War Eagle Mine
USA /
California /
Tecopa /
World
/ USA
/ California
/ Tecopa
World / United States / California
mine, production
The War Eagle Mine is located about 6 miles east of Tecopa, or about 43 miles west of Las Vegas. The mine, discovered in 1910 at the south end of the Nopah Range, began commercial operations in 1912. It operated fairly continuously, passing through a number of hands, until 1957, when it was shut down by the Anaconda Copper Corporation. The mine is adjacent to both the Columbia and Noonday Mines; the Noonday being named for the dolomite formation the mines are found in (or possibly the formation was named after the Noonday Mine).
Mineralization focus was argentiferous galena (PbS with silver replacement), which appears to lie along a north-south vein dipping shallowly to the east. Some native gold has been reported in the mine, along with pyrite (FeS₂) and chalcopyrite (CuFeS₂). The upper extensions of the ore shoots exhibit a substantial degree of oxidation with lead carbonates (cerrusite – PbCO₃) and sulfates (anglesite – PbSO₄) present.
It is thought the same ore vein characteristics exist in War Eagle as in the Noonday and Columbia Mines. Those are a main ore vein that is offset by a post mineral fault system, striking north at 65° W. A series of northeast trending fractures with steep northwest dips that control the localization of the orebodies (identified by Norman & Stewart in 1951).
The mine runs about 2,500' along the orebody, north and south; with a 1,200 foot cross-shaft, approximately in the middle. The main workings are thought to be 150' to 200' deep; accessed by a series of raises and an inclined shaft.
geology.csupomona.edu/drjessey/fieldtrips/nopah/wareagl...
www.robertwynn.com/Wareagle.htm
www.theweekendminer.com/CaInyoCountyWarEagleMinePage.ht...
Mineralization focus was argentiferous galena (PbS with silver replacement), which appears to lie along a north-south vein dipping shallowly to the east. Some native gold has been reported in the mine, along with pyrite (FeS₂) and chalcopyrite (CuFeS₂). The upper extensions of the ore shoots exhibit a substantial degree of oxidation with lead carbonates (cerrusite – PbCO₃) and sulfates (anglesite – PbSO₄) present.
It is thought the same ore vein characteristics exist in War Eagle as in the Noonday and Columbia Mines. Those are a main ore vein that is offset by a post mineral fault system, striking north at 65° W. A series of northeast trending fractures with steep northwest dips that control the localization of the orebodies (identified by Norman & Stewart in 1951).
The mine runs about 2,500' along the orebody, north and south; with a 1,200 foot cross-shaft, approximately in the middle. The main workings are thought to be 150' to 200' deep; accessed by a series of raises and an inclined shaft.
geology.csupomona.edu/drjessey/fieldtrips/nopah/wareagl...
www.robertwynn.com/Wareagle.htm
www.theweekendminer.com/CaInyoCountyWarEagleMinePage.ht...
Nearby cities:
Coordinates: 35°49'14"N 116°5'29"W
- Western Talc Mine (abandoned) 6 km
- Eclipse Mine 26 km
- Gerstley Mine 26 km
- Colosseum Mine 54 km
- Black Magic Mines 56 km
- Rainbow Quarries 57 km
- Mountain Pass Rare Earth Mine 63 km
- Arden Gypsum Mines 73 km
- Upper Biddy McCarthy Mine 77 km
- Boraxo Mine 82 km
- Shoshone Mining District 1.9 km
- Kingston Range 17 km
- Dumont Dunes 19 km
- Pahrump, Nevada 43 km
- Confidence Hills 50 km
- Owlshead Mountains 54 km
- Leach Lake 61 km
- Fort Irwin National Training Center 69 km
- Desert Warfare Training area 71 km
- Death Valley National Park 101 km
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