The West Fork G Taylor-Fry is a chromium mine located in Sweet Grass county, Montana at an elevation of 8,150 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
Elevation: 8,150 Feet (2,484 Meters)
Commodity: Chromium
Lat, Long: 45.3825, -110.00444
Map: View on Google Maps
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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.
West Fork G Taylor-Fry MRDS details
Site Name
Primary: West Fork G Taylor-Fry
Secondary: Fry-Taylor
Secondary: West Fork
Secondary: Fry Dillon
Secondary: Taylor-Fry-Tuttle
Commodity
Primary: Chromium
Secondary: Platinum
Secondary: Rhodium
Secondary: Palladium
Location
State: Montana
County: Sweet Grass
District: In Stillwater Complex
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.
Holdings
Not available
Workings
Not available
Ownership
Not available
Production
Not available
Deposit
Record Type: Site
Operation Category: Occurrence
Operation Type: Unknown
Discovery Year: 1919
Years of Production:
Organization:
Significant: N
Deposit Size: S
Physiography
General Physiographic Area: Rocky Mountain System
Physiographic Province: Middle Rocky Mountains
Mineral Deposit Model
Model Name: Bushveld Cr
Orebody
Form: MASSIVE BAND, DISSEMINATED
Structure
Type: R
Description: The Stillwater Complex Is Exposed Along The Northern Margin Of The Beartooth Uplift, One Of Several Laramide Basement-Cored Ranges That Make Up The Rocky Mountain Foreland Of South-Central Montana (Foose And Others, 1961: Kulik And Schmidt, 1988)
Type: L
Description: Cross-Faulting
Alterations
Not available
Rocks
Name: Harzburgite
Role: Host
Age Type: Host Rock
Age Young: Early Cretaceous
Name: Harzburgite
Role: Host
Age Type: Associated Rock Unit
Age Young: Neoarchean
Analytical Data
Analytical Data: TRENCHES YIELDED 0.3-4.6 FT OF 0.69-44.3% CR2O3 (AVERAGE 3 FT, 19.6% CR2O3). AVERAGE OF CHROMITITE SAMPLES: 497.1 PPB PT, 1.05 PPM PD, 138.5 PPB RH (MAX. 8 PPM PT, 11 PPM PD, 1.7 PPM RH). 1 FT WIDE MASSIVE ZONE AVERAGED 42.91% CR2O3, DISSEMINATED ZONE 12.15% CR2O3
Materials
Ore: Chromite
Gangue: Olivine
Comments
Comment (Location): UNSURVEYED. LOCATED ON EAST SLOPE OF CRESCENT CREEK, NORTH SIDE OF CRESCENT CREEK VALLEY, WEST SIDE OF WEST FORK STILLWATER RIVER. IN CUSTER NATIONAL FOREST
Comment (Workings): TRENCHES
Comment (Geology): AGE OF STILLWATER COMPLEX IS 2,705 +/- 4 MA BASED ON U-PB SYSTEMATICS ON ZIRCON-BADDELEYITE (PREMO AND OTHERS, 1990)
Comment (Deposit): MAIN MASSIVE BAND IS G CHROMITITE. MAXIMUM GIVEN IS FOR MASSIVE ORE. DISSEMINATED ORE MAXIMUM IS 2.8 FT. CHROMITITE BANDS OFFSET BY SMALL FAULTS TRENDING NE
References
Reference (Deposit): SCHAFER, P.A., 1937, CHROMITE DEPOSITS OF MONTANA: MONTANA BUREAU OF MINES AND GEOLOGY MEMOIR 18, P. 14-16.
Reference (Deposit): WIMMLER, N.L., 1948, INVESTIGATION OF CHROMITE DEPOSITS OF THE STILLWATER COMPLEX, STILLWATER AND SWEETGRASS COUNTIES, MONT.: U.S. BUREAU OF MINES REPORT OF INVESTIGATIONS 4368, P.
Reference (Deposit): HOWLAND, A.L., 1955, CHROMITE DEPOSITS IN THE CENTRAL PART OF THE STILLWATER COMPLEX, SWEET GRASS COUNTY, MONTANA: U.S. GEOLOGICAL SURVEY BULLETIN 1015-D, P. 114.
Reference (Deposit): PAGE, N.J, RILEY, L.B., AND HAFFTY, JOSEPH, 1972, VERTICAL AND LATERAL VARIATION OF PLATINUM, PALLADIUM, AND RHODIUM IN THE STILLWATER COMPLEX, MONTANA: ECONOMIC GEOLOGY, V. 67, P. 918.
Reference (Deposit): PREMO, W.R., HELZ, R.T., ZIENTEK, M.L., AND LANGSTON, R.B., 1990, U-PB AND SM-ND AGES FOR THE STILLWATER COMPLEX AND ITS ASSOCIATED SILLS AND DIKES, BEARTOOTH MOUNTAINS, MONTANA: IDENTIFICATION OF A PARENT MAGMA?: GEOLOGY, V. 18, P. 1065-1068.
Reference (Deposit): ZIENTEK, M.L., 1993, MINERAL RESOURCE APPRAISAL FOR LOCATABLE MINERALS: THE STILLWATER COMPLEX, IN HAMMARSTROM, J.M., ZIENTEK, M.L., AND ELLIOTT, J.E., EDS., MINERAL RESOURCE ASSESSMENT OF THE ABSAROKA-BEARTOOTH STUDY AREA, CUSTER AND GALLATIN NATIONAL FORESTS, MONTANA: U.S. GEOLOGICAL SURVEY OPEN-FILE REPORT 93-207, P. F1-F83.
Reference (Deposit): PAGE, N.J, RILEY, L.B., AND HAFFTY, JOSEPH, 1969, PLATINUM, PALLADIUM, AND RHODIUM ANALYSES OF ULTRAMAFIC AND MAFIC ROCKS FROM THE STILLWATER COMPLEX, MONTANA: U.S. GEOLOGICAL SURVEY CIRCULAR 624, P. 9-10.
Reference (Deposit): 1955 GEOLMAP HOWLAND, BULL. 1015-
Reference (Reserve-Resource): SCHAFER
Principal Gold Districts of Montana
In Montana, 54 mining districts have each have produced more than 10,000 ounces of gold. The largest producers are Butte, Helena, Marysville, and Virginia City, each having produced more than one million ounces. Twenty seven other districts are each credited with between 100,000 and one million ounces of gold production. Read more: Principal Gold Districts of Montana.
