Red Bluff Mine

The Red Bluff Mine is a tungsten mine located in Valley county, Idaho at an elevation of 8,199 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: Red Bluff Mine

State:  Idaho

County:  Valley

Elevation: 8,199 Feet (2,499 Meters)

Commodity: Tungsten

Lat, Long: 45.1597, -115.40280

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 Red Bluff Mine

Red Bluff Mine MRDS details

Site Name

Primary: Red Bluff Mine


Commodity

Primary: Tungsten
Tertiary: Lead
Tertiary: Copper
Tertiary: Zinc


Location

State: Idaho
County: Valley
District: Edwardsburg District


Land Status

Land ownership: National Forest
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.
Administrative Organization: Payette National Forest


Holdings

Not available


Workings

Not available


Ownership

Not available


Production

Year: 1954
Material type: ORE
Description: Ap_Grade: ^.98 % Wo4 Average


Deposit

Record Type: Site
Operation Category: Past Producer
Deposit Type: Vein
Operation Type: Unknown
Year First Production: 1954
Discovery Year: 1952
Discovery Method: Unknown
Years of Production:
Organization:
Significant: N
Deposit Size: S


Physiography

General Physiographic Area: Rocky Mountain System
Physiographic Province: Northern Rocky Mountains
Physiographic Detail: Salmon River Mountains


Mineral Deposit Model

Not available


Orebody

Form: STRINGERS


Structure

Type: L
Description: Fractures


Alterations

Alteration Type: L
Alteration Text: Silicification, Black Manganese Stain


Rocks

Name: Dacite
Role: Associated
Age Type: Associated Rock
Age Young: Pliocene


Analytical Data

Analytical Data: AVERAGE GRADE 1.0 - 1.5% WO4


Materials

Ore: Chalcopyrite
Ore: Scheelite
Ore: Galena
Ore: Huebnerite
Ore: Sphalerite
Gangue: Rhodonite
Gangue: Pyrite
Gangue: Quartz


Comments

Comment (Location): BETWEEN MIDDLE AND SOUTH FORKS OF SMITH CREEK

Comment (Deposit): STEEPLY DIPPING QUARTZ VEIN AND SEVERAL SMALLER, SIMILAR VEINS

Comment (Geology): KIRKPATRICK (1974) IS UNSURE OF THE AGE OF THE QUARTZ - FELDSPAR GNEISS, HE BELIEVES IT IS BETWEEN PRECAMBRIAN AND CRETACEOUS; OTHER PRIOR AUTHORS, INCLUDING HOBBS (1964), HAVE LABELED THIS ROCK AS CRETACEOUS GRANITIC ROCKS OF THE IDAHO BATHOLITH


References

Reference (Deposit): KIRKPATRICK, G. E., 1974, GEOLOGY AND ORE DEPOSITS OF THE BIG CREEK AREA, VALLEY AND IDAHO COUNTIES, IDAHO: MOSCOW, IDAHO, UNIV. OF IDAHO, M.S. THESIS, P. 43 - 45

Reference (Deposit): HOBBS, S. W., 1964, MINERAL RESOURCE - TUNGSTEN, IN MINERAL AND WATER RESOURCES OF IDAHO: IDAHO BUREAU OF MINES AND GEOLOGY SPEC. REPT. NO. 1, P. 223 - 233

Reference (Deposit): 1964 COMPILE IDAHO BUREAU OF MINES AND GEOLOGY SPEC. REPT. NO.

Reference (Production): KIRKPATRICK, G. E., 1974, UNIV. OF IDAHO, M.S. THESIS.


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