The Tom Payne Mine is a lead and zinc mine located in Santa Fe county, New Mexico at an elevation of 6,440 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: 6,440 Feet (1,963 Meters)
Commodity: Lead, Zinc
Lat, Long: 35.49944, -106.13167
Map: View on Google Maps
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Tom Payne Mine MRDS details
Site Name
Primary: Tom Payne Mine
Secondary: Mine: Tom Paine
Secondary: Claim: Tom Paine Or Tom Payne
Commodity
Primary: Lead
Primary: Zinc
Secondary: Copper
Secondary: Silver
Location
State: New Mexico
County: Santa Fe
District: Cerrillos
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
Type: Underground
Ownership
Owner Name: Mineral Products Corp.
Home Office: Albuquerque, Nm
Years: 1961 -
Production
Not available
Deposit
Record Type: Site
Operation Category: Past Producer
Deposit Type: Vein
Operation Type: Unknown
Year First Production: 1885
Discovery Year: 1879
Discovery Method: Ore-Mineral In Place
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
Form: LINEAR
Structure
Type: R
Description: Faults And Shear Zones
Type: L
Description: Faults And Shear Zones
Alterations
Not available
Rocks
Name: Monzonite
Role: Associated
Age Type: Associated Rock
Age Young: Oligocene
Name: Monzonite
Role: Associated
Age Type: Host Rock
Age Young: Oligocene
Name: Monzonite
Role: Associated
Age Type: Associated Rock Unit
Age Young: Oligocene
Name: Monzonite
Role: Associated
Age Type: Host Rock Unit
Age Young: Oligocene
Analytical Data
Not available
Materials
Ore: Chalcopyrite
Ore: Pyrite
Ore: Galena
Gangue: Quartz
Gangue: Chalcedony
Gangue: Opal
Gangue: Ankerite
Gangue: Calcite
Comments
Comment (Location): LOCATION IS ACCURATE FOR THE SHAFT ; INFO FROM LAND.ST :(1979)
Comment (Deposit): THE VEIN IS A NARROW ZONE OF SHEARED AND HYDROTHERMALLY ALTERED MONZONITE CONTAINING THIN TABULAR SHOOTS AND STRINGERS OF ORE. THE VEIN FOLLOWS A SLIGHTLY SINUOUS COURSE; THROUGHOUT MOST OF ITS EXTENT IT STRIKES N 10-20 E, BUT ON THE SECOND LEVEL, 220 FEET NORTH OF THE SHAFT, IT BENDS MORE TO THE NORTHEAST. THIS CURVE COINCIDES WITH THE NORTH END OF THE RICHEST ORE SHOOT MINED. THE DIPS ARE STEEP TO THE WEST, WITH REVERSAL OF DIP INDICATED LOCALLY. THE ORE SHOOTS ARE ELONGATE ALONG THE STRIKE.
Comment (Workings): WORKINGS CONSIST OF THE MAIN INCLINE SHAFT AND 6 LEVELS WHICH DEVELOPED THE VEIN LATERALLY TO THE NORTH AND SOUTH. THE SHAFT INCLINES 79 TO 86 DEGREES TO THE WEST, FOLLOWING THE VEIN TO A DEPTH OF 310 FEET BELOW THE OUTCROP. IN 1945, LEVEL 1 WAS AT 102-FT DEPTH AND 820 FEET LONG; LEVEL 2 WAS AT 175-FT DEPTH AND 785 FEET LONG; LEVEL 3 WAS AT 271-FT AND 330 FEET LONG; LEVEL 4 WAS AT 295-FT AND 60 FEET LONG. IN 1951 A NEW LEVEL WAS OPENED AT 250 FEET WITH DRIFTS 125 FEET TO THE NORTH AND SOUTH. IN 1955 ANOTHER LEVEL WAS OPENED AT 200 FEET AND WAS 60 FEET LONG. DISBROW AND STOLL (1957) HAVE A MINE MAP OF THE TOM PAYNE.
Comment (Production): THE RECORDED PRODUCTION FOR THE PERIOD 1911 TO 1952 WAS ABOUT 7000 TONS; THE ORE WAS HIGH IN ZINC COMPARED TO THE AVERAGE FOR THE DISTRICT.
References
Reference (Deposit): NMBMMR GENERAL FILE DATA
Reference (Deposit): DISBROW, A.E. AND W.C. STOLL, 1957, NMBMMR BULL 48, P. 53-54
Reference (Deposit): ELSTON, W.E., 1967, NMBMMR BULL 81, P. 30-33
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