on Jackson Creek early in January 1852, these men discovered gold shimmering in the gravel of the creek bottom.
    The news of the strike spread rapidly to the partly exhausted gold fields of Northern California, and hordes of miners left their diggings to try their luck in New Eldorado. A steady stream of men poured into the Rogue River Valley, and spreading out from Jackson Creek, scattered throughout the surrounding hills. The inrush of people continued during 1853. In that year 150 wagons of immigrants, containing 400 men, 120 women and 170 children, and 2600 cattle, came north from California, and as many more arrived via Northern Oregon. The majority of the arrivals from California were miners, pure and simple, while those who came from the Willamette Valley saw possibilities in agriculture as well as in mining. Many of the Willamette Valley travelers devoted themselves wholly to farming, and found a lucrative market for their wheat and vegetables among the miners. The men who hurried from the California gold fields were of all nationalities and often of a lawless sort.
    After the first discovery of gold, fortunes were accumulated rapidly. Among the lucky ones was James Skinner, nephew of Judge A. A. Skinner, who mined a fortune within a week. "Old Man" Shively was another fortunate one. He gathered $50,000 worth of gold dust and left for civilization, heavily armed, determined to defend the fortune which he had acquired after a long life of prospecting.
    Rich strikes were reported on every hand. One hundred men were soon at work with rockers at Big Bar. Gravel rich in gold was found at the Cameron place on the Applegate. Forest Creek and Foots Creek were other districts where heavy-producing placers were soon being worked.
    The best evidence as to the amount of gold actually given up by mother earth is that furnished by C. C. Beekman, pioneer banker of Southern Oregon, who operated an express business between Yreka and Jacksonville during the early days. He carried $10,000,000 worth of gold dust out of Jackson County between 1856 and 1860, he believes, and an equal amount found other ways of exit.
    After 1856 the output of the mines decreased annually. Before 1860 the average amount mined every year was estimated at $1,250,000. In 1860 the mines produced $1,150,000, in 1870 two-thirds of that sum, and in 1880 less than $250,000. Between 1856 and 1880 there were 5438 mining locations filed upon. Of this number 16 were copper, one was tin, 124 were cinnabar (sulphide of mercury), and the rest gold and silver. In 1855 came Jackson County's maximum gold prosperity. That year it was said that gold dust to the value of $3,000,000 was mined. At that time Jackson County was the wealthiest and the most populous in Oregon, Multnomah County included.
    Jacksonville, whose essential claims upon life today are the rugged beauty of its scenery and that it is the county seat, was then in the height of its prosperity, with multitudinous saloons, and gambling dens galore.

Unidentified Oregon Mine, circa 1910
A water-powered arrastra at an unidentified Oregon mine, circa 1907

