Shafts West of Big Pinto Spring

The Shafts West of Big Pinto Spring is a mine located in Beaver county, Utah at an elevation of 8,281 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: Shafts West of Big Pinto Spring  

State:  Utah

County:  Beaver

Elevation: 8,281 Feet (2,524 Meters)

Commodity:

Lat, Long: 38.15306, -113.85056

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 Shafts West of Big Pinto Spring

Shafts West of Big Pinto Spring MRDS details

Site Name

Primary: Shafts West of Big Pinto Spring


Commodity

Tertiary: Copper


Location

State: Utah
County: Beaver
District: Indian Peak District


Land Status

Land ownership: BLM Administrative Area
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

Type: Underground


Ownership

Not available


Production

Not available


Deposit

Record Type: Site
Operation Category: Occurrence
Deposit Type: Vein
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: TABULAR


Structure

Type: R
Description: Pioche Mineral Belt, Sevier Orogenic Belt.

Type: L
Description: Fracture Zone At N 60 W 71 Ne To Vertical


Alterations

Alteration Type: L
Alteration Text: Propylitic And Weak Argillic


Rocks

Name: Ash-Flow Tuff
Role: Associated
Age Type: Associated Rock
Age Young: Oligocene

Name: Ash-Flow Tuff
Role: Associated
Age Type: Host Rock
Age Young: Oligocene

Name: Ash-Flow Tuff
Role: Associated
Age Type: Associated Rock Unit
Age Young: Oligocene


Analytical Data

Not available


Materials

Ore: Chrysocolla
Ore: Malachite
Gangue: Quartz
Gangue: Limonite
Gangue: Pyrite


Comments

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

Comment (Deposit): DEPOSIT CONSISTS OF A MASSIVE CHALCEDONY VEIN ABOUT 5 FEET WD WITH ADJACENT QUARTZ STOCK WORK UP TO 20 FEET WIDE. PYRITE AND LIMESITE ASSOCIATED WITH MINOR CHRYSOCOLLA AND MALACHITE STAIN IN VEIN MATERIAL.

Comment (Workings): WORKINGS CONSIST OF TWO SHAFTS. ONE SHAFT IS 25 FEET DEEP WITH A 15 FOOT LONG DRIFT. THE OTHER ADIT IS ABOUT 50 FEET DEEP AND FLOODED AT THE BOTTOM.


References

Reference (Deposit): GRANT, S.K., AND BEST, M.G., 1979, GEOLOGIC MAP OF THE PINTO SPRINGS AND PART OF THE ATCHISON CREEK QUADRANGLES, BEAVER AND IRON COUNTIES, UTAH: U.S. GEOLOGICAL SURVEY OPEN FILE REPORT 79-1656.

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


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