Gold prospects in the Granite Wash Mountains were first discovered in the 1860's but there was little active mining until after completion of the railroad in the early 1900's. Other periods of activity included the 1930's, 1940's and the 1950's when there was active exploration for the production of tungsten. the largest mine in the area is the Yuma Mine with recorded production of 8,600 tons @ 2.3~ Cu, 0.3 oz Ag, and .03 oz Au/T. Recorded metal production from the entire Granite Wash Mountains includes several thousand units of tungsten and several hundred to one thousand tons of ore each from the Glory Hole, Dandy, Desert Queen and True Blue Mines, averaging .40 to .60 oz Au/T. During the copper boom of the 1960's and 1970's both Bear Creek and Tenneco reportedly examined the Yuma Copper Mine and may have drilled a hole or two in its vicinity. Oliver Kilroy has held a major land position in the area for almost 20 years, has carried out extensive geophysical surveys, and has drilled fifteen holes for copper
mineralization with negative results. Exploration activity that presumably was directed toward gold mineralization during the 1980's has included dozing and
trenching by Bill Baker at the True Blue Mine, and by Charles Willmore at the Pandora's Box and Dandy prospects in Secs 6 and 7, T5N, RI4W. The Dona Kay prospect
in Secs 12 and 13, T5N, RI5W was drilled by Baroque Resources and Weaco in 1985 and five or six rotary holes were drilled on the major low-angle fault and
associated veins at the Three Musketeers tungsten property in SW% of Sec 24, T7N, RI5W. Most of the land in the area is Federal, administered by the ~ and old
claim posts run rampant through the mountains and over the adjacent alluvial covered pediment. The only active mine in the District is the Yuma Mine where
Donald Nelson is mining gem quality azurite and malachite.
1. Dona Kay/OroFino/Mineral Hill Mine
- Cu, Ag, Au
-Copper, silver, and Au mineralization, with quartz gangue in an irregular deposit in a fissure zone in a thin sequence of lithic sandstone member of the
McCoy Mountains Formation and in large, overlying and underlying diorite-andesite bodies. -Keith (1978, p. 148), geologic update by this study