The Baultoff Creek is a copper mine located in Alaska at an elevation of 5,098 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: 5,098 Feet (1,554 Meters)
Commodity: Copper
Lat, Long: 62.1054, -141.21590
Map: View on Google Maps
Baultoff Creek MRDS details
Site Name
                            
                            Primary: Baultoff Creek
                        
                    
                            Secondary: Baultoff
                        
                
Commodity
                                        
                Primary: Copper
                
                            
                Tertiary: Molybdenum
                
                            
                Tertiary: Gold
                
                            
                Tertiary: Silver
                
                        
Location
                                                State: Alaska 
                                                            District: Chisana 
                    
Land Status
                                                Land ownership: Federal
                        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
 
                   
                                    
                        Type: Located Claim
                    
                            
Workings
Not available
Ownership
                Owner Name: Gerald Wood
                Info Year: 1984
Production
Not available
Deposit
                            Record Type: Site
                Operation Category: Prospect
                Operation Type: Unknown
                Mining Method: Unknown
                Years of Production: 
                Organization: 
                Significant: Y
                Deposit Size: M
           
        
Physiography
Not available
Mineral Deposit Model
                                            Model Name: Porphyry Cu
                                                Model Name: Porphyry Cu-Mo
                        
        
Orebody
Not available
Structure
Not available
Alterations
                    Alteration Type: L
                    Alteration: Gypsiferous 
            
Rocks
    
                    Name: Diorite
                    Role: Host
                    Age Type: Host Rock Unit
                    Age in Years: 114.000000+-
                    Dating Method: K-Ar
                    Age Young: Cretaceous
Analytical Data
Not available
Materials
                                       
                    Ore: Chalcopyrite 
                           
                    Ore: Pyrite 
                           
                    Gangue: Albite 
                           
                    Gangue: Quartz 
                           
                    Gangue: Actinolite 
                           
                    Gangue: Sericite 
                           
                    Unknown: Magnetite 
                           
                    Unknown: Bornite 
                        
Comments
Comment (Geology): Geologic Description = At the Baultoff prospect, disseminated pyrite and chalcopyrite occur in hornblende diorite and quartz porphyry of the mid-Cretaceous, Klein Creek pluton (Matson and Richter, 1971 [OFR 71-202]: Richter and others, 1975; Hollister and others, 1975). A 400- by 1,000-meter central altered zone is characterized by albite, chlorite, sericite and late anhydrite veins. It is within a 2,000- by 3,000-meter outer zone marked by abundant sericite and pyrite. Local actinolite veins and disseminations are present in the alteration zones. A post-mineralization fault bounds the alteration zone to the east. Surface samples contain less than 0.25 percent copper, and average 0.10 percent copper and less than 0.01 percent molybdenum (Richter and others, 1975). Low amounts of gold and silver are also present. The deposit is estimated to contain 160 million tons with an average grade of 0.20 percent copper and very low amounts of molybdenum (Richter and others, 1975). The diorite and porphyry that host the deposit are part of the Klein Creek pluton which has a K/Ar date of 111 +/- 3.6 Ma (Richter, Lanphere, and Matson, 1975).
Comment (Reserve-Resource): Reserves = The deposit is estimated to contain 160 million tons with an average grade of 0.20 percent copper and very low amounts of molybdenum (Richter and others, 1975).
Comment (Workings): Workings / Exploration = Surface exploration and some diamond drilling have been used to evaluated this deposit. Average grades from surface sampling: 0.10% Cu, with all samples below 0,25% Cu and less than 0.01% Mo, Au and Ag also present (Richter and others, 1975, USGS MF-655K, loc. 53).
Comment (Reference): Primary Reference = Richter, D.H., Singer, D.A., and Cox, D.P., 1975, Mineral resources map of the Nabesna quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-655-K, 1 sheet, scale 1:250,000.
Comment (Deposit): Other Comments = The prospect is in the Wrangell-St. Elias National Preserve. This is one of 8 known porphyry copper deposits which make up the principal mineral resource potential of Nabesna quadrangle. See also: Orange Hill, Bond Creek, Carl Creek, and Horsfeld.
Comment (Age): Mid-Cretaceous; the diorite and porphyry that host the deposit are part of the Klein Creek pluton which has a K/Ar date of 111 +/- 3.6 Ma (Richter, Lanphere, and Matson, 1975).
Comment (Geology): Original Alteration entry - Potassic, propylitic; extensive. Locally gypsiferous alteration composed of central altered zone 400 m by 1000 m with chlorite,sericite, and albite cut by late stage anhydrite veins. Outer altered zones characterized by intense sericitization and pyritization.
Comment (Geology): Most recent Alteration = A 400- by 1,000-meter central altered zone is characterized by albite, chlorite, sericite and late anhydrite veins. It is within a 2,000- by 3,000-meter outer zone marked by abundant sericite and pyrite. Local actinolite veins and disseminations are present in the alteration zones. A post-mineralization fault bounds the alteration zone to the east (Richter and others, 1973).
References
                
