The Arickaree Mine is a phosphorus-phosphates mine located in Rich county, Utah at an elevation of 6,460 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: 6,460 Feet (1,969 Meters)
Commodity: Phosphorus-Phosphates
Lat, Long: 41.73956, -111.05031
Map: View on Google Maps
Arickaree Mine MRDS details
Site Name
                            
                            Primary: Arickaree Mine
                        
                    
                            Secondary: Arikaree Mine
                        
                
Commodity
                                        
                Primary: Phosphorus-Phosphates
                
                            
                Tertiary: Selenium
                
                        
Location
                                                State: Utah 
                                                County: Rich 
                                                District: Crawford Mountains 
                    
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
                Owner Name: Bradley Estates
                Owner Name: San Francisco Chemical Co.
Production
                        			
                Year: 1920
                Time Period: 1908 To 1920
                Material type: P
                Description: Cp_Grade: ^Over 34 Percent P2o5
            
                    
Deposit
                            Record Type: Site
                Operation Category: Past Producer
                Deposit Type: Bedded - Phosphate
                Operation Type: Surface
                Year First Production: 1907
                Discovery Year: 1897
                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: Crawford Mountains
Mineral Deposit Model
Not available
Orebody
                                                                            Form: TABULAR
                                    
Structure
 
                    Type: R
                   Description: Woodruff Thrust And Crawford Thrust
            
 
                    Type: L
                   Description: Syncline
            
Alterations
Not available
Rocks
    
                    Name: Shale
                    Role: Host
                    Age Type: Host Rock
                    Age Young: Late Permian
Analytical Data
                                    
                Analytical Data: 5' 5" THICK BEDS AVERAGING 70.3% CA3(PO4)2 EQUIVALENCE
            
                    
Materials
                                       
                    Ore: Whitlockite 
                        
Comments
Comment (Reserve-Resource): MINE WORKED OUT
Comment (Commodity): PHOSPHATE ROCKS HAVE AN OOLITIC TEXTURE . SELENIUM IS FOUND IN THE CARBONACEOUS SHALES.
Comment (Location): SECTION SUBDIVISIONS W 1/2 N 1/2
Comment (Deposit): THERE ARE TWO LAYERS OF HIGH GRADE OOLITIC PHOSPHATE ROCKS SEPERATED BY A THIN STRIP ( 7 IN ) OF LOW GRADE ROCK
Comment (Workings): PORTAL CAVED. SEVERAL INCLINED STOPES DRIVEN TO SURFACE
Comment (Geology): GEOL.DESC: THE PHOSPHATE BEDS ARE INTERSTRATIFIED WITH SHALE AND LIMESTONE CONTAINING MARINE FAUNA
Comment (Deposit): SOUTHERN END OF WORKINGS COVERED BY SIOUX CLAIM ; INFO.SRC : 1 PUB LIT; 3 FIELD OBSERV
References
                
                                        Reference (Deposit): TRIPP, B T, 1980, ON SITE INVESTIGATION:  UTAH GEOL AND MINERAL SURVEY. 
                                                                
            
                
                                        Reference (Deposit): KING, D L, 1967, SAN FRANCISCO CHEM CO:  FIFTEENTH ANNUAL FIELD CONF 
                                                                
            
                
                                        Reference (Deposit): WIDEMAN, F L, 1958, MINING INCLINED BEDS OF PHOSPHATE ROCK SAN FRANCISCO CHEMICAL CO MINES:  USBM IC-7849. 
                                                                
            
                
                                        Reference (Deposit): DASCH,M.D., 1964, ANTIMONY AND OTHER MINOR METALS IN MINERAL AND WATER RESOURCES OF UTAH: UTAH GEOL. & MIN. SURV., BULL. 73, P. 143. 
                                                                
            
                
                                        Reference (Deposit): 1909 RECON GALE AND RICHARDS BULL 430 
                                                                
            
                
                                        Reference (Deposit): 1979 RECON TRIPP UGMS 
                                                                
            
                
                                        Reference (Production): TRIPP, B T, 1980, UT GEOL AND MINERAL SUR ON SITE INVESTIGATION 
                                                                
            
                
                                        Reference (Reserve-Resource): TRIPP, B T, 1980, ON SITE INVESTIGATION:  UTAH GEOL AND MINER SUR 
                                                                
            
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