The Welcome Spring Prospects is a copper mine located in Washington county, Utah at an elevation of 4,770 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: 4,770 Feet (1,454 Meters)
Commodity: Copper
Lat, Long: 37.10139, -113.90528
Map: View on Google Maps
Satelite View
MRDS mine locations are often very general, and in some cases are incorrect. Some mine remains have been covered or removed by modern industrial activity or by development of things like housing. The satellite view offers a quick glimpse as to whether the MRDS location corresponds to visible mine remains.
Welcome Spring Prospects MRDS details
Site Name
Primary: Welcome Spring Prospects
Commodity
Primary: Copper
Location
State: Utah
County: Washington
District: Tutsagubet District
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
Discovery Method: Ore-Mineral In Place
Years of Production:
Organization:
Significant: N
Deposit Size: S
Physiography
Not available
Mineral Deposit Model
Not available
Orebody
Form: IRREGULAR
Structure
Type: R
Description: Detachment Faul
Type: L
Description: Detachment Fault
Alterations
Alteration Type: L
Alteration Text: Argillic, Chloritization, Silicification
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
Comments
Comment (Geology): VERY COARSE GRAINED GRANITE OR SYENITE ASSOCIATED WITH DEPOSIT. MINERALIZATION OCCURS IMMEDIATELY BENEATH A DETACHMENT FAULT SEPARTAING GNEISS FROM OVERLYING MISSISSIPPIAN LIMESTONE
Comment (Commodity): TUNGSTEN IS REPORTED TO BE PRESENT BUT HAS NOT BEEN DOCUMENTED. POSSIBLY ANOMALOUS GOLD
Comment (Deposit): DEPOSIT IS HOSTED BY SILICIFIED AND CHLORITIZED GNEISS WITH ABUNDANT QUARTZ VEINS AND VEINLETS. ALTERED AND MINERALIZED ROCK IMMEDIATELY UNDERLIES A DETACHMENT FAULT SEPARATING GNEISS AND OVERLYING LIMESTONE
Comment (Workings): WORKINGS CONSIST OF SEVEN PROSPECT PITS AND DOZER CUTS, ONE STEEPLY INCLINED SHAFT, AND ONE COLLAPSED ADIT
References
Reference (Deposit): SHUBAT, M.A., 1985, ON-SITE INVESTIGATION, UGMS FILES
Reference (Deposit): COOK, E.F., 1960, GEOLOGIC ATLAS OF UTAH, WASHINGTON COUNTY: UGMS BULL. 70
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