The Strawberry Mine is a copper mine located in Morgan county, Utah at an elevation of 5,200 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: 5,200 Feet (1,585 Meters)
Commodity: Copper
Lat, Long: 41.13361, -111.83194
Map: View on Google Maps
Strawberry Mine MRDS details
Site Name
                            
                            Primary: Strawberry Mine
                        
                
Commodity
                                        
                Primary: Copper
                
                            
                Secondary: Iron
                
                        
Location
                                                State: Utah 
                                                County: Morgan 
                                                District: Morgan 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: Surface/Underground
        
Ownership
Not available
Production
Not available
Deposit
                            Record Type: Site
                Operation Category: Past Producer
                Operation Type: Unknown
                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: DIKE
                                    
Structure
 
                    Type: R
                   Description: Wasatch Fault
            
Alterations
Not available
Rocks
    
                    Name: Pegmatite
                    Role: Associated
                    Age Type: Associated Rock Unit
                    Age Young: Neoproterozoic
    
                    Name: Pegmatite
                    Role: Associated
                    Age Type: Host Rock
                    Age Young: Neoproterozoic
    
                    Name: Pegmatite
                    Role: Associated
                    Age Type: Associated Rock
                    Age Young: Neoproterozoic
    
                    Name: Pegmatite
                    Role: Associated
                    Age Type: Host Rock Unit
                    Age Young: Neoproterozoic
Analytical Data
Not available
Materials
                                       
                    Ore: Limonite 
                           
                    Ore: Malachite 
                           
                    Gangue: Feldspar 
                        
Comments
Comment (Workings): THREE ADITS AND OPEN CUTTING ALONG DIKE, MIDDLE ADIT 66 FT. LONG, LOWER ADIT 130 FT LONG, UPPER ADIT CAVED AT PORTAL
Comment (Location): SECTION SUBDIVISIONS S 1/4 SW 1/4 SW 1/4 SEC. 27, NE 1/4 NW 1/4 NW 1/4 SEC. 34
Comment (Deposit): PEGMATITE INTRUDES INTO GNEISS OF THE FARMINGTON CANYON COMPLEX ; INFO.SRC : 3 FIELD OBSERV
References
                
                                        Reference (Deposit): TRIPP, B.T., 1980, ON SITE INVESTIGATION:  UTAH GEOL. AND MINERAL SURVEY 
                                                                
            
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