The Venice Tunnel is a lead mine located in Salt Lake county, Utah at an elevation of 7,999 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: 7,999 Feet (2,438 Meters)
Commodity: Lead
Lat, Long: 40.52472, -112.17444
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.
Venice Tunnel MRDS details
Site Name
Primary: Venice Tunnel
Commodity
Primary: Lead
Location
State: Utah
County: Salt Lake
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
Type: Underground
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: Colorado Plateaus
Physiographic Section: High Plateaus Of Utah
Physiographic Detail: Uinta Extension
Mineral Deposit Model
Not available
Orebody
Form: LENSE
Structure
Type: R
Description: Basin And Range
Type: L
Description: Fissures, Fractures And Faults
Alterations
Alteration Type: L
Alteration Text: Dolomitization And Silicification
Rocks
Name: Quartz Monzonite
Role: Associated
Age Type: Host Rock
Age Young: Pennsylvanian
Name: Quartz Monzonite
Role: Associated
Age Type: Host Rock Unit
Age Young: Pennsylvanian
Name: Quartz Monzonite
Role: Associated
Age Type: Associated Rock
Age Young: Pliocene
Analytical Data
Not available
Materials
Ore: Galena
Gangue: Orthoclase
Gangue: Quartz
Gangue: Garnet
Gangue: Rhodochrosite
Gangue: Barite
Comments
Comment (Location): INFO FROM LAND.ST :(1977)
Comment (Geology): THE COUNTRY ROCK IS MADE UP OF QUARTZITES AND GRAY IN PURE ARGILLACEOUS LIMESTONE. THE HANGING WALL IS QUARTZITE AND FOOT WALL IS LIMESTONE.
Comment (Deposit): DEPOSIT LIES IN THE BRECCIATED AND ALTERED WALLROCKS, VERY CLOSE TO PARNELL LODE AND ZONE OF CROSS-FAULTING
Comment (Workings): TWO ADITS 150 AND 300 FT LONG
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 OF UTAH, NO. 16 UTAH GEOLOGICAL SOCIETY, 145P.
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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