The South Fork Welcome Creek Prospects is a copper mine located in Washington county, Utah at an elevation of 4,731 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: 4,731 Feet (1,442 Meters)
Commodity: Copper
Lat, Long: 37.09333, -113.89861
Map: View on Google Maps
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South Fork Welcome Creek Prospects MRDS details
Site Name
Primary: South Fork Welcome Creek Prospects
Commodity
Primary: Copper
Location
State: Utah
County: Washington
District: Tutsagubet 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
Not available
Ownership
Not available
Production
Not available
Deposit
Record Type: Site
Operation Category: Occurrence
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: Colorado Plateaus
Physiographic Section: High Plateaus Of Utah
Physiographic Detail: Beaver Dam Mountains
Mineral Deposit Model
Not available
Orebody
Form: IRREGULAR
Structure
Type: R
Description: Detachment Fault
Type: L
Description: Detachment Fault
Alterations
Alteration Type: L
Alteration Text: Chloritization
Rocks
Name: Granite
Role: Associated
Age Type: Host Rock
Age Young: Neoproterozoic
Analytical Data
Not available
Materials
Ore: Chalcopyrite
Ore: Malachite
Gangue: Quartz
Gangue: Chlorite
Gangue: Pyrite
Gangue: Limonite
Comments
Comment (Geology): VERY COARSE GRAINED GRANITE OR SYENITE INTERCALATED WITH GNEISS. MINERALIZATION PRESUMABLY IS RELATED TO A DETACHMENT FAULT WHICH STRUCTURALLY OVERLIES PROSPECT BY LESS THAN 100 FEET.
Comment (Location): INFO FROM LAND.ST :(1975)
Comment (Commodity): TUNGSTEN WAS VERBALLY REPORTED TO BE PRESENT IN THE AREA BUT NOT DOCUMENTED. POSSIBLY ANOMALOUS GOLD
Comment (Deposit): DEPOSIT HOSTED BY CHLORITIZED GNEISS WITH ABUNDANT QUARTZ VEINS AND VEINLETS. GNEISS IS INTERCALATED WITH GRANITE OR SYENITE. CHALCOPYRITE, MALACHITE, AND PYRITE PRESENT. PERVASIVE LIMONITE STAIN.
Comment (Workings): WORKINGS CONSIST OF THREE DOZER CUTS.
References
Reference (Deposit): SHUBAT, M.A., 1985, ON-SITE INVESTIGATION, UGMS FILES
Reference (Deposit): COOK, E.F., 1960, GEOLOGIC ATLAS OF UTAH, WASHINGTON COUNTY: UTAH GEOL. AND MINERAL SURVEY BULL. 70
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