The Murphy-Lucky Strike Prospects is a gold, silver, copper, and arsenic mine located in Tooele county, Utah at an elevation of 5,220 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: 5,220 Feet (1,591 Meters)
Commodity: Gold, Silver, Copper, Arsenic
Lat, Long: 40.17083, -113.81222
Map: View on Google Maps
Murphy-Lucky Strike Prospects MRDS details
Site Name
                            
                            Primary: Murphy-Lucky Strike Prospects
                        
                
Commodity
                                        
                Primary: Gold
                
                            
                Primary: Silver
                
                            
                Primary: Copper
                
                            
                Primary: Arsenic
                
                        
Location
                                                State: Utah 
                                                County: Tooele 
                                                District: Clifton (Gold Hill) District 
                    
Land Status
                                                Land ownership: BLM Administrative Area
                        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
                Owner Name: Joseph Murphy, Buzz Jones
Production
Not available
Deposit
                            Record Type: Site
                Operation Category: Occurrence
                Deposit Type: Contact Metasomatic
                Operation Type: Unknown
                Discovery Method: Ore-Mineral In Place
                Years of Production: 
                Organization: 
                Significant: N
                Deposit Size: S
           
        
Physiography
                General Physiographic Area: Intermontane Plateaus
                Physiographic Province: Basin And Range Province
                Physiographic Section: Great Basin
                Physiographic Detail: Deep Creek Mountains
Mineral Deposit Model
Not available
Orebody
                                                                            Form: IRREGULAR, TABULAR
                                    
Structure
 
                    Type: R
                   Description: Basin And Range
            
Alterations
                    Alteration Type: L
                    Alteration Text: Recrystallization, Silication, Silicification Of Ls.
            
Rocks
    
                    Name: Diorite
                    Role: Associated
                    Age Type: Associated Rock
                    Age Young: Late Jurassic
    
                    Name: Diorite
                    Role: Associated
                    Age Type: Associated Rock Unit
                    Age Young: Late Jurassic
    
                    Name: Diorite
                    Role: Associated
                    Age Type: Host Rock Unit
                    Age Young: Mississippian
    
                    Name: Diorite
                    Role: Associated
                    Age Type: Host Rock
                    Age Young: Mississippian
Analytical Data
Not available
Materials
                                       
                    Ore: Conichalcite 
                           
                    Ore: Tenorite 
                           
                    Gangue: Grossularite 
                           
                    Gangue: Wollastonite 
                           
                    Gangue: Quartz 
                           
                    Gangue: Calcite 
                           
                    Gangue: Andradite 
                           
                    Gangue: Limonite 
                           
                    Gangue: Opal 
                        
Comments
Comment (Deposit): N17-77W, 36-67NE BEDDING REPLACEMENT ORESHOOTS: MOST ARE PROBABLY 10-20 FT. WIDE OR LESS. EST. WIDTHS ARE DETERMINED BY THE WIDTH OF THE SKARN ZONES; TRUE WIDTHS MUST BE DETERMINED BY ASSAY.
Comment (Deposit): DURING THE BRIEF FIELD INVESTIGATION (MESSENGER, 1981,) THE ONLY QTZ. MONZONITE-LS. CONTACT IDENTIFIED WAS A CONTACT WITH A SILL IN A 118 FT. ADIT DRIVEN ALONG THE CONTACT. IN ALL THE OTHER WORKINGS THE QTZ. MONZONITE-LS. CONTACT IS BELIEVED TO BE AT A SHALLOW DEPTH. ; INFO.SRC : 3 FIELD OBSERV; 1 PUB LIT
Comment (Location): INCORRECTLY LABELED "ALVARADO MINE" ON THE GOLD HILL 7.5 MIN. QUADRANGLE MAP.
Comment (Workings): FIVE SHAFTS 10-25 FT. DEEP, 3 THIRTY FT. DEEP SHAFTS, ONE 50 FT. DEEP SHAFT, A 118 FT. LONG ADIT, A 48 FT. LONG ADIT, TRENCHES AND PITS. ALL SHAFT DEPTHS ARE ESTIMATED.
References
                
                                        Reference (Deposit): MESSENGER, H. M. III, 1981, ON-SITE INVESTIGATION:  UTAH GEOL. AND MINERAL SURVEY 
                                                                
            
                
                                        Reference (Deposit): NOLAN, T. B., 1935, THE GOLD HILL MINING DISTRICT, UTAH:  U.S. GEOLOGICAL SURVEY PROF PAPER 177 
                                                                
            
                
                                        Reference (Deposit): 1935 GEOLMAP NOLAN, T. B., 1935, PROF. PAPER 177, P1.2 
                                                                
            
                
                                        Reference (Deposit): 1981 RECON UGMS, OPEN FILE REPT. 
                                                                
            
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