Mine detail: Pine Hen Spring Prospect

Previously called ''

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Location

Lat / long:

38.39969, -112.54996

Resource(M)

Tertiary:	Uranium
Gangue:	Limonite

Production

Operation type:	Unknown
Production size:	None
Development status:	Occurrence

Geology

Host type:	Intermediate Volcanic Rock
Associated rock:	Bullion Canyon Volcanics
Associated type:	Intermediate Volcanic Rock
Structure:	Pioche-Marysvale Mineral Belt, Marysvale Volcanic Field
Tectonic:	Basin And Range-Colorado Plateau Transist Zone
Alteration processes:	Strong Argillization, Patchy Silicification, Limonite Staining

References

MRDS	M058865
DEP	10042307
Reference	{Deposit:: CUNNINGHAM, C.G., AND STEVEN, T.A., 1980, GEOLOGIC MAP OF THE BEAVER NE QUADRANGLE, WEST-CENTRAL UTAH: U.S. GEOLOGICAL SURVEY MAP MF-1191}{Deposit:: STEVEN, T.A., AND MORRIS, H.T., 1984, MINERAL RESOURCE POTENTIAL OF THE RICHFIELD 1X2 QUADRANGLE, WEST-CENTRAL UTAH: U.S. GEOLOGICAL SURVEY OPEN-FILE REPORT 84-521}{Deposit:: SHUBAT, M.A., 1985, ON-SITE INVESTIGATION, UGMS}
Reporter	Shubat, Michael A.