Open Pit Pennsylvania Mine

The Open Pit Pennsylvania Mine is a gold, silver, and copper mine located in Lincoln county, Nevada at an elevation of 5,751 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: Open Pit Pennsylvania Mine  

State:  Nevada

County:  Lincoln

Elevation: 5,751 Feet (1,753 Meters)

Commodity: Gold, Silver, Copper

Lat, Long: 37.41361, -114.47472

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 Open Pit Pennsylvania Mine

Open Pit Pennsylvania Mine MRDS details

Site Name

Primary: Open Pit Pennsylvania Mine
Secondary: Tom Johnston Property In Part
Secondary: Part of Alta Claims
Secondary: Jumbo Claim Area?


Commodity

Primary: Gold
Primary: Silver
Primary: Copper
Tertiary: Barium-Barite


Location

State: Nevada
County: Lincoln
District: Pennsylvania 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

Not available


Ownership

Owner Name: Westward Energy And Resources, Inc.
Years: 1983 -


Production

Not available


Deposit

Record Type: Site
Operation Category: Past Producer
Operation Type: Unknown
Years of Production:
Organization:
Significant: N
Deposit Size: S


Physiography

Not available


Mineral Deposit Model

Not available


Orebody

Not available


Structure

Type: R
Description: Caliente Caldron Complex

Type: L
Description: Ne-And Nw- Striking Faults.


Alterations

Alteration Type: L
Alteration Text: Argillization, Silicification,


Rocks

Not available


Analytical Data

Not available


Materials

Ore: Malachite
Ore: Brochantite
Ore: Gold
Ore: Chalcopyrite
Gangue: Pyrite
Gangue: Calcite
Gangue: Clay
Gangue: Quartz


Comments

Comment (Workings): PROPERTY CONTAINS SMALL SHALLOW OPEN-PIT MINE AND STOCK PILES OF REWORKED DUMP MATERIAL FROM OTHER MINESITES IN DISTRICT. FAIRLY MODERN CRUSHING AND SORTING EQUIPMENT PRESENT. OLD CHARCOAL KILNS, (SMELTERS), SEVERAL LEACH? PONDS IN DRAINAGE AND CANISTERS OF SODIUM LSULFISDE AT SITE. SHALLOW SURFACE SCRAPING

Comment (Reserve-Resource): EASILY MINEABLE (OPEN PIT) ORE FROM THE JUMBO SHOOT

Comment (Location): UNSURVEYED ; INFO FROM LAND.ST :1972

Comment (Development): SEVERAL CORE BOXES INDICATE PROPERTY WAS DRILLED. OPEN PIT OPERATION APPEARS TO BE 2.5 YEARS OLD. EQUIPMENT IS MODERN, BUT NO SIGN OF CURRENT ACTIVITY. ORANGE FAGGING ON OUTCROPS AT WEST EDGE OF PIT INDICATES RECENT SAMPLING OF PROPERTY

Comment (Deposit): AREA OF SHEETED QUARTZ VEINS AND QUARTZ-CEMENTED BRECCIA WHICH WAS EMPLACED ALONG ASHEAR ZONE. INTERVENING WALLROCK FRAGMENTS AND LENSES CONSIST OF ALTERED ANDESITE, MAPPED AS MIOCENE ASH-FLOW TUFF. ROCKS ARE HIGHLY ALTERED; FELDSPARS ALTERED TO CLAY. THERE ARE SOME FRAGMENTS OF CONGLOMERATE OR FINE-GRAINED CLASTIC ROCK ALSO. FRAGMENTS OF QUARTZ VEIN, RECEMENTED BY WHITE QUARTZ WERE ALSO OBSERVED, INDICATING MULTIPLE VEINING AND BRECCIATION. THE QUARTZ IN OUTCROP IS LIGHT GREEN TO TAN TO GREY IN COLOR, SUGARY TO MASSIVE IN TEXTURE AND CHARACTERISTICALLY VUGGY WITH SOME GOSSANY PORTIONS. THE VUGS ARE FILLED WITH EUHEDRAL PRISMATIC QUARTZ WHICH IS HIGHLY IRON-STAINED. FISSURE-TYPE BANDING IS COMMON AS IS QUARTZ AFTER CALCITE TEXTURES. SOME COARSE WHITE CALCITE VEIN IS ALSO PRESENT. THE REMNANT MOST ROCK IS THOROUGHLY KAOLINIZED AND SILICIFIED. MOST OF THE VEINS ARE SUBPARALLEL WITH A GENERAL N-NW STRIKE AND SHALLOW E-NE DIP. THE OUTCROP IS SHEARED (FRACTURED) BOTH PARALLEL TO AND AT A

Comment (Deposit): HIGH ANGLE TO THE SHEETED VEIN SYSTEM. THE DOMINANT NW SHEARING AND VEINING REFLECTS A MAJOR NE-STRIKING 30E-DIPPING FAULT WHICH BOUNDS THE INFERRED SOUTHERN LIMIT OF THE CALIENTE CALDRON COMPLEX. SO

Comment (Commodity): BA IS UNCERTAIN.


References

Reference (Deposit): BENTZ, J. AND SMITH, P., 1983, FIELD EXAMINATION REPORT ON SEPT 13,1983.

Reference (Deposit): TSCHANZ AND PAMPEYAN, 1970, NBMG BULL 73, P. 170-172, PL. I., II.

Reference (Deposit): NBMG DISTRICT FILES, REPORT ON TOM JOHNSON PROPERTY

Reference (Deposit): GRAPEVINE SPRING G-E-M RESOURCES AREA TECHNICAL REPORT, 1983. FOR BLM

Reference (Reserve-Resource): NBMG DISTRICT FILES, UNPUB. REPORT ON TOM JOHNSTON PROPERTY


Nevada Gold

Gold Districts of Nevada

Nevada has a total of 368 distinct gold districts. Of the of those, just 36 are major producers with production and/or reserves of over 1,000,000 ounces, 49 have production and/or reserves of over 100,000 ounces, with the rest having less than 100,000 ounces. Read more: Gold Districts of Nevada.