The Lady Bryan Mine is a copper, lead, and iron mine located in Beaver county, Utah at an elevation of 6,621 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: 6,621 Feet (2,018 Meters)
Commodity: Copper, Lead, Iron
Lat, Long: 38.3353, -113.15560
Map: View on Google Maps
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Lady Bryan Mine MRDS details
Site Name
Primary: Lady Bryan Mine
Commodity
Primary: Copper
Primary: Lead
Primary: Iron
Location
State: Utah
County: Beaver
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
Type: Patented
Workings
Not available
Ownership
Owner Name: Utah -Mining-Milling-Trans Co.
Info Year: 1979
Owner Name: Dr. Russell Miller-Las Vegas
Info Year: 1979
Production
Not available
Deposit
Record Type: Site
Operation Category: Past Producer
Operation Type: Underground
Mining Method: Unknown
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
Mineral Deposit Model
Not available
Orebody
Not available
Structure
Not available
Alterations
Not available
Rocks
Not available
Analytical Data
Not available
Materials
Not available
Comments
Not available
References
Reference (Deposit): BULLOCK K.C.1976 FLUORITE OCCURENCE IN UT UGMS BULL 110 P13
Reference (Deposit): 6
Reference (Deposit): E MILFORD FLAT QUAD STAR DIST BEAVER CO UT UGMS SPEC STUDY 4
Reference (Deposit): ABOU-ZIED S.AND WHELAN J.A.1973 GEOLOGY AND MINERALOGY OF TH
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