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Black Warrior Mine, Buena Vista Mining District, Pershing County, Nevada, USAi
Regional Level Types
Black Warrior MineMine
Buena Vista Mining DistrictMining District
Pershing CountyCounty
NevadaState
USACountry

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Latitude & Longitude (WGS84):
40° 25' 45'' North , 118° 6' 53'' West
Latitude & Longitude (decimal):
Type:
KΓΆppen climate type:
Nearest Settlements:
PlacePopulationDistance
Humboldt119 (2011)22.5km
Imlay171 (2011)25.9km
Lovelock1,878 (2017)41.2km
Mindat Locality ID:
8729
Long-form identifier:
mindat:1:2:8729:5
GUID (UUID V4):
8d03a447-e627-4b16-ad2b-93db85e23166


Located near Unionville.
Sec 35 T30N R34E
Structure: Faults, Cross Faults

Alteration: Some Argillization And Silicification

Deposit: Discovered and worked in 1870, reworked during periods 1916-18 and 1940-41. Mine is developed by adits and a shaft. The vein exposed in main adit has been stoped, in some places up to the surface. ; info.src : 1 pub lit; 2 unpub rept; 3 field observ the black warrior mine is developed on quartz-stibnite veins varying from 3 to 40 inches in width. The ore mineral stibnite occurs As small pods and streaks, and As individual crystals and blebs in the quartz. Tetrahedrite, pyrite and sphalerite are associated with the pods and streaks of stibnite. The larger and higher grade ore bodies are in the rhyolite with size and grade of deposits decreasing upward into the prida formation and downward into the rhyolite pyroclastic rocks. Rhyolite wall rock has been alltered adjacent to the veins. Pyrite commonly altered to limonite; tetrahedrite partially converted to malachite and azurite.. Wallrocks are pyritized and silicified.adjacent to veins.; model name could also be: simple sb.

Deposit type: Low-sulfide Au-quartz vein

Development: Discovered and worked in 1870, reworked during periods 1916-18 and 1940-41.. No activity in 1984, long idle.

Geology: Mine developed on quartz-stibnite veins varying 3 to40 inches in width. Stibnite occurs As small pads and streaks,, and As individual crystals and blebs in the quartz. Tetrahedrite, pyrite and sphalerite are associated with the pods and streaks of stibnite. The larger and higher grade ore bodies are in the rhyolite with size and grade of deposit decreasing upward into the prida formation and downward into the rhyolite pyroclastic rocks. Rhyolite wall rock has been altered adjacent to the veins. Pyrite commonly altered to limonite; tetrahedrite partially converted to malachite and azurite.

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Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded at this locality.


Mineral List


6 valid minerals.

Rock Types Recorded

Note: data is currently VERY limited. Please bear with us while we work towards adding this information!

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Alphabetical List Tree Diagram

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
β“˜Sphalerite2.CB.05aZnS
β“˜Stibnite2.DB.05Sb2S3
β“˜Pyrite2.EB.05aFeS2
β“˜Kermesite2.FD.05Sb2S2O
β“˜'Tetrahedrite Subgroup'2.GB.05Cu6(Cu4C2+2)Sb4S12S
Group 4 - Oxides and Hydroxides
β“˜Quartz4.DA.05SiO2
β“˜'Stibiconite'4.DH.20Sb3+Sb5+2O6(OH)
Group 5 - Nitrates and Carbonates
β“˜Malachite5.BA.10Cu2(CO3)(OH)2
Unclassified
β“˜'Limonite'-

List of minerals for each chemical element

HHydrogen
Hβ“˜ MalachiteCu2(CO3)(OH)2
Hβ“˜ StibiconiteSb3+Sb25+O6(OH)
CCarbon
Cβ“˜ MalachiteCu2(CO3)(OH)2
OOxygen
Oβ“˜ KermesiteSb2S2O
Oβ“˜ MalachiteCu2(CO3)(OH)2
Oβ“˜ QuartzSiO2
Oβ“˜ StibiconiteSb3+Sb25+O6(OH)
SiSilicon
Siβ“˜ QuartzSiO2
SSulfur
Sβ“˜ KermesiteSb2S2O
Sβ“˜ PyriteFeS2
Sβ“˜ SphaleriteZnS
Sβ“˜ StibniteSb2S3
Sβ“˜ Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
FeIron
Feβ“˜ PyriteFeS2
CuCopper
Cuβ“˜ MalachiteCu2(CO3)(OH)2
Cuβ“˜ Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
ZnZinc
Znβ“˜ SphaleriteZnS
SbAntimony
Sbβ“˜ KermesiteSb2S2O
Sbβ“˜ StibiconiteSb3+Sb25+O6(OH)
Sbβ“˜ StibniteSb2S3
Sbβ“˜ Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S

Other Databases

Link to USGS MRDS:10103885

Other Regions, Features and Areas containing this locality


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References

 
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