Copper King Mine

The Copper King Mine is a tungsten mine located in Pershing county, Nevada at an elevation of 4,462 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

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.

Site Name

Primary: Copper King Mine
Secondary: Copper King Claims
Secondary: NBMG Sample Sites 2292,2293, 2294
Secondary: Blue Wolf
Secondary: Copper Kelly

Commodity

Primary: Tungsten
Tertiary: Copper
Tertiary: Molybdenum
Tertiary: Iron
Tertiary: Manganese
Tertiary: Silver
Tertiary: Uranium

Location

State: Nevada
County: Pershing
District: Ragged Top District

Land Status

Land ownership: Private
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: Surface/Underground

Ownership

Owner Name: Nevada Copper And Tungsten, Inc.

Production

Year: 1956
Material type: ORE WO3
Description: Ap_Grade: ^0.22% Wo3
Year: 1956
Time Period: 1951,1956
Material type: ORE W
Description: Cp_Grade: ^0.7 % W03

Deposit

Record Type: Site
Operation Category: Occurrence
Operation Type: Unknown
Year First Production: 1952
Discovery Year: 1906
Discovery Method: Ore-Mineral In Place
Years of Production:
Organization:
Significant: N
Deposit Size: S

Physiography

Not available

Mineral Deposit Model

Model Name: W skarn

Orebody

Form: IRREGULAR, LENSES, PODS

Structure

Not available

Alterations

Alteration Type: L
Alteration Text: Silicification

Rocks

Name: Diorite
Role: Associated
Age Type: Associated Rock Unit
Age Young: Late Cretaceous

Name: Diorite
Role: Associated
Age Type: Host Rock
Age Young: Late Jurassic

Name: Diorite
Role: Associated
Age Type: Host Rock Unit
Age Young: Late Jurassic

Name: Diorite
Role: Associated
Age Type: Associated Rock
Age Young: Late Cretaceous

Analytical Data

Analytical Data: 10 PPM Y, -500 PPM ZN, 20 PPM ZR. SAMPLE 2994 OF SKARN FROM THE COPPER KI-NG PIT CONTAINS 5 % FE, 0.7 % MG, 10 % CA, .1 % TI, 1500 PPM M-N, 1 PPM AG, 15 PPM B, 70 PPM BA, 5 PPM CO, 20 PPM CR, 500 PPM- CU, 10 PPM MO, 20 PPM NI, 7 PPM SC, 100 PPM SR, 20 PPM V, 100- PPM ZR.
Analytical Data: SAMPLE 2992 DUMP SAMPLE OF SKARN CONTAINS 7 % FE, 0.03 % MG, 10 % CA, 0.015 % TI, 1500 PPM MN, 10 PPM AG, 30 PPM B-, 20 PPM BA, 1.5 PPM BE, 50 PPM CO, 20000 PPM CU, 7 PPM MO, 7 -PPM NI, 10 PPM PB, 100 PPM SR, 30 PPM V, 70 PPM W, 200 PPM ZN.- SAMPLE 2993 OF GOSSAN ALONG SHEAR ZONE AT MAIN SHAFT CONTAINS- 15 % FE, 0.07 % MG, 7 % CA, 0.05 % TI, 2000 PPM MN, 10 PPM AG-, 30 PPM B, 30 PPM BA, 20 PPM CD, 50 PPM CO, 10 PPM CR, 20000 -PPM CU, 20 PPM MO, 15 PPM NI, 10 PPM V, 150 PPM W

Materials

Ore: Chalcopyrite
Ore: Powellite
Ore: Scheelite
Ore: Bornite
Ore: Chalcocite
Ore: Malachite
Ore: Molybdenite
Gangue: Garnet
Gangue: Quartz
Gangue: Epidote

Comments

Comment (Deposit): Discovery Year: 1906, 1908

Comment (Deposit): THE COPPER KING CLAIMS WERE ORIGINALLY LOCATED FOR COPPER IN 1906 & 1908. THERE IS NO RECORD OF ANY COPPER PRODUCTION DURING THIS PERIOD. IN 1949 E.J. BOTTOMLEY ACQUIRED THE PROPERTY. IN 1952 THE PROPERTY WAS OPTIONED TO THE CORDERO MINING CORP. WHICH SHIPPED 750 TONS OF TUNGSTEN ORE RECOVERING 614 TUNGSTEN TON UNITS. AFTER THIS SEVERAL LESSEES WORKED THE PROPERTY ON A SMALL SCALE. WALLACE & DURBIN SHIPPED 193 TONS OF 0.22% WO3 IN 1956, PRODUCING 1,216 LBS OF TUNGSTEN. PROPERTY WAS IDLE 1956 TO 1968 WHEN THE PROPERTY WAS EXAMINED BY NEVADA COPPER & TUNGSTEN, INC. EXPLORATION STUDIES HAVE BEEN DONE UP TO THE PRESENT, BUT NO MINING ACTIVITY. PROPERTY IS DEVELOPED BY 3 SHAFTS 50-250 FT. DEEP, 2 PITS 6-8 FEET DEEP, 4 TRENCHES 40-50 FT. LONG, AND 3 SHALLOW TRENCHES. ; INFO.SRC : 1 PUB LIT; 2 UNPUB REPT; 3 FIELD OBSERV

Comment (Reserve-Resource): STAGER, H.K., UNPUBLISHED MANUSCRIPT.

Comment (Location): UTM IS FOR SAMPLE SITE 2992. UTM FOR SAMPLE SITE 2993 IS N4429955, E343160. UTM FOR SAMPLE SITE 2994 IS N4429910, -E343200. ; INFO FROM LAND.ST :(1980)

Comment (Production): OVER 614 TUNGSTEN TON UNITS. WALLACE AND DURBIN SHIPPED 193 TONS OF 0.22% WO3 IN 1956, PRODUCING 1,216 LB. TUNGSTEN.