    Of the $30,000,000 mined in Jackson County between 1851 and 1884, only $500,000 was produced by quartz mines. Occasionally pockets of gold contained in decomposed quartz had been found on the surface of the ground, but previous to the breaking out of the quartz mining fever in California in 1859 the Jackson County miners had not explored quartz leads underground. The Hicks lead on the left fork of Jackson Creek was the first quartz lead successfully prospected. Sonora Hicks and her brother [sic--Sonora was apparently a man] discovered a rich pocket in this lead and, according to the seeming sensational news columns of the Jacksonville Sentinel, took out $1000 in gold in two hours. The total yield of this, the first quartz mine operated in Southern Oregon, totaled $2000, only one small pocket of gold being found.
    In January 1860, "Emigrant" Graham discovered the Gold Hill ledge, which was the first important quartz gold discovery. The float rock on the surface yielded astounding returns to Graham and his associates. The strike was the signal for a new outburst of mining enthusiasm. The surrounding hills were quickly staked out, and the outlying districts teemed with prospectors. Jacksonville, which of late years had not been so lively, prepared for the reversal of happy and prosperous times. Two mule-power arrastras were placed on the original claim, and armed men guarded while they were operated. It is said that every Saturday night a cleanup of 1000 ounces of gold was divided among the five owners. Henry Klippel, known as the father of quartz mining in Southern Oregon, bought an interest in the mine. Klippel, in company with McLoughlin and Williams, finally sent to San Francisco for a 12-stamp steam mill, taking a contract to work the quartz for $8 a ton. The machinery, including boiler and mortars, was shipped to Scottsburg and thence carried by pack train to Gold Hill. The freight charges on the mill amounted to $2600.
    With this, the first steam stamp mill of Southern Oregon, in operation, the owners felt that fortune would smile upon them indeed. One hundred tons of refuse quartz, which had been considered too poor for the arrastras, were first run through the mill, yielding $100 to the ton, but here the good luck ended.
    The next body of ore to be worked yielded $3 a ton, and the next $2.80. When all hope of success at the Gold Hill quartz mines was finally abandoned by the owners of the mill, the machinery was converted into a saw mill on Big Butte Creek. Henry Klippel estimated that the total output was $150,000. The Blackwell, Jewett, Swinden, McDonough, Schumpf, Johnson, Lyon, Peebler, Holman and Fowler quartz ledges were worked at this time with varying degrees of success. The Steamboat lode was perhaps the most productive of these quartz ledges. During 1860 and 1861 it yielded $280,000. These two years included the early quartz mining history of Southern Oregon. No great successes were gained after that period. The gold was too scattered in pockets, and methods were too primitive then to give lasting success to quartz mining, and it was abandoned for a number of years.
    Of late, renewed interest, however, has been taken in quartz mining. There are 52 quartz mines now in operation or in stages of development in the district, embracing Southern Oregon and Northern California.
    That many of the miners who rushed into Jackson County in the early '50s amassed fortunes the amount of gold sent out of the country bears witness, but that many, especially after the best strikes had been made, expended their energy in vain the thousands of little excavations scattered throughout the country and found scarring every hillside give evidence. As the supply of gold which could be mined according to the primitive methods of the day gave out, most of the miners went to other fields. The discovery of gold in Idaho caused a large exodus of miners [whose] absence was felt keenly for a time by the farmers and tradesmen whose customers they had been. The cattlemen, who with their herds inhabited the grassy plains of Klamath County, soon took the place of the miners who had departed, and the stagnation due to [the] oversupplied market was relieved.
    One race of foreigners which prospered where white men failed was the Chinese. Chinamen swarmed into the country, taking possession of the worn-out placers. By 1859 the yellow face of the Mongolian was everywhere in evidence. They were peaceful and law-abiding, but notwithstanding the usual racial prejudice sprang up among the disaffected miners. It was charged that the Chinamen were mining American gold and taking it to the Flowery Kingdom. As the Celestials were law-abiding and absolutely refused to quarrel, there was no pretext for exterminating them or driving them from the country, as there was in the case of the redskins. Finally, in 1859 the California method of treating them was adopted. A tax of $2 a month for miners and $50 a month for merchants was levied upon them under the caption of "Foreigners' Tax." [Oregon's "poll tax" on Chinese residents was instituted in 1857 by the state legislature. In 1859 it was extended to Hawaiians, in 1862 to "Negroes and mulattoes."] Even these stringent measures had but mediocre success in stemming the tide of Chinese immigration, as the tax was difficult to collect. The Chinese were satisfied if their mines would pay wages, and in their slow but sure way amassed what was to them a fortune and left for their native country. Gradually Yellow "John" has quit this field of enterprise, and few Chinese are seen today in the Rogue River Valley.
    Placer mining in Southern Oregon has gone through much the same stages as in California. First the Mexican batea, or an ordinary cone-shaped pan, was used by the miners. Then the rocker or cradle came into use. After this came the tom, an apparatus with cross riffles which permitted the play of a continual stream of water. Then sluice boxes were built across the claims where there was sufficient water. By this method miners could shovel gold-bearing gravel into running water from both sides. The gold in the gravel was caught on the quicksilver plates at the riffles.

Rocker, 1903 New Mexico
A rocker in use in New Mexico, 1903.

Long Tom circa 1852, California
A long tom circa 1852, California.

