South Fork Welcome Creek Prospects

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

Name: South Fork Welcome Creek Prospects  

State:  Utah

County:  Washington

Elevation: 4,731 Feet (1,442 Meters)

Commodity: Copper

Lat, Long: 37.09333, -113.89861

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.


Satelite image of the South Fork Welcome Creek Prospects

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

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 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: Pyrite
Gangue: Quartz
Gangue: Chlorite
Gangue: Limonite


Comments

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

Comment (Commodity): TUNGSTEN WAS VERBALLY REPORTED TO BE PRESENT IN THE AREA BUT NOT DOCUMENTED. POSSIBLY ANOMALOUS GOLD

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


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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