The Bates Canyon Mine is a lead, zinc, copper, and iron mine located in Tooele county, Utah at an elevation of 5,459 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: 5,459 Feet (1,664 Meters)
Commodity: Lead, Zinc, Copper, Iron
Lat, Long: 40.62278, -112.23833
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.
Bates Canyon Mine MRDS details
Site Name
Primary: Bates Canyon Mine
Commodity
Primary: Lead
Primary: Zinc
Primary: Copper
Primary: Iron
Location
State: Utah
County: Tooele
District: Bingham 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
Not available
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
Form: IRREGULAR
Structure
Type: R
Description: Basin And Range
Type: L
Description: Faults, Fissures, Fractures And Folds
Alterations
Alteration Type: L
Alteration Text: Dolomitization, Sericitization And Silicification
Rocks
Name: Quartzite
Role: Host
Age Type: Host Rock Unit
Age Young: Pennsylvanian
Name: Quartzite
Role: Host
Age Type: Host Rock
Age Young: Pennsylvanian
Analytical Data
Not available
Materials
Ore: Galena
Ore: Chalcopyrite
Ore: Pyrite
Ore: Sphalerite
Gangue: Talc
Gangue: Sericite
Gangue: Calcite
Gangue: Chlorite
Comments
Comment (Location): INFO FROM LAND.ST :(1977)
Comment (Deposit): DEPOSIT IS LOCATED IN BRECCIATED, AND HIGHLY ALTERED HOSTROCKS
Comment (Workings): TWO TUNNELS, CAVED AND INACCESSIBLE.
Comment (Geology): THE MINERALIZATION IS CONTROLLED BY FISSURES AND FRACTURES. ORE MINERALS ARE INTIMATELY ASSOCIATED WITH CRYPTOCRYSTALLINE SILICA; VEINS OF CALCITE AND QUARTZ ARE COMMON IN WALLROCKS
Comment (Deposit): THE DEPOSIT LIES IN AN AREA CLOSE TO THE NORTH OQUIRRH THRUST ZONE. ; INFO.SRC : 1 PUB LIT; 3 FIELD OBSERV
References
Reference (Deposit): BRAY, E.R., WILSON J.C., 1975, GUIDE BOOK TO THE BINGHAM MINING DISTRICT: SOCIETY OF ECONOMIC GEOLOGISTS
Reference (Deposit): COOK, D.R., 1961, GEOLOGY OF THE BINGHAM MINING DISTRICT AND NORTHERN OQUIRRH MOUNTAIN, GUIDE BOOK TO THE GEOLOGY REFERENCE 3
Reference (Deposit): BUTLER, B.S., ET. AL., 1920, THE ORE DEPOSITS OF UTAH: USGS P.P. 111, 672P.
Reference (Deposit): BOUTWELL, J.M., 1905, ECONOMIC GEOLOGY OF THE BINGHAM MINING DISTRICT, UTAH: USGS P.P. 38, 410P.
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