The Lion No. 2 Mine is a lead and zinc mine located in Grant county, New Mexico.
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
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.
Lion No. 2 Mine MRDS details
Site Name
Primary: Lion No. 2 Mine
Commodity
Primary: Lead
Primary: Zinc
Secondary: Copper
Secondary: Silver
Tertiary: Vanadium
Tertiary: Molybdenum
Location
State: New Mexico
County: Grant
District: Central District (Bayard District)
Land Status
Not available
Holdings
Not available
Workings
Type: Underground
Ownership
Not available
Production
Year: 1930
Time Period: -1930
Description: Cp_Grade: ^16.2% Pb
Deposit
Record Type: Site
Operation Category: Past Producer
Operation Type: Unknown
Year First Production: 1930
Years of Production:
Organization:
Significant: N
Deposit Size: S
Physiography
General Physiographic Area: Intermontane Plateaus
Physiographic Province: Basin And Range Province
Physiographic Section: Mexican Highland
Mineral Deposit Model
Not available
Orebody
Not available
Structure
Type: L
Description: Slate Fault, Owl-Hobo Fault
Alterations
Not available
Rocks
Name: Diorite
Role: Associated
Age Type: Host Rock
Age Young: Late Cretaceous
Name: Diorite
Role: Associated
Age Type: Associated Rock
Age Young: Late Cretaceous
Name: Diorite
Role: Associated
Age Type: Host Rock Unit
Age Young: Late Cretaceous
Analytical Data
Not available
Materials
Ore: Smithsonite
Ore: Sphalerite
Ore: Galena
Ore: Hydrozincite
Ore: Endlichite
Ore: Wulfenite
Ore: Cuprodescloizite
Ore: Calamine
Gangue: Quartz
Gangue: Limonite
Gangue: Calcite
Comments
Comment (Deposit): VEINS ALONG THE SLATE FAULT, A FOOTWALL SPUR OF THE OWL-HOBO FAULT, THAT TRENDS ENE AND DIPS 70SE CUTTING THE CRETACEOUS COLORADO FORMATION AND A CRETACEOUS QUARTZ DIORITE DIKE.
Comment (Production): CARBONATE ORE IS ARGENTIFEROUS
Comment (Workings): SHAFT 30 M. DEEP WITH A DRIFT ON THE 16 M. LEVEL
References
Reference (Production): LASKY, S. G., 1936, U.S. GEOLOGICAL SURVEY BULL. 870, P. 133-134.
Reference (Deposit): LASKY, S. G., 1936, U.S. GEOLOGICAL SURVEY BULL. 870, P. 133-134
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