Sluicebox, Dakota Territory 1889
A sluice box in the Dakota Territory, 1889.
Sterling Mine circa 1900
Hydraulic mining at the Sterling Mine in Jackson County, circa 1900

    After the sluicebox, the hydraulic method was inaugurated. Water was conveyed through pipes to the workings at a high pressure and played upon the gold-bearing gravels. A whole hillside can be washed into sluiceboxes and the gold saved by this method.
    The greatest handicap to hydraulic mining in Southern Oregon has been the scarcity of water. Most of the mines can only be worked during the rainy season, as the majority of the smaller streams dry up in the summer. Projects have been proposed several times to bring water 50 or 70 miles to the mines from one or other of the large streams, but as yet none of them has materialized.
    The Jacksonville Sentinel, in 1859, referred to the possibilities of hydraulic power contained in the opening of artesian wells. The paper went on [to] show that the Rogue River made the proper bend at a high altitude and that the lower strata of ground were of the proper gravelly nature to ensure the presence of these artesian wells. However, only two artesian wells have been found. These are in the Talent orchard, where their limited flow of sparkling aqua is used in stimulating the growth of the celebrated Rogue River Valley [omission] bring a harvest as truly golden as placer mining.
    At present the Rogue River Canal Company is preparing to build 200 miles of ditches from the headwaters of Big Butte Creek. The water is for irrigating purposes, but there is no cause to prevent some of the flow being used in mining, as the highest ditch will run well back into the hills where the placers are situated.

Sterling Mine circa 1905
Sterling Mine, circa 1905

    The heaviest producer of the hydraulic placers of Southern Oregon has been the Sterling or Ankeny mine, on Sterling Creek, a few miles from Jacksonville. This mine is said to have produced from $25,000 to $60,000 every year for the last quarter century. The equipment consists of a 25-mile ditch, carrying 2500 miners' inches and supplying water for two and three giants nine months in the year. The mine includes 700 acres of deep red clay gravel deposit.
    There are many signs of awakening interest in mining throughout the coast. California, for the first time since 1897, has gained first place from Colorado as the foremost gold-producing state in the Union. The increased production of gold in California has been due to the development of dredge mining. Operations of this character are being started on Foots Creek in the [western] part of Jackson County.
    The possibilities of dredge mining in Southern Oregon, where many streams with rich channels abound, are just now beginning to be investigated.
    As a reaction from concentration of energy upon the exploitation of Oregon's horticulture possibilities, great effort is now being made toward the advertisement and development of Oregon's mineral wealth. Sumpter this year held its first mining congress--representative mining men coming from all parts of the district, which extends into Idaho. A meeting of miners of the Southern Oregon and Northern California districts has been called at Ashland for January 17. This getting together of mining men will mean much for the development of the mines of Oregon. The state miners' association, with L. D. Mahone as secretary, is showing unexpected life and is becoming a strong factor in putting mining upon a practical business basis.
    Gold is by no means the only mineral to be found in Southern Oregon. Quicksilver, coal and silver as well as copper mines are being developed. W. H. Jackson is developing the Mammoth quicksilver mine on the Rogue River, and cinnabar properties are also being opened on Evans Creek. A large body of coal has been found within five miles of Medford and is being sold for fuel. The coal will be of special value as fuel for the smelters of the Blue Ledge copper mines when railroad communications are built. Undeveloped deposits of lead, salt, coal and limestone exist in this region. Limestone for years was burned in kilns situated on Jackson Creek.
    Marble and granite quarries are being operated at Tolo and near Medford. The crushers at Tolo are able to turn out 50 carloads of crushed granite for use on roads every day when in full operation. This plant is equipped with air compressors, air drills and grinding and polishing machinery to furnish granite for building purposes and monumental work. Electric power generated at Gold Ray Dam, on the Rogue River, is used in this quarry.
    The tremendous water power now running unharnessed in the Rogue River, Big Butte Creek and other smaller streams will furnish all the power needed for the development of mining and quarrying for centuries to come.
    The mineral springs which are found scattered through Southern Oregon are another natural resource furnished by nature. Extensive bottling works are being operated at Wagner, Colestin and Shasta springs.
Opp Mine, 1909
Opp Mine, 1909

    That the mining industry of Southern Oregon will soon came into its own, not even a pessimist can deny. The mineral wealth which has heretofore lain secluded in the mountains will soon be reached by railroads. Then the capitalist machinery and advanced mining methods which have revolutionized mining will be given a chance.
    There is no rational ground for believing that the miners of the '50s could have uncovered so much treasure as they did and not leave untold wealth which their primitive methods and tools could not reach.
Medford Mail Tribune, February 5, 1911, page B1   This article was originally printed in the Sunday Oregonian of January 22, 1911, page 18.



Last revised February 26, 2014