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Wisconsin Mine | |
Alternate NamesBuckthorn Mining District and MinesGreaterville District USBM: Historical: Shallow shafts and tunnel. Adit 50 ft. long with stope to surface, and several shafts (about 20 feet deep) and surface prospects.1 Historical: The Wisconsin mine is 1.2 miles northwest of Greaterville, on an iron-stained quartz vein 1 foot wide, in granite near overlying siliceous shale and dolomitic beds on the east. The vein dips 45° SW. It is opened by a number of shallow shafts and contains, from the surface down, pyrite and galena, which at a depth of about 30 feet becomes plentiful and carry workable quantities of silver and a little gold. Some of the surface ore is said to have run $5 to the ton in gold and silver.2 A former small underground Ag-Cu-Pb-Au mine located in East-central sec. 14, T.19S., R.15E., 1.2 miles NW of Greaterville, and 37 miles SE of Tucson. Produced 1880-1937. Owned by Pallanes. Operated by J.B. Daugherty.3 LocationLatitude & Longitude (WGS84):31° 47' 0'' North , 110° 46' 27'' West4 E. cent. sec. 14, T. 19 S., R. 15 E.1 31.78374N, -110.77485W1 Mineral ProductsUSBM: samples 131 - 135. Ag 5 - 250 ppm, Au <5 - 706 ppb, Cr 390 - 780 ppm, Cu 85 - 1,020 ppm, Pb 248 - 7856 ppm. Also SR131 Mn 8035 ppm, SR132 Sb 633 ppm, SR134 751 ppm1. Chalcopyrite, Galena, Gold, Pyrite.3 GeologyFissure and stockwork quartz vein. Vein is massive to splaying stringers of quartz, heavily iron oxide stained with chalcopyrite, pyrite and galena 1. Mineralization is a tabular ore body with partially oxidized sulfides with free gold in an oxidized zone in an iron-stained quartz vein cutting Precambrian granodiorite near overlying siliceous shale and dolomitic beds on the east. The vein is 0.3 meters wide, strikes NW-SE and dips 45ºSW. An associated rock unit is Precambrian granodiorite at 1450 ± 10 MY. Type of Operation and ProductionWorkings include several shallow shafts, an incline and a tunnel. Worked in the late 1880's and 1936-1937, producing a small tonnage of Au, Ag, Pb & Cu ore.3 References
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