Goshute Quartz Crystal

The Goshute Quartz Crystal is a tungsten mine located in Juab county, Utah at an elevation of 7,700 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: Goshute Quartz Crystal

State:  Utah

County:  Juab

Elevation: 7,700 Feet (2,347 Meters)

Commodity: Tungsten

Lat, Long: 39.82083, -113.95000

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 Goshute Quartz Crystal

Goshute Quartz Crystal MRDS details

Site Name

Primary: Goshute Quartz Crystal


Commodity

Primary: Tungsten


Location

State: Utah
County: Juab
District: Deep Creek


Land Status

Not available


Holdings

Not available


Workings

Not available


Ownership

Not available


Production

Not available


Deposit

Record Type: Site
Operation Category: Producer
Operation Type: Unknown
Years of Production:
Organization:
Significant: N


Physiography

Not available


Mineral Deposit Model

Not available


Orebody

Not available


Structure

Not available


Alterations

Not available


Rocks

Name: Quartz Monzonite
Role: Host
Age Type: Host Rock
Age Young: Pliocene


Analytical Data

Not available


Materials

Not available


Comments

Not available


References

Reference (Deposit): THOMPSON, K. C., 1973 , MINERAL DEPOSITS OF THE DEEP CREEK MTNS., TOOELE AND JUAB COUNTIES, UTAH: UTAH GEOL. & MIN. SURVEY BULL. 99 .

Reference (Deposit): NELSON, R. B., 1966 , STRUCTURAL DEVELOPEMENT OF NORTHERN MOST SNAKE RANGE, KERN MOUNTAIN AND DEEP CREEK RANGE, NEVADA & UTAH: AM. ASSOC. PETROLEUM GEOLOGISTS BULL., VOL. 50 , NO. 5 , PP. 921 - 951 .


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