Bloody Canyon Mine

The Bloody Canyon Mine is a antimony and silver mine located in Pershing county, Nevada at an elevation of 6,401 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: Bloody Canyon Mine  

State:  Nevada

County:  Pershing

Elevation: 6,401 Feet (1,951 Meters)

Commodity: Antimony, Silver

Lat, Long: 40.51667, -118.13556

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 Bloody Canyon Mine

Bloody Canyon Mine MRDS details

Site Name

Primary: Bloody Canyon Mine
Secondary: Red Star
Secondary: Hutton
Secondary: Cosmopolitan


Commodity

Primary: Antimony
Primary: Silver
Tertiary: Iron
Tertiary: Lead


Location

State: Nevada
County: Pershing
District: Star 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: Neal, Hybert L.
Home Office: Winnemucca, Nev.
Years: 1960 -


Production

Year: 1942
Material type: SB ORE
Description: Ap_Grade: ^55% Sb
Year: 1940
Material type: SB ORE
Description: Ap_Grade: ^13% Sb
Year: 1938
Material type: SB ORE
Description: Ap_Grade: ^60 % Sb
Year: 1912
Material type: SB ORE
Description: Ap_Grade: ^60 % Sb
Year: 1907
Material type: SB ORE
Description: Ap_Grade: ^60 % Sb
Year: 1942
Time Period: To 1942
Material type: ORE SB AG
Description: Cp_Grade: ^60 % Sb


Deposit

Record Type: Site
Operation Category: Producer
Operation Type: Unknown
Year First Production: 1871
Discovery Year: 1868
Discovery Method: Other
Years of Production:
Organization:
Significant: N
Deposit Size: S


Physiography

General Physiographic Area: Intermontane Plateaus
Physiographic Province: Basin And Range Province
Physiographic Section: Great Basin
Physiographic Detail: Basin And Mountains


Mineral Deposit Model

Model Name: Low-sulfide Au-quartz vein


Orebody

Form: VEINS


Structure

Type: R
Description: Reg.Struct: Faults And Cross Faults, Tnding N-S, Nne-Ssw, Cause Alot Of Gouge

Type: L
Description: Faults And Cross-Faults Trending N-S, Nne-Ssw


Alterations

Alteration Type: L
Alteration Text: Silicification, Some Sericitized Feldspar


Rocks

Name: Limestone
Role: Associated
Age Type: Host Rock
Age Young: Late Triassic


Analytical Data

Not available


Materials

Ore: Stibnite
Gangue: Quartz
Unknown: Chalcopyrite
Unknown: Pyrite


Comments

Comment (Commodity): OTHER ORE MINERALS NOT GIVEN IN THE LITERATURE

Comment (Deposit): DEPOSIT CONSISTS OF AN EAST AND WEST VEIN. THE ORE WAS MOSTLY HIGH QUALITY ANTIMONY ASSOCIATED WITH AG AND MINOR PB, CONTAINED IN 2 QUARTZ STIBNITE VEINS A FEW FEET THICK ABOUT 200 FEET APART IN A MINERALIZED ZONE OF STEEPLY DIPPING FISSURE VEINS. THE WEST VEIN IS OFFSET BY AN EAST-WEST FAULT WITH THE NORTHERN SEGMENT STRIKING N10E AND DIPS 85 DEGREES W AND IS RELATIVELY BARREN; THE SOUTHERN SEGMENT STRIKES N10W, DIPS 80-85 DEGREES E AND CONTAINS ABUNDANT STIBNITE. THE EAST VEIN STRIKES N10-25E AND DIPS 80-85E AND INTERSECTS A BARREN FAULT WITH STRIKE N25E, DIPPING EAST. STIBNITE OCCURS AS PODS, STREAKS AND SINGLE CRYSTALS IN THE QUARTZ, AND IN GOUGE. PYRITE IS COMON BOTH IN VEINS AND DISSEMINATED THROUGH WALL ROCK. LIMESTONNE, SANDSTONE AND SILTSTONES OF THE STAR PEAK FORMATION OVERLIE THE RHYOLITE AND CROP OUT A SHORT DISTANCE WEST OF THE WORKINGS. ORE IS CONFINED TO RHYOLITE.; MODEL NAME COULD ALSO BE: SIMPLE SB.

