The Adams Creek is a gold mine located in Alaska.
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
Adams Creek MRDS details
Site Name
                            
                            Primary: Adams Creek
                        
                
Commodity
                                        
                Primary: Gold
                
                        
Location
                                                State: Alaska 
                                                            District: Nome 
                    
Land Status
Not available
Holdings
Not available
Workings
Not available
Ownership
Not available
Production
Not available
Deposit
                            Record Type: Site
                Operation Category: Past Producer
                Operation Type: Unknown
                Years of Production: 
                Organization: 
                Significant: 
           
        
Physiography
Not available
Mineral Deposit Model
                                            Model Name: Placer Au-PGE
                        
        
Orebody
Not available
Structure
Not available
Alterations
Not available
Rocks
Not available
Analytical Data
Not available
Materials
                                       
                    Ore: Gold 
                           
                    Gangue: Garnet 
                           
                    Gangue: Magnetite 
                        
Comments
Comment (Exploration): Status = Inactive
Comment (Deposit): Model Name = Placer Au-PGE (Cox and Singer, 1986; model 39a).
Comment (Workings): Workings / Exploration = Small-scale sluicing took place somewhere on the drainage in 1900.
Comment (Geology): Geologic Description = Gold was discovered early on Adams Creek and small-scale mining produced 50 to 60 ounces on one claim in 20 days (Brooks and others, 1901). The stream gravels are 4 to 6 feet thick and heavy mineral concentrate contains garnet and magnetite. The active drainage is incised 5 feet into an alluvial terrace. Bedrock in the area is mostly part of a metavolcanic assemblage thought to be Ordovician in age (Till and others, 1986).
Comment (Production): Production Notes = Brooks and others (1901) report that 50 to 60 ounces of gold (worth $19.40 per ounce) were recovered in a 20-day period from one claim.
Comment (Reference): Primary Reference = Brooks and others, 1901
Comment (Geology): Age = Quaternary.
References
                
                                        Reference (Deposit): Cobb, E.H., 1972, Metallic resources map of the Solomon quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-445, scale 1:250,000. 
                                                                
            
                
                                        Reference (Deposit): Till, A.B., Dumoulin, J.A., Gamble, B. ., Kaufman, D.S., and Carroll, P.I., 1986,  Preliminary geologic map and fossil data, Soloman, Bendeleben, and southern Kotzebue quadrangles, Seward Peninsula, Alaska: U.S. Geological Survey Open-File Report 86-276, 10 p., 3 plates, scale 1:250,000. 
                                                                
            
                
                                        Reference (Deposit): Cobb, E.H., 1978, Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Solomon quadrangle, Alaska: U.S. Geological Survey Open-File Report 78-181, 185 p. 
                                                                
            
                
                                        Reference (Deposit): Brooks, A.H., Richardson, G. B., and Collier, A. J., 1901,  Reconnaissance in the Cape Nome and Norton Bay regions, Alaska, in 1900: U.S. Geological Survey Special Publication,  p. 1-180. 
                                                                
            
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