The Arizona sentinel., 1900-12-19
LA FORTUNA MINE.

In the early days of gold discovery of Califor- nia l64S when the news reached the gold miners of Sonora, there was a general exodus of the able-bodied men who were able to get away northwest to the new Fl Dorado in California and the state of Sonora contributed many men to the mining population. They took the old road, which was known as the ''camino real, '' from Estancia and Altar northwestward, nearly parallel to the gulf, following the mountain ridge known as the Gila range. just north of our present boundary. The road led to Yuma, and in passing the Gila range they went within a few feet or yards of a very modest outcrop of quartz which no one seemed to consider of sui icient value to merit any attention. That hum ble and insignificant quartz outcrop is today the outcrop Of the great Fortuna mine
 It is situated on the westward slope and nearly st the base of the range of mountains called on some of the old maps the Gila range. This trends northwesterly and reaches nearly to the Gila river at the point now known as Blaisdell The railway in its course to Yuma passes around the northwest point of this range. Where the rocks are exposed at that point they are mostly of homogeneous granite, of gray color and weathered out at the surfaces, which, however are much pitted as if by decompoSi- tion of some soft substance. But beyond these low-lying hills of granite there arc big outcropS of rock which to the experienced eye indicate stratifed formations. They are indeed strait fled, for the bulk of the range Southward and Southeastward is composed of regular strati3ed, laminated, hard gneiSsic rock. use the word "gneissic' in a very general and comprehensive sense, for you can describe these rocks with much more accuracy if you localize them as mica states and hornblendic states, with inter- polations of quartzite beds, especially in the upper part of the series, with green stains, SUD- posed to be stains of copper and decomposition of copper ore, which they probably are, al- though there are peculiaritieS of color, and some yellow colorS, which indicate to me the presence of some other mineral, possibly, tel lurium, which by it's decomposition has given these colors. The fact remains, however, that the bullion from the upper part of the vein con- tainS more copper than it now contains in the lower levels of the mine. The workings which have been carried on here have developed a condition of things which could not be foretold from an inspection of the outcrop. The vein or lode appears to be chimney, not continO ous ore body, nor a continuous vein witl an ore body or chimney or chute upon it. As re-
  there is no very great longitudinal extension oi this ore body.
 The vein is remarkable first in this limited out crop; second. in its continuity in depth, it's con tinued satisfactory richness, and the promise ii gives of enrichment by further veins dipping into it on the foot-wall sides.
 Some facts in regard to the product or yield The ore paid from the surface The product ol ore extracted up to the time has been about st tons per day which is sent to the 2Ostamp mill each stamp of which crushes about tons 1T every tweutyf0I- hours. The extraction i. chiefly ana largely by power drills. A fore, of So men is employed by this mine and mill The greater part Of the labor underground anC mining is done by compressed air The lode was told, was to 15 feet wide This larg' space permits the use of power drills to grea advantage. In the material hoiSted there ar fragments of the wall rocks, some of which ar thrown out. but many pieces pass through tn mill. They would prefer to reject most of thi wall rock but it would take more time and ex pensc than it does to mill it, and there is chance of some Of it containing gold. Fron these 80 tons of roc; crushed daily the averag' product is perhaps $4sO0O worth of gold pc month. Some months they have produced a high as S90,C00.
 Tn the region of the Fortuna mine the forma tionS appear to be wholly of mica slate an' horablende slate with some arenaceous layer Ike old micaccoul sandStoneS and quartZites The miEe is surrounded by black hOrnblendi states and mica states, dipping southwaTd an southwestward at an angle of about 45 degrees end these states are very evenly laminated ridge uFtel ridge. This k apparently coz