The Manning Canyon Mine #3 is a gold mine located in Tooele county, Utah at an elevation of 7,001 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.
Mine Info
Elevation: 7,001 Feet (2,134 Meters)
Commodity: Gold
Lat, Long: 40.32278, -112.19750
Map: View on Google Maps
Satelite View
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 Mine #3 MRDS details
Site Name
Primary: Manning Canyon Mine #3
Commodity
Primary: Gold
Secondary: Mercury
Secondary: Antimony
Secondary: Arsenic
Secondary: Silver
Tertiary: Iron
Location
State: Utah
County: Tooele
District: Mercur District
Land Status
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.
Holdings
Not available
Workings
Not available
Ownership
Owner Name: Getty Oil Co.
Production
Not available
Deposit
Record Type: Site
Operation Category: Past Producer
Operation Type: Unknown
Discovery Method: Ore-Mineral In Place
Years of Production:
Organization:
Significant: N
Deposit Size: S
Physiography
General Physiographic Area: Intermontane Plateaus
Physiographic Province: Basin And Range Province
Physiographic Section: Great Basin
Physiographic Detail: Uinta Extension
Mineral Deposit Model
Not available
Orebody
Form: IRREGULAR
Structure
Type: R
Description: Basin And Range
Type: L
Description: Fissures And Fractures
Alterations
Alteration Type: L
Alteration Text: Dolomitization And Silicification
Rocks
Name: Limestone
Role: Host
Age Type: Host Rock
Age Young: Mississippian
Analytical Data
Not available
Materials
Ore: Orpiment
Ore: Stibnite
Ore: Pyrite
Ore: Cinnabar
Ore: Limonite
Ore: Realgar
Gangue: Chlorite
Gangue: Talc
Gangue: Sericite
Gangue: Quartz
Gangue: Calcite
Comments
Comment (Deposit): WALLROCKS ARE HIGHLY DEFORMED AND ALTERED. MINERALIZATION IS CONTROLLED BY FRACTURES AND FISSURES. ORE MINERALS ARE ASSOCIATED WITH QUARTZ VEINS.
Comment (Location): INFO FROM LAND.ST :(1977)
Comment (Workings): THREE PITS OF 50X70X15, 50X60X10, AND 30X20X8 FEET SIZE; ONE TRENCH OF 120X15 FEET SIZE; AND OTHER SMALL PITS.
Comment (Production): PRODUCTION FIGURES ARE NOT AVAILABLE
Comment (Geology): LIMESTONES ARE GRAY, CHERTY, DOLOMITIZED AND SILICIFIED. LIMONITIC STAINS ARE VERY COMMON. SHALES OCCUR AS PULVERIZED INTERBEDDINGS IN LIMESTONES. THEY ARE CALCAREOUS, CARBONACEOUS, SERICITIC AND KAOLIMITIC.
References
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. PRO. 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.
Reference (Production): MOHAMMAD, H., 1981, ON SITE INVESTIGATION:U.G.M.S.
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