The Arizona sentinel., 1902-04-16
LA FORTUNA MINE.

Tn the early days of gold discovery Of Califor- pia 1s4s 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 Jidge known as the Gila range. just north of our present boundary The road led to Yuma, and fa passing the CIila range u e. went within few feet or yards of a very modest outcrop of quartz which no one seemed to consider of sui ficient value to merit any attention. That hum. ble and insignificant quartz ou5crop is today the oGtcrop of the great Fortuna mine
 IL is situated on the westward slope and nearly Rt 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 Blaisdejl. The railway in it's course to Yuma passes around the northwest poiat of this range. Where the rocks are exposed at that point they are mostly of homogeneous granite. Of gray color and weatheTed out at the surfaces which, how.ver are much pitted as if by deconpoSi- ton of some soft substance. But beyond these low-lying hills of granite there are big outcrops of rock which to the experienced eye indicate Stratiied formations They are indeed strait fled. for the bulk of the range SOuthward and southeaStward IS composed of regular Stratifed. 1amlnated, hard GnelSSlc rock. use the word ''gneisSic' in a very general and comprehensive sense for you can describe tEeSe rocks with much more accuracy if you localile them as
 
 polationS of quartZite beds, especially in the upper part of the series with green stains sup 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 its decomposition has given these colorS. The fact remains, however that the bullion from the upper part of the vein con tains more copper than 1t now contains in the lower levels of the mine. The workings which have been carried on here have developed condition of things which could not be fOretold from an inspection of the ouJcrop. The vein CT lode appears to be chimney, not contino- ous ore body, nor continuous vein with an ore body or chimney or chute upon it. As re- marked the outcropping points indicate that there IS no very great longitudinal extension Of this ore body.
 The vein is remarkable first in this limited out crop; second in its continuity in depth, it's con- tinuee satisfactory richness, and the promise it 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 or ore extracted up to the time has been about so tons per day, which is sent to the 20-Stamp mill, each stamp of which cruShcS about tons in every twentyfour hours. The extraction is chiefly and largely by power drills force of so men is employed by this mine and mill. The greater part Of the labor underground and mining is done by compressed air. The lode. told, was to l5 feet wide. This large space permits the use of power drills to great advantage. In the material hoiSted there arc fragments of the wall rocks, some of which are thrown out, but many pieces pass through the mill They would prefer to reject most of this wall rock. but it would take more time and ex penSe than it does to mill it, and there is a chance of some of it containing gold. From these 30 tons of rock crushed daily the average product is perhaps S4S000 worth of gold pel month. Some months they have produced a. high as S99000.
 In the region of the Fortuna mine the forma tiOns appear to be wholly of mica slate aD( hOrnblende slate. with some arenaceouS layer Ike old micaceouS SandStoneS and QuartZites The mine is surrounded by black hOrnblendi states and mica states, dipping SOuthward ant southwestward at an angle of about 45 degrees and these states are very evenly laminated ridge after ridge.