The Arizona sentinel., 1900-11-07
LA FORTUNA MINE.

In the early days of gold discovery of Califor- nia Is4s, when the news reached the gold miners of Sonora, there was a general exodus cf the able-bodied men who were able to get away northwest to the new El 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 few feet or yards of a very modest outcrop of quartz which no one seemed to consider of sui fcient 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 at the base of the range of mountains called on some of the old maps the Gila range. This trends north westerly and reaches nearly to the Gila river at the point now known as Blaisden. 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 nlEcs pitted as if by decomposi- tion 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 fed for the bulk of the range southward and southeastward is composed of regular stratifed, 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 Slates, 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 lUTiuIn. which by it's decomposition has given these coloTS. 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 a chimney, not contino- ous ore body, nor a 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 it's continuity in depth it's con- tinued satisfactory richness, and the promise il 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 80 tons per day, which is sent to the 2Ostamp mill each stamp of which crushes about 1 tons in every twentyfour hours. The extraction is chiefly and largely by power drills. A 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, was 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 arc thrown out, but many pieces pass through tho 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 chance Of some of it containing gold. Fron these 80 tons of rock crushed daily the averag, product is perhaps S4s,OOO worth of gold pc month. Some months they have produced a. high as S90,00O.
 In the region of the Fortuna mine the forma tions appear to be wholly of mica slate anC hornblende slate, with some arenaceouS layer Ike old micaceouS sandstones and quartzites The mine is surrounded by black hornblend slates and mica states, dipping southward anC southwestward at an angle of about 45 degrees and these slates are very evenly laminated ridge after ridge. This is apparently con