The Muscovite Claim is a mica mine located in Albany county, Wyoming at an elevation of 9,144 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: 9,144 Feet (2,787 Meters)
Commodity: Mica
Lat, Long: 41.0516, -106.17600
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.
Muscovite Claim MRDS details
Site Name
Primary: Muscovite Claim
Commodity
Primary: Mica
Tertiary: Tungsten
Tertiary: Pumice
Tertiary: Feldspar
Tertiary: Garnet
Location
State: Wyoming
County: Albany
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
Not available
Ownership
Not available
Production
Not available
Deposit
Record Type: Site
Operation Category: Past Producer
Operation Type: Unknown
Mining Method: Unknown
Years of Production:
Organization:
Significant: N
Physiography
General Physiographic Area: Rocky Mountain System
Physiographic Province: Southern Rocky Mountains
Mineral Deposit Model
Not available
Orebody
Not available
Structure
Not available
Alterations
Not available
Rocks
Not available
Analytical Data
Not available
Materials
Ore: Muscovite
Ore: Tantalite
Ore: Columbite
Ore: Beryl
Trace: Andradite
Unknown: Microcline
Unknown: Quartz
Comments
Comment (Geology): GRANITE PEGMATITE CUTS PRECAMBRIAN METADIABASES,SCHISTS,GNEISSES. (Bull. 50, p. 132)
Comment (Deposit): "A granite pegmatite dike strikes N50E and cuts pre-Cambrian metadiabases, hornblende schist, and gneisses for a distance of 600 ft. Maximum width of the dike is 70 ft; the average is 40 ft. In places, quartz and white feldspar show a graphic structure. Fine-grained aggregates of quartz and feldspar enclose some pink microcline crystals several inches in diamter. Some muscovite books are up to a foot wide but contain numerous dark iron spots. Tantalite-columbite crystals are associated with green beryl along fractures in the wall rock. Black tourmaline crystals up to several inches long are found in metadiabse and schist wallrock and as fine-grained veinlets in the pegmatite. Andradite(?) garnet is a minor accessory mineral." (Bull. 50, p. 132-133)
References
Reference (Deposit): Hausel and Sutherland, 2000, WSGS Bull. 71, 268 p.
Reference (Deposit): Osterwald and others, 1966, WGS BULL #50, 287 p.
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