The Brady Glacier Deposit is a copper and nickel 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
Brady Glacier Deposit MRDS details
Site Name
                            
                            Primary: Brady Glacier Deposit
                        
                
Commodity
                                        
                Primary: Copper
                
                            
                Primary: Nickel
                
                            
                Secondary: Cobalt
                
                            
                Tertiary: PGE
                
                        
Location
                                                State: Alaska 
                                            
Land Status
Not available
Holdings
Not available
Workings
Not available
Ownership
Not available
Production
Not available
Deposit
                            Record Type: Site
                Operation Category: Occurrence
                Operation Type: Unknown
                Years of Production: 
                Organization: 
                Significant: N
           
        
Physiography
Not available
Mineral Deposit Model
Not available
Orebody
Not available
Structure
Not available
Alterations
Not available
Rocks
Not available
Analytical Data
Not available
Materials
                                       
                    Ore: Chalcopyrite 
                           
                    Ore: Chromite 
                           
                    Ore: Ilmenite 
                           
                    Ore: Pentlandite 
                        
Comments
Comment (Reserve-Resource): DISS. ORE AVERAGES 0.20 PPM PGM AND MASS. ORE 1.30 PPM PGM. MINERALS BEARING PGM HAVE NOT BEEN FOUND.
Comment (Commodity): VALUES ARE PERMISSIVE OF MANTLE DERIVATION FOR THE S AND C BUT ARE NOT DIAGNOSTIC OF SUCH ORIGIN.
Comment (Deposit): DISSEMINATED, INTERSTITIAL, INFREQUENTLY MASSIVE.
Comment (Geology): ASSAYS AND CONDUCTIVITY MEASUREMENTS ON CORE SAMPLES SUGGEST IN SOME AREAS 130 - 200 M. THICKNESS ROCK MAY HOST INTERCONNECTING SULPHIDE NETWORK AVERAGING 70.4 % NI. AND 0.3 % CU.
References
                
                                        Reference (Deposit): CZAMANSKE, G. K. ETAL, APRIL 25 - 27 , 1977 , GEOL. ASSN. CA. ETAL, ANNUAL MEETINGS:  GEOL. ASSN. CA., VANCOUVER, B.C., PROGRAM WITH ABSTRACTS VOL. 
                                                                
            
                
                                        Reference (Reserve-Resource): CZAMANSKE, G.K. ETAL, APRIL 25 - 27 , 1977 , GEOL. ASSN. CA. ETAL., ANNUAL MEETINGS;  GEOL. ASSN. CA., VANCOUVER, B.C, PROG. W/ABSTRACTS VOL. 2 
                                                                
            
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