                                        Reference (Deposit): Richter, D.H., Singer, D.A., and Cox, D.P., 1975, Mineral resources map of the Nabesna quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-655-K, scale 1:250,000. 
                                                                
            
                
                                        Reference (Deposit): Hollister, V.F., Anzalone, S.A., and Richter, D.H., 1975, Porphyry copper belts of southern Alaska and contiguous Yukon Territory: CIM (Canadian Mining and Metallurgical) Bulletin, v. 68, no. 756, p. 104-112. 
                                                                
            
                
                                        Reference (Deposit): Richter, D.H., Lanphere, M.A., and Matson, N.A., Jr., 1975, Granite plutonism and metamorphism, eeastern Alaska Range, Alaska: Geological Society of American Bulletin, v. 86, p. 819-820. 
                                                                
            
                
                                        Reference (Deposit): Cobb, E.H., and Richter, D.H., 1980, Summaries of data on and list of references to metallic and selected nonmetallic mineral deposits in the Nabesna quadrangle, Alaska: U.S. Geological Survey Open-File Report 80-927, 117 p. 
                                                                
            
                
                                        Reference (Deposit): Richter, D.H., Matson, N.A., Jr., and Smoll, H.R., 1973, Reconnaissance geologic map of the Nabesna A-1 quadrangle, Alaska: U.S. Geological Survey Miscellaneous Investigations Series Map 1-807, scale 1:63,360. 
                                                                
            
                
                                        Reference (Deposit): Matson, N.A., and Richter, D.H., 1971, Geochemical data from the Nabesna A-1 quadrangle, Alaska: U.S. Geological Survey Open-File Report 71-0202, 10 p. 
                                                                
            
                
                                        Reference (Ownership): ALASKA KARDEX 078-085 
                                                                
            
                
                                        Reference (Deposit): Matson, N.A., and Richter, D.H., 1971, Geochemical data from the Nabesna A-1 quadrangle, Alaska: U.S. Geological Survey Open-File Report 71-0202, 10 p.,  loc. 4, samples 138, 139 
                                                                
            
                
                                        Reference (Reserve-Resource): Engineering & Mining Journal 7905, p. 83 
                                                                
            
                
                                        Reference (Deposit): MTA 82 No. E-56 
                                                                
            
                
                                        Reference (Deposit): MacKevett, E.M., Jr., and Holloway, C.D., 1977, Map showing metalliferous and selected nonmetalliferous mineral deposits in the eastern part of southern Alaska: U.S. Geological Survey Open-File Report 77-169-A, 99 p., 1 sheet, scale 1:1,000,000. 
                                                                
            
                
                                        Reference (Deposit): Engineering & Mining Journal 7905, p. 83, No. 144 
                                                                
            
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