Comment (Workings): MOST OF THE ORE WAS MINED FROM THE SOUTH SEGMENT OF THE WEST VEIN BY STOPING FROM THE MAIN ADIT THAT CUTS THE VEIN 200 FT BELOW SURFACE. SEVERAL SHORT ADITS AND TRENCHES EXPLORE SURFACE EXPOSURES OF EAST AND WEST VEINS.

Comment (Location): WEST SIDE OF SOUTH BRANCH OF BLOODY CANYON; ADITS APPEAR AROUND A SPRING; PREVIOUS QUAD DESIGNATION = IMLAY (1956) 1:625000

Comment (Production): BY 1942; AT LEAST 1218 TONS SB

Comment (Development): EXPL.COM: THE MINE WAS WORKED INTERMITTENTLY TO 1942 ; MILL.CAP: 9.125 ; ECON.YEAR: 1937

Comment (Geology): GEOL.COM: THE ORE WAS MOSTLY HIGH QUALITY ANTIMONY ASSOCIATED WITH AG AND MINOR PB, CONTAINED IN TWO QUARTZ STIBNITE VEINS A FEW FEET THICK ABOUT 200 FEET APART IN A MINERALIZED ZONE OF STEEPLY DIPPING FISSURE VEINS. THE WEST VEIN IS OFFSET BY AN EAST-WEST FAULT WITH THE NORTHERN SEGMENT STRIKING N10E AND DIPS 85 DEGREES W AND IS RELATIVELY BARREN; THE SOUTHERN SEGMENT STRIKES N10W, DIPS 80-85 DEGREES E AND CONTAINS ABUNDANT STIBNITE. THE EAST VEIN STRIKES N10-25E AND DIPS 80-85E AND INTERESCTS A BARREN FAULT WITH STRIKE N25E, DIPPING EAST. STIBNITE OCCURS AS PODS, STREAKS, AND SINGLE CRYSTALS IN THE QUARTZ, AND IN GOUGE. PYRITE IS COMMON BOTH IN VEINS AND DISSEMINATED THROUGH WALL ROCK. LIMESTONE, SANDSTONE AND SILTSTONES OF THE STAR PEAK FORMATION OVERLIE THE RHYOLITE AND CROP OUT A SHORT DISTANCE WEST OF THE WORKINGS. ORE IS CONFINED TO RHYOLITE.

Comment (Deposit): DISCOVERED IN 1868. ANTIMONY FIRST PRODUCED IN 1871.OTHER YEARS OF PRODUCTION 1907, 1912, 1917-21, 1938, 1940, 1942. MINE WORKED INTERMITTENTLY TO 1942. THIS MINE WAS ONE OF THE LARGEST PRODUCERS OF ANTIMONY ORE IN NEVADA. MOST OF ORE WAS MINED FROM THE SOUTH SEGMENT OF THE WEST VEIN BY STOPING FROM THE MAIN ADIT THAT CUTS THE VEIN 200 FEET BELOW SURFACE. SEVERAL SHORT ADITS AND TRENCHES EXPLORE SURFACE EXPOSURES OF WESTVEIN AND ALSO FOLLOW THE EAST VEIN. ; INFO.SRC : 1 PUB LIT


References

Reference (Deposit): RAYMOND, 1873, STATISTICS OF MINES AND MINING IN THE STATES AND TERRITORIES WEST OF THEOCKY MOUNTAINS, 5TH MANAUL REPORT; WASHINGTON, GOVT. PRINTING OFFICE

Reference (Production): LAWRENCE, 1963

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

Reference (Deposit): LAWRENCE, 1963, ANTIMONY DEPOSITS OF NEVADA; NBMG BULL. 61


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.