Bonanza King Mine

The Bonanza King Mine is a gold mine located in Pershing county, Nevada at an elevation of 4,951 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: Bonanza King Mine

State:  Nevada

County:  Pershing

Elevation: 4,951 Feet (1,509 Meters)

Commodity: Gold

Lat, Long: 40.33222, -118.10250

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 Bonanza King Mine

Bonanza King Mine MRDS details

Site Name

Primary: Bonanza King Mine
Secondary: Eagle
Secondary: Lady Mary


Commodity

Primary: Gold
Secondary: Silver
Tertiary: Zinc
Tertiary: Lead
Tertiary: Copper


Location

State: Nevada
County: Pershing
District: Spring Valley 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: Past Producer
Deposit Type: Vein
Operation Type: Unknown
Discovery Year: 1868
Years of Production:
Organization:
Significant: N
Deposit Size: S


Physiography

Not available


Mineral Deposit Model

Model Name: Low-sulfide Au-quartz vein


Orebody

Not available


Structure

Type: L
Description: Ne-Trending Fault, Fracture Zone


Alterations

Not available


Rocks

Name: Rhyolite
Role: Associated
Age Type: Associated Rock
Age Young: Late Triassic


Analytical Data

Analytical Data: 1908 CARLOAD-2.65 OZ AU, 8.32 OZ AG, 2% FE, CONSIDERABLE PB, LITTLE ZN & S, TRACE CU PER TON


Materials

Ore: Sphalerite
Ore: Pyrite
Ore: Argentite
Ore: Chalcocite
Ore: Gold
Ore: Tetrahedrite
Ore: Stephanite
Ore: Chalcopyrite
Ore: Galena
Ore: Covellite
Gangue: Quartz
Gangue: Tourmaline


Comments

Comment (Deposit): DISCOVERED IN 1868, UNDER THE NAME LADY MARY, THEN RELOCATED IN 1871 AS THE EAGLEMINE. THE MINE WAS ACTIVELY WORKED DURING THE PERIOD 1868-85, THEN INTERMITTENTLY UNTIL 1910. THE MINE IS DEVELOPED ON A STEEPLY DIPPING, NW-TRENDING QUARTZ-TOURMALINE VEIN IN AN ALTERED DIABASE DIKE IN ROCHESTER RHYOLITE. THE VEIN WAS MINED BY DRIFTING EASTWARD FROM A SHAFT AT WEST END OF THE MINE STOPED TO THE SURFACE ALONG A LENGTH OF ABOUT 200 TO 250 FEET. ; INFO.SRC : 1 PUB LIT; 2 UNPUB REPT

Comment (Deposit): THE STEEPLY-DIPPING, NW-TRENDING QUARTZ-TOURMOLINE VEIN IS 2 1/2 TO 5 FT WIDE TERMINATING ON THE WEST END IN DIABASE DIKE AND ON THE EAST END AT A NORTHEAST TRENDING FAULT. TOURMALINE REPLACED QUARTZ AFTER SULFIDE MINERALIZATION. VISIBLE GOLD WAS OBSERVED AS FLAKES IN LIMONITE (FROM PYRITE), IN TETRAHEDRITE, AND RARELY IN GALENA. ORE DEPOSIT IS GENETICALLY RELATED TO THE GRANODIORITE STOCK EXPOSED IN SPRING VALLEY AND THE DIABASE DIKE THAT INTRUDES THE RHYOLITE MAY BE AN OFF SHOOT FROM THIS BODY.; MODEL NAME COULD ALSO BE: POLYMETALLIC VEINS.

Comment (Location): PREVIOUS QUAD DESIGNATION = UNIONVILLE (1954) 1:625000

Comment (Production): TOTAL PRODUCTION UNKNOWN, ESTIMATED OVER $50,000

Comment (Workings): THE VEIN WAS MINED BY DRIFTING EASTWARD FROM A SHAFT AT THE WEST END OF THE MINE STOPED TO THE SURFACE ALONG A LENGTH OF ABOUT 200 TO 250 FT.

Comment (Geology): VEIN IS 2 1/2 TO 5 FEET TERMINATING ON THE WEST END IN DIABASED DIKE AND ON EAST END AT A NORTHWEST TRENDING FAULT. TOURMALINE REPLACED QUARTZ AFTER SULFIDE MINERALIZATION. VISIBLE GOLD WAS OBSERVED AS FLAKES IN LIMONITE (FROM PYRITE), IN TETRAHEDRITE, AND RARELY IN GALENA. ORE DEPOSIT IS GENETICALLY RELATED TO THE GRANODIORITE STOCK EXPOSED IN SPRING VALLEY AND THE DIABASE DIKE THAT INTRUDES THE RHYOLITE MAY BE AN OFF SHOOT FROM THIS BODY.

Comment (Development): FIRST EXPLORED UNDER THE NAME LADY MARY, THEN RELOCATED IN 1871 AS THE EAGLEMINE. IT WAS ACTIVELY WORKED DURING 1868-85, THEN, INTERMITTENTLY UNTIL 1910.


References

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

Reference (Deposit): CAMPBELL, D.F., 1939, GEOLOGY OF THE BONANZA KING MINE, HUMBOLDT RANGE, PERSHING COUNTY, NEVADA; ECON. GEOL. V. 34, PP 96-112

Reference (Deposit): NBMG STAFF, 1985, NBMG OFR 85-3

Reference (Deposit): VANDERBURG, 1936, RECONNAISSANCE OF MINING DISTRICTS IN PERSHING COUNTY, NEVADA: USBM IC 6902

Reference (Production): JOHNSON, 1977


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.