The Iron Mine is a lead and silver mine located in Tooele county, Utah at an elevation of 8,399 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: 8,399 Feet (2,560 Meters)
Commodity: Lead, Silver
Lat, Long: 40.36139, -112.24167
Map: View on Google Maps
Satelite View
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Iron Mine MRDS details
Site Name
Primary: Iron Mine
Commodity
Primary: Lead
Primary: Silver
Secondary: Gold
Tertiary: Copper
Location
State: Utah
County: Tooele
District: Ophir District; Lion Hill Area
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
Year First Production: 1916
Year Last Production: 1936
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, And Folds
Alterations
Alteration Type: L
Alteration Text: Dolomitization And Silicification
Rocks
Name: Diorite
Role: Associated
Age Type: Associated Rock
Age Young: Pliocene
Name: Diorite
Role: Associated
Age Type: Associated Rock Unit
Age Young: Pliocene
Name: Diorite
Role: Associated
Age Type: Host Rock
Age Young: Mississippian
Analytical Data
Not available
Materials
Ore: Plumbojarosite
Ore: Gold
Ore: Cerargyrite
Gangue: Gypsum
Gangue: Calcite
Gangue: Talc
Gangue: Sericite
Gangue: Chlorite
Gangue: Barite
Comments
Comment (Location): INFO FROM LAND.ST :(1977)
Comment (Production): PRODUCTION FIGURES ARE NOT AVAILABLE
Comment (Deposit): MINERALIZED ZONE LIES JUST BELOW THE LONG TRAIL SHALE MEMBER, IN THE LOWER PART OF THE 'GREAT BLUE' LIMESTONES, ON THE EASTERN FLANK OF THE OPHIR ANTICLINE. THE ORE DEPOSIT OCCURS IN OR CLOSELY ASSOCIATED WITH THE JASPEROID. THE JASPEROID LIES IMMEDIATELY BENEATH A SILL OF 'BIRD EYE PORPHYRY'. THE ORE FOLLOWED IRREGULARLY THE NORTH-EASTERLY FISSURES IN THE JASPEROID. THE ORE IS PRACTICALLY ALL OXIDIZED. ; INFO.SRC : 1 PUB LIT; 3 FIELD OBSERV
Comment (Deposit): ORE ZONES ARE LOCALIZED IN FISSURES WITH QUARTZ FILLINGS, IN DEFORMED AND HIGHLY ALTERED WALLROCKS; ORE IS COMPLETELY OXIDIZED
Comment (Workings): ADITS AND DRIFTS; ALL CAVED AND INACCESSIBLE.
Comment (Geology): WALLROCKS ARE DEFORMED AND ALTERED. LIMESTONES ARE DARK GRAY, DOLOMITIZED AND SILICIFIED. SHALES ARE GREENISH GRAY TO BLACK, CARBONACEOUS, CALCAREOUS, KAOLINITIC, SERICITIC, AND SILICEOUS. EFFECTS OF LIMONITIZATION ARE VERY SIGNIFICANT ON HOSTROCKS. VEINS OF JASPEROID, QUARTZ AND CALCITE HAVE IMPREGNATED THE WALLROCKS.
References
Reference (Deposit): BISSELL, H.J., ET. AL., 1959, GUIDEBOOK TO THE GEOLOGY OF UTAH, NO. 14, UT. GEOL. SOC.: U.G.M.S. BULL. 14, 262P.
Reference (Deposit): GILLULY, J., 1932, GEOLOGY AND ORE DEPOSITS OF THE STOCKTON AND FAIRFIELD QUADRANGLES: U.S.G.S. PROF. PA. 173, 167P.
Reference (Deposit): BUTLER, B.S., ET. AL., 1920, THE ORE DEPOSITS OF UTAH: U.S.G.S. PROF. PA. 111, 672P.
Reference (Deposit): SPURR, J.E., 1895, ECONOMIC GEOLOGY OF THE MERCUR MINING DISTRICT, UTAH: U.S.G.S. 16TH. ANN. REPT., PT. 2, 454P.
Reference (Production): GILLULY, J., 1932: P. 140-141
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