Pine Hen Spring Prospect

The Pine Hen Spring Prospect is a mine located in Beaver county, Utah at an elevation of 7,999 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: Pine Hen Spring Prospect  

State:  Utah

County:  Beaver

Elevation: 7,999 Feet (2,438 Meters)

Commodity:

Lat, Long: 38.39972, -112.54917

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 Pine Hen Spring Prospect

Pine Hen Spring Prospect MRDS details

Site Name

Primary: Pine Hen Spring Prospect


Commodity

Tertiary: Uranium


Location

State: Utah
County: Beaver
District: Newton District


Land Status

Land ownership: National Forest
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: Tushar Mountains


Mineral Deposit Model

Not available


Orebody

Not available


Structure

Type: R
Description: Pioche-Marysvale Mineral Belt, Marysvale Volcanic Field


Alterations

Alteration Type: L
Alteration Text: Strong Argillization, Patchy Silicification, Limonite Staining


Rocks

Name: Intermediate Volcanic Rock
Role: Associated
Age Type: Associated Rock
Age Young: Miocene

Name: Intermediate Volcanic Rock
Role: Associated
Age Type: Associated Rock Unit
Age Young: Miocene


Analytical Data

Not available


Materials

Gangue: Limonite


Comments

Comment (Geology): LOCATED NEAR THE TOPOGRAPHIC WALL OF THE MOUNT BELKNAP CALDERA

Comment (Commodity): COMMODITY IS PROBABLY U, BUT WAS NOT VISUALLY IDENTIFIED

Comment (Location): INFO FROM LAND.ST :(1975)

Comment (Deposit): DEPOSIT CONSISTS OF STRONGLY ARGILLIZED VOLCANICS WITH DISSEMINATED LIMONITE STAIN AND PATCHY SILICIFICATION.

Comment (Workings): WORKINGS CONSIST OF SEVERAL SMALL DOZER CUTS.


References

Reference (Deposit): SHUBAT, M.A., 1985, ON-SITE INVESTIGATION, UGMS

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

Reference (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


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