The Middle Canyon Mines is a lead and zinc mine located in Tooele county, Utah at an elevation of 6,719 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: 6,719 Feet (2,048 Meters)
Commodity: Lead, Zinc
Lat, Long: 40.50722, -112.20806
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.
Middle Canyon Mines MRDS details
Site Name
Primary: Middle Canyon Mines
Commodity
Primary: Lead
Primary: Zinc
Secondary: Silver
Secondary: Copper
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
Structure
Type: R
Description: Basin And Range
Type: L
Description: Fissures, Fractures, Faults, And Folds
Alterations
Alteration Type: L
Alteration Text: Dolomitzation 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: Sphalerite
Gangue: Quartz
Gangue: Gypsum
Gangue: Calcite
Gangue: Sericite
Gangue: Chlorite
Gangue: Talc
Comments
Comment (Geology): LIMESTONE IS DARK GRAY TO BLACK, WEATHERING LIGHT GRAY BLUE WITH A SMOOTH SURFACE, VERY FINE-GRAINED, THIN BEDDED TO PLATY, WITH SOME SILT STRINGERS AND SMALL 1/2" TO 1" DIAMETER BLACK ROUNDED GLOBULAR CHERT NODULES. QUARTZ AND CALCITE VEINS ARE COMMON.
Comment (Deposit): DEPOSIT LIES CLOSE TO A FAULT PLANE. MINERALIZATION IS CONTROLLED BY FISSURES. HOSTROCKS ARE SHEARED AND ALTERED. ORE MINERALS ARE ASSOCIATED WITH QUARTZ VEINS
Comment (Workings): TWO ADITS; CAVED AND INACCESSIBLE.
Comment (Location): INFO FROM LAND.ST :(1977); 1:24000 QUADRANGLE IS A 1975 EDITION
References
Reference (Deposit): BOUTWELL, J.M., 1905, ECONOMIC GEOLOGY OF THE BINGHAM MINING DISTRICT, UTAH: USGS P.P. 38, 410P.
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 OF UTAH, NO, 16 UTAH GEOLOGICAL SOCIETY, 145P.
Reference (Deposit): BUTLER, B.S., ET. AL., 1920, THE ORE DEPOSITS OF UTAH: USGS P.P. III. 672P.
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