The Mercur Mine #2 is a gold mine located in Tooele county, Utah at an elevation of 6,841 feet.
About the MRDS Data:
All mine locations were obtained from the USGS Mineral Resources Data System. The locations and other information in this database have not been verified for accuracy. It should be assumed that all mines are on private property.
Elevation: 6,841 Feet (2,085 Meters)
Primary Mineral: Gold
Lat, Long: 40.3275, -112.20667
Map: View on Google Maps
MRDS mine locations are often very general, and in some cases are incorrect. Some mine remains have been covered or removed by modern industrial activity or by development of things like housing. The satellite view offers a quick glimpse as to whether the MRDS location corresponds to visible mine remains.
Mercur Mine #2 MRDS details
Primary: Mercur Mine #2
District: Mercur District
Land ownership: Private
Note: the land ownership field only identifies whether the area the mine is in is generally on public lands like Forest Service or BLM land, or if it is in an area that is generally private property. It does not definitively identify property status, nor does it indicate claim status or whether an area is open to prospecting. Always respect private property.
Owner Name: Getty Oil Co.
Record Type: Site
Operation Category: Past Producer
Operation Type: Unknown
Discovery Method: Ore-Mineral In Place
Years of Production:
Deposit Size: S
General Physiographic Area: Intermontane Plateaus
Physiographic Province: Basin And Range Province
Physiographic Section: Great Basin
Physiographic Detail: Uinta Extension
Mineral Deposit Model
Alteration Type: L
Alteration Text: Dolmitization, Sericitization, Kaolimization And Silicification
Age Type: Host Rock
Age Young: Mississippian
Comment (Location): INFO FROM LAND.ST :(1977)
Comment (Deposit): MINERALIZATION IS CONTROLLED BY FRACTURES AND FISSURES IN ALTERED WALLROCKS.
Comment (Workings): TWO PITS OF 120X100X8 AND 120X30X5 FT. SIZE; ONE TRENCH OF 150X10FT. SIZES ONE SMALL ADIT, CAVED AND INACCESSIBLE.
Comment (Geology): WALLROCKS ARE HIGHLY DEFORMED AND ALTERED. LIMESTONES ARE DARK GRAY TO BLACK, FRACTURED, DOLOMITIZED, AND SILICIFIED. SHALES ARE GREENISH GRAY TO BLACK, PULVERIZED, SERICITIC, KAOLIMITIC, AND CARBONACEOUS. LIMONITIC STAINS ARE COMMON ON WALLROCKS.
Reference (Deposit): BISSELL, H.J., ET. AL., 1959, GUIDEBOOK TO THE GEOLOGY OF UTAH, NO. 14, UT. GEOL. SOC.: U.G.M.S. BULL.14,262P.
Reference (Deposit): GILLULY, J., 1932, GEOLGOY AND ORE DEPOSITS OF THE STOCKTON AND FAIRFIELD QUADRANGLES:U.S.G.S. PROF. PA.173,167P.
Reference (Deposit): BUTTLER, B.S., ER,. AL.,1920, THE ORE DEPOSITS OF UTAH: U.S.G.S. PROF. PA. 111, 672P.
Reference (Deposit): SPURR, J.E., 1895, ECONOMIC GEOLOGY OF THE MERCUR MINING DISTRICT, UTAH: U.S.G.S. 16TH. ANN. REPT.,PT.2,454P.