The Manning Canyon Prospect #2 is a gold and arsenic mine located in Tooele county, Utah at an elevation of 6,801 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: 6,801 Feet (2,073 Meters)
Primary Mineral: Gold, Arsenic
Lat, Long: 40.31861, -112.18861
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.
Manning Canyon Prospect #2 MRDS details
Primary: Manning Canyon Prospect #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.
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: Silicification
Age Type: Host Rock
Age Young: Mississippian
Comment (Deposit): WALL ROCKS ARE HIGHLY DEFORMED AND ALTERED. MINERALIZATION IS CONTROLLED BY TRACTURES AND FISSURES.
Comment (Workings): PIT AND TRENCHES
Comment (Geology): LIMESTONES ARE DARK GREY TO BLACK, CHERTY, AND SILICIFIED. INTERCALATIONS OF SHALES ARE COMMON. HOST ROCKS ARE IMPREGNATED WITH VEINS OF QUARTZ AND CALCITE.
Comment (Location): INFO FROM LAND.ST :(1977)
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.