The Barneys Canyon Mine is a lead and zinc mine located in Salt Lake 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: Lead, Zinc
Lat, Long: 40.59333, -112.14694
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.
Barneys Canyon Mine MRDS details
Site Name
Primary: Barneys Canyon Mine
Commodity
Primary: Lead
Primary: Zinc
Secondary: Silver
Secondary: Copper
Tertiary: Iron
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
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: Colorado Plateaus
Physiographic Section: High Plateaus Of Utah
Physiographic Detail: Uinta Extension
Mineral Deposit Model
Not available
Orebody
Form: IRREGULAR
Structure
Type: R
Description: Basin And Range
Type: L
Description: Fissures, Fractures, And Folds
Alterations
Alteration Type: L
Alteration Text: Dolomitization And Silicification
Rocks
Name: Quartzite
Role: Host
Age Type: Host Rock
Age Young: Late Permian
Name: Quartzite
Role: Host
Age Type: Associated Rock Unit
Age Young: Eocene
Name: Quartzite
Role: Host
Age Type: Host Rock Unit
Age Young: Late Permian
Analytical Data
Not available
Materials
Ore: Sphalerite
Ore: Galena
Ore: Chalcopyrite
Ore: Limonite
Ore: Pyrite
Gangue: Barite
Gangue: Sericite
Gangue: Talc
Gangue: Calcite
Gangue: Chlorite
Comments
Comment (Location): INFO FROM LAND.ST :(1977)
Comment (Deposit): DEPOSIT LIES ON THE SOUTHERN LIMB OF AN OVERTURNED ANTICLINE. MINERALIZATION IS CONTROLLED BY FISSURES IN HIGHLY ALTERED WALLROCKS.
Comment (Workings): ONE TUNNEL, COLLAPSED AND INACCESSIBLE; MANY OTHER SMALL PITS AND TRENCHES.
Comment (Deposit): HOSTROCKS ARE DARK GRAY, WEATHERING TO A LIGHT BLUISH GRAY, SMOOTH SURFACED, FINE-GRAINED, LAMINATED LIMESTONES, WITH BANDS OF QUARTZITES. LENSES OF COARSE-GRAINED, WELL-ROUNDED QUARTZOSE SAND OR FINE-GRAINED SILT MAKES UP ABOUT 20% OF THE ROCK. INTRAFORMATIONAL BRECCIA AND CONTORTED LAMINATIONS ARE COMMON. ; INFO.SRC : 1 PUB LIT; 3 FIELD OBSERV
Comment (Geology): ORE MINERALS ARE INTIMATELY ASSOCIATED WITH QUARTZ OCCURRING AS VEINS IN THE ALTERED WALLROCKS.
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 HE 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.
The Top Ten Gold Producing States
These ten states contributed the most to the gold production that built the West from 1848 through the 1930s. The Top Ten Gold Producing States.