Comment (Development): EXPLORED RECENTLY WITH NO MINING ACTIVITY (1970'S). UTAH INTERNATIONAL WAS STUDYING AND DRILLING THE PROPERTY IN 1979-1980 TO DETERMINE OREBODY EXTENT . US VANADIUM EXPLORED THE PROPERTY IN 1944 BUT SOON ABANDONED IT

Comment (Geology): MINERALIZATION IN THE AREA CONSISTS OF SCHEELITE AND MINOR POWELLITE IN TACTITE AREAS NEAR LIMESTONE GRANODIORITE CONTACTS, AND COPPER IN SHEAR ZONES WHICH APPEAR TO CUT THE TACTITES. FOUR TACTITE ZONES, OF BOTH CONTACT AND STRATABOUND TYPES, HAVE BEEN OUTLINED AT COPPER KING. SCHEELITE IN THE VARIOUS TACTITE ZONES IS ERRATICALLY DISTRIBUTED, GENERALLY AS IRREGULAR LENSES AND PODS. ANOMALOUS AMOUNTS OF IRON (PYRITE), COPPER (CHALCOPYRITE, CHALCOCITE, MALACHITE) AND MOLYBDENUM (MOLYBDENITE) ARE FOUND WITHIN THE GRANODIORITE INTRUSIVE. IT SEEMS LIKELY THIS DISSEMINATED IRON-COPPER-MOLYBDENUM TYPE MINERALIZATION IS BOTH GENETICALLY AND SPACIALLY RELATED TO TACTITE DEVELOPMENT. THERE IS A POSSIBILITY FOR RECOVERY OF MINOR BYPRODUCT COPPER AND MOLYBDENUM SULFIDES FROM TACTITE BODIES MINED FOR TUNGSTEN.

Comment (Workings): 3 SHAFTS, PITS, TRENCHES. OLD 2-COMPARTMENT VERTICAL SHAFT ABOUT 60 FT DEEP AT SAMPLE SITE 2992; COPPER KING SHAFT AT SAMPLE SITE 2993.

Comment (Deposit): SHEAR ZONES, CONTACT TACTITE ZONES. AT SAMPLE SITE 2992, DUMP COMPOSED OF MASSIVE GARNET SKARN, STAINED WITH CHRYSOCOLLA, GREEN CU OXIDES, SOME MN O-XIDE, CLOTS OF FE OX AND CU OX GOSSAN (MELACONITE). SOME ALTER-ED APLITIC INTRUSIVE ON DUMP WITH LIMONITE POINTS. CU OX AND F-E-MN OX COATING LARGE BLOCKS, CRYSTALLINE CALCITE, PATCHES OF -APLITE, MARBLE, SKARN EXPOSED AROUND SHAFT IN WASH AND SEVERAL-SHALLOW TRENCHES. GARNET APPEARS TO BE A POD-LIKE BODY OR LENS- ALONG IRREGULAR CONTACT; AREA COVERED BY THIN PEDIMENT GRAVEL-S- HARD TO SEE TRENDS. GRANODIORITE TO S AND SW, LIMESTONE AND- MARBLE TO N AND NW. COPPER KING SHAFT (SITE 2993) IS SUNK ON -GARNET SKARN WHERE IT IS CUT BY N60E, 70 NW-DIPPING SHEAR ZONE- ABOUT 4-5 FT WIDE, GOSSANY WITH FE OX AND CU OX ALONG IT; GAR-NET ZONE EXTENDS ABOUT 100 FT TO OPEN PIT TO EAST (1985). . THE URANIUM OCCURRENCE IS LOCATED APPROXIMATELY 0.25 MILES NE OF THE MINE BUILDING AND MAJOR WORKINGS OF THE COP-PER KING MINE. THERE IS ANOMALOUS

Comment (Deposit): SCINTILLOMETER COUNT BUT NO -VISIBLE URANIUM IS PRESENT IN LIME GARNET SKARN IN A SMALL PIT-. THE HIGHEST RADIATION IS IN A POD IN COARSE CRYSTALLINE MARB-LE ADJACENT TO THE HIGHEST CONCENTRATION OF GREEN GARNET.

References

Reference (Deposit): SEEL, C., 1977, COPPER KING-AJAX PROSPECTS, PERSHING-CHURCHILL COUNTIES, NEVADA-A PROGRESS REPORT: UNPUBLISHED

Reference (Deposit): JOHNSON & BENSON, 1963, TUNGSTEN RESOURCES OF NEVADA; USBM.

Reference (Deposit): TINGLEY, J. V., 1985, NBMG FIELD EXAMINATION, 4/16/85.

Reference (Deposit): STAGER, H. K., UNPUBLISHED BULLETIN ON TUNGSTEN IN NEVADA.

Reference (Deposit): 1980 UNPUBLISHED PROGRESS REPORT ON COPPER KING PROJECT.

Reference (Deposit): SMOUSE, DEFORREST, 1979, UNPUBLISHED URANIUM OCCURRENCE REPORT FOR UTAH INTERNATIONAL.

Reference (Production): JOHNSON, M.G., 1977

Reference (Deposit): JOHNSON, M.G., 1977, GEOLOGY AND MINERAL DEPOSITS OF PERSHING COUNTY, NEVADA; NBMG BULL. 89

Reference (Deposit): TINGLEY, J.V., 1975, COPPER KING-AJAX CLAIMS, GENERAL ELECTRIC CO., PROPRIETY REPORT: UNPUBLISHED

Nevada Gold

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.