The Highland Boy is a copper 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: Copper
Lat, Long: 40.51528, -112.16722
Map: View on Google Maps
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Highland Boy MRDS details
Site Name
Primary: Highland Boy
Secondary: Utah - Apex
Secondary: Utah Consolidated Mining Company
Commodity
Primary: Copper
Secondary: Lead
Secondary: Silver
Secondary: Gold
Location
State: Utah
County: Salt Lake
District: Bingham District
Land Status
Not available
Holdings
Not available
Workings
Not available
Ownership
Owner Name: Anaconda Co.
Production
Not available
Deposit
Record Type: Site
Operation Category: Producer
Operation Type: Unknown
Year First Production: 1896
Discovery Year: 1873
Discovery Method: Ore-Mineral In Place
Years of Production:
Organization:
Significant: N
Physiography
Not available
Mineral Deposit Model
Not available
Orebody
Form: THREE WELL - DEFINED LENSES
Structure
Type: L
Description: Limestone (N 45 - 80 E, 25 - 55 N), Fissures (N 85 E; N 85 W; N 30 - 45 W; N - S), Slip Planes (N - Ne, 90 ; E - Ne, 45 N)
Alterations
Alteration Type: L
Alteration Text: Oxidation To A Depth Of 300 Ft
Rocks
Name: Monzonite
Role: Associated
Age Type: Associated Rock
Age Young: Pliocene
Name: Monzonite
Role: Associated
Age Type: Host Rock
Age Young: Pennsylvanian
Analytical Data
Analytical Data: WHITE LS: 43.4 % SIO2 , 1.31 % MGO, 45.52 % CAO, 0.23 % H2O, 8.28 % CO2
Analytical Data: 1900'S : 12 % CU, $4 AU, 3 % AG. CHEMICAL ANALYSIS IN 1905 : GREY LS: 4.87 % SIO2 , 0.3 % AL2O3, 0.99 % MGO, 53.50 % CAO, 39.32 % CO2
Materials
Ore: Enargite
Ore: Chalcanthite
Ore: Chalcopyrite
Ore: Specularite
Ore: Limonite
Ore: Chalcocite
Ore: Bornite
Ore: Marcasite
Ore: Pyrite
Ore: Galena
Gangue: Serpentine
Gangue: Quartz
Gangue: Olivine
Gangue: Tremolite
Gangue: Calcite
Comments
Comment (Geology): GEOL.DESC: THE ORE DIP AND STRIKE ALMOST PARALLEL TO THE BEDDING. UNDERLYING THE LIMESTONE IS QUARTZITE AND OVERLYING THE ORE BODIES IS A BARREN BED OF MARBLE OR SILICIFIED LIMESTONE.
Comment (Production): FROM 1,000,000 TONS ORE
Comment (Development): DEEPER PARTS (SKARN ZONE) WILL BE REOPENED IN 1980 AS PART OF THE CARR FORK MINE (FOR MORE DETAILS, LOOK UP THE MINE)
Comment (Workings): WORKINGS IN 1905 CONSIST OF FIVE TUNNELS FROM 725 TO 1,900 FT LONG. A 12,600 FT TRAMWAY WAS BUILD TO TRANSPORT ORE TO SANDY. NEAR TOOELE, UTAH.
Comment (Deposit): THE LENSES SHOW A MASSIVE BEDDED STRUCTURE. THE REPLACEMENT SHOOTS ARE IN CARBONATES IN THE UPPER PARTS OF THE MINE. SKARN ORE ARE NEAR THE INTRUSIVE CONTACT AT DEPTH; PYRITIFEROUS COPPER ORE ASSOCIATED WITH PORPHYRITIC IGNEOUS ROCK.
Comment (Location): CONSOLIDATED IN 1896 BY THE UTAH CONSOLIDATED MINING CO. AND IN 1901 AS THE UTAH - APEX WITH THE RED WING MINE. THE MINE TODAY IS EXCAVATED BY THE BINGHAM OPEN PIT.
Comment (Commodity): THE CHALCOPYRITE IS TARNISHED AND COATED WITH BORNITE AND SEAMED WITH LIMONITE.
References
Reference (Deposit): USGS BULL. 213, 1902, P. 108.
Reference (Deposit): USGS BULL. 260, 1904, P. 238.
Reference (Deposit): 3A) USGS PROF PAPER 38 , P. 264 .
Reference (Deposit): 3B) USGS MIN. RES. 1916 - 1924 .
Reference (Deposit): CONSV. DIV. COMP. DATE, 05-12-1965
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