The Mercur Prospect #5 is a gold mine located in Tooele county, Utah at an elevation of 7,041 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: 7,041 Feet (2,146 Meters)
Primary Mineral: Gold
Lat, Long: 40.32889, -112.19722
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 Prospect #5 MRDS details
Primary: Mercur Prospect #5
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.
Record Type: Site
Operation Category: Occurrence
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
Description: Basin And Range
Description: Fissures And Fractures
Alteration Type: L
Alteration Text: Dolomitization And Silicification
Age Type: Host Rock
Age Young: Mississippian
Age Type: Host Rock Unit
Age Young: Mississippian
Comment (Location): INFO FROM LAND.ST :(1977)
Comment (Deposit): MINERALIZATION IS CONTROLLED BY FRACTURES AND FISSURES IN ALTERED WALLROCKS.
Comment (Workings): PIT AND TRENCHES
Comment (Geology): LIMESTONES ARE BRECCIATED, DOLOMITIZED AND SILICIFIED. SHALES ARE PULVERIZED, SLIGHTLY SERICITIZED, CARBONACEOUS AND CALCAREOUS. LIMONITIC STEINS ARE COMMON ON HOSTROCKS
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, GEOLOGY AND ORE DEPOSITS OF THE STOCKTON AND FAIRFIELD QUADRANGLES:U.S.G.S. PROF. PA.173,167P.
Reference (Deposit): BUTTLER, B.S., ET. 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.