The Big Cottonwood Mine is a iron mine located in Salt Lake county, Utah at an elevation of 9,751 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: 9,751 Feet (2,972 Meters)
Commodity: Iron
Lat, Long: 40.58278, -111.58417
Map: View on Google Maps
Big Cottonwood Mine MRDS details
Site Name
                            
                            Primary: Big Cottonwood Mine
                        
                    
                            Secondary: Mountain Lake Group
                        
                    
                            Secondary: Great Western Mines
                        
                
Commodity
                                        
                Primary: Iron
                
                            
                Secondary: Copper
                
                            
                Tertiary: Tungsten
                
                        
Location
                                                State: Utah 
                                                County: Salt Lake 
                                                District: Big Cottonwood 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
                Owner Name: Great Western Mines Co.
                Home Office: Ogden, Ut.
Production
Not available
Deposit
                            Record Type: Site
                Operation Category: Past Producer
                Operation Type: Unknown
                Year First Production: 1875
                Year Last Production: 1907
                Discovery Year: 1875
                Discovery Method: Ore-Mineral In Place
                Years of Production: 
                Organization: 
                Significant: N
                Deposit Size: S
           
        
Physiography
                General Physiographic Area: Rocky Mountain System
                Physiographic Province: Middle Rocky Mountains
                Physiographic Detail: Wasatch Mountains
Mineral Deposit Model
Not available
Orebody
                                                                            Form: IRREGULAR
                                    
Structure
 
                    Type: R
                   Description: Vinta-Cottonwood Arch, Sevier Overthrust Belt, Cordilleran Hingeline
            
 
                    Type: L
                   Description: Grizzly Thrust Fault
            
Alterations
                    Alteration Type: L
                    Alteration Text: Calc-Silicate Zone Of Skarn Environment, Oxidation
            
Rocks
    
                    Name: Diorite
                    Role: Associated
                    Age Type: Associated Rock
                    Age Young: Oligocene
    
                    Name: Diorite
                    Role: Associated
                    Age Type: Host Rock
                    Age Young: Mississippian
Analytical Data
                                    
                Analytical Data: 1.67% CU, 60% RECOVERY OF FE FROM THE ORE
            
                    
Materials
                                       
                    Ore: Magnetite 
                           
                    Ore: Chalcopyrite 
                           
                    Ore: Scheelite 
                           
                    Ore: Bornite 
                           
                    Gangue: Talc 
                           
                    Gangue: Epidote 
                           
                    Gangue: Brucite 
                           
                    Gangue: Phlogopite 
                           
                    Gangue: Chlorite 
                           
                    Gangue: Tremolite 
                           
                    Gangue: Actinolite 
                           
                    Gangue: Garnet 
                           
                    Gangue: Serpentine 
                           
                    Gangue: Forsterite 
                        
Comments
Comment (Development): SURFACE RIGHTS ARE OWNED BY WASATCH NATIONAL FOREST. METALURGICAL TESTING BY THE USBM IN 1970, USING STRAIGHT MAGNETIC SEPARATION AND FLOTATION SUCCESSFULLY REMOVED COPPER AND SULFUR FROM IRON ORE. GRINDING TO-100 MESH WAS NECESSARY.
Comment (Commodity): MOSTLY AN IRON (MAGNETITE) PROSPECT WITH LOW GRADE COPPER ASSOCIATED
Comment (Location): TOWNSHIP IS UNSURVEYED. MINE LOCATION IS MISLABELED ON 7.5 TOPOGRAPHIC MAP OF THE BRIGHTON QUADRANGLE ; INFO FROM LAND.ST :1983
Comment (Production): SMALL SHIPMENTS WERE MADE IN 1875. IN 1907 SMALL SHIPMENTS OF COPPER ORE WERE SENT TO THE TINTIC SMELTER
Comment (Reserve-Resource): BULLOCK, K.C., 1970
Comment (Deposit): Discovery Year: LATE 1800'S
Comment (Deposit): DEPOSIT IS A LOW-GRADE COPPER-BEARING MAGNETITE METASOMATIC REPLACEMENT DEPOSIT. THE NORTH ORE BODY IS CRESCENT SHAPED, 375 FT LONG, 50 FT THICK, AND STRIKES EAST-WEST. THE SOUTH ORE BODY STRIKES NNW FOR 315 FT AND IS 20 FT THICK. THE THIRD ORE BODY IS UNDERGROUND, STRIKE, NNW, AND IS OF UNDETERMINED EXTENT
Comment (Workings): THE PORTAL OF THE MINE IS CUT IN GRANODIORITE, THE ADIT EXTENDS SW FOR 700 FT IN GRANODIORITE. THEN A CROSSCUT PASSES THROUGH 110 FT 8F SKARN. A DRIFT THEN CUTS ABOUT 30 FT OF MAGNETITE
Comment (Geology): SOME UNUSUAL BORATES, LUDWIGITE AND MAGNESIOLUDWIGITE, ARE ABUNDANT. OTHER, UNUSUAL MINERALS SUCH AS EPHOSITE, SUSSEXITE, XANTHOPHYLLITE, AND HYDROMAGNESITE MAY ALSO BE PRESENT. CARBONATES FORM A ROOF PENDANT SUSPENDED BETWEEN THE ALTA STOCK TO THE NORTHWEST AND THE CLAYTON PEAK STOCK TO THE SOUTHEAST. THE SKARN ZONE IS ABOUT 50 FT THICK.
References
                
                                        Reference (Deposit): JAMES, L.P., 1979, GEOLOGY, ORE DEPOSITS, AND HISTORY OF THE BIG COTTONWOOD MINING DISTRICT, SALT LAKE COUNTY, UTAH: U.G.M.S. BULL. NO. 114. 
                                                                
            
                
                                        Reference (Deposit): CALKINS, F.C., AND BUTLER, B.S., 1943, GEOLOGY AND ORE DEPOSITS OF THE COTTONWOOD-AMERICAN FORK AREA, UTAH: U.S. GEOLOGICAL SURVEY PROF. PAPER, NO. 201. 
                                                                
            
                
                                        Reference (Deposit): BUTLER, B.S., LOUGHLIN, G.F., HEIKES, V.C., AND OTHERS, 1920, THE ORE DEPOSITS OF UTAH: U.S. GEOLOGICAL SURVEY PROF. PAPER, NO. 111. 
                                                                
            
                
                                        Reference (Deposit): BAKER, A.A., CALKINS, F.C., CRITTENDEN, M.D., JR., AND BROMFIELD, C.S., 1966, GEOLOGIC MAP OF THE BRIGHTON QUADRANGLE, UTAH: U.S. GEOLOGICAL SURVEY GEOL. QUAD. MAP GQ-534 
                                                                
            
                
                                        Reference (Deposit): BULLOCK, K.C., 1970, IRON DEPOSITS OF UTAH: U.G.M.S. BULL. 88, P. 72 
                                                                
            
                
                                        Reference (Deposit): CRAWFORD, A.L., AND BURANEK, A.M., 1957, TUNGSTEN RESERVES DISCOVERED IN THE COTTONWOOD-AMERICAN FORLE MINING DISTRICTS. UTAH: UTAH GEOL. AND MIN. SURVEY REPRINT NO. 55 
                                                                
            
                
                                        Reference (Production): BULLOCK, K.C., 1970 
                                                                
            
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