The Copper Hill Prospect is a copper mine located in Juab county, Utah at an elevation of 5,479 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: 5,479 Feet (1,670 Meters)
Commodity: Copper
Lat, Long: 39.82833, -112.91722
Map: View on Google Maps
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Copper Hill Prospect MRDS details
Site Name
Primary: Copper Hill Prospect
Commodity
Primary: Copper
Location
State: Utah
County: Juab
District: Keg Mountain Area
Land Status
Not available
Holdings
Not available
Workings
Not available
Ownership
Owner Name: Prospect Lies Within The Holdings Of Robert And Terry Steele
Production
Not available
Deposit
Record Type: Site
Operation Category: Occurrence
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: Keg Mountains
Mineral Deposit Model
Not available
Orebody
Not available
Structure
Type: R
Description: Deep Creek-Tintic District Mineral Belt
Type: L
Description: Thrust Fault Just Below Prospect, Numerous Fractures, High-Angle, Ne-Striking Fault To East
Alterations
Alteration Type: L
Alteration Text: Oxidation
Rocks
Name: Diorite
Role: Associated
Age Type: Host Rock
Age Young: Late Cambrian
Analytical Data
Analytical Data: A SAMPLE OF FRACTURED QUARTZITE CONTAINING CHALCOPYRITE PODS CONTAINED 26 PPB AU 7.1 PPM SB, 108 PPM AS, 220 PPM BA, 230 PPM CR, 27 PPM CO, 10.0 % FE, 13 PPM MO, <50 PPM NI, <5 PPM AG, <2 PPM W, 17.0 PPM U, <200 PPM ZN, 11.05 %CU, 195 PPM PB, <1 PPM BI
Materials
Ore: Chalcopyrite
Ore: Covellite
Ore: Malachite
Gangue: Limonite
Gangue: Hematite
Gangue: Quartz
Comments
Comment (Commodity): ANALYSES SHOW THAT THE PROSPECT CONTAINS MUCH COPPER BUT LITTLE OF ANYTHING ELSE
Comment (Deposit): CHALCOPYRITE OCCURES AS PODS REPLACING QUARTZITE LOCALIZED ALONG FRACTURES STRIKING N50 W, 80 SW. DEPOSIT LIES IMMEDIATELY ABOVE A THRUST FAULT AND NEAR A NE STRIKING HIGH-ANGLE FAULT.
Comment (Workings): WORKINGS CONSIST OF A VERY SMALL PROSPECT PIT.
References
Reference (Deposit): SHUBAT, M.A., 1987, GEOLOGY AND MINERAL OCCURRENCES OF NORTHERN KEG MOUNTAIN, JUAB COUNTY, UTAH, IN KOPP, R.S., AND COHENOUR, R.E., EDS., CENOZOIC GEOLOGY OF WESTERN UTAH: UTAH GEOLOGICAL ASSOCIATION PUBLICATION 16, P. 451-462.
Reference (Deposit): MORRIS, H.T., 1978, UNPROSPECTED ZONE OF PYRITIC ALTERATION IN WEST-CENTRAL UTAH: U.S. GEOLOGICAL SURVEY OPEN-FILE REPORT 78-791.
Reference (Deposit): MORRIS, H.T., 1987, PRELIMINARY GEOLOGIC MAP OF THE DELTA 2 DEGREE QUADRANGLE, TOOELE, JUAB, MILLARD, AND UTAH COUNTIES, UTAH: U.S. GEOLOGICAL SURVEY OPEN-FILE REPORT 87-185.
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