Pintada Mine

The Pintada Mine is a copper mine located in Guadalupe county, New Mexico at an elevation of 5,059 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

Name: Pintada Mine  

State:  New Mexico

County:  Guadalupe

Elevation: 5,059 Feet (1,542 Meters)

Commodity: Copper

Lat, Long: 34.92167, -104.88750

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.


Satelite image of the Pintada Mine

Pintada Mine MRDS details

Site Name

Primary: Pintada Mine
Secondary: Patented Claims 1939: Pintada Lode #1-4


Commodity

Primary: Copper


Location

State: New Mexico
County: Guadalupe
District: Pastura District


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.
Administrative Organization: Blm Roswell Resource Area


Holdings

Not available


Workings

Type: Surface/Underground


Ownership

Owner Name: Robert E. Roberts
Home Office: P.O. Box 389, Santa Rosa, N.M.
Years: 1970 -


Production

Not available


Deposit

Record Type: Site
Operation Category: Past Producer
Operation Type: Unknown
Year First Production: 1939
Year Last Production: 1970
Discovery Year: 1895
Discovery Method: Ore-Mineral In Place
Years of Production:
Organization:
Significant: N
Deposit Size: S


Physiography

General Physiographic Area: Interior Plains
Physiographic Province: Great Plains Province
Physiographic Section: Pecos Valley


Mineral Deposit Model

Model Name: Sediment-hosted Cu


Orebody

Form: TABULAR


Structure

Type: L
Description: Minor Folds, Wavy Bedding, And Small Gravity Faults


Alterations

Not available


Rocks

Name: Sandstone
Role: Host
Age Type: Host Rock Unit
Age Young: Late Permian

Name: Sandstone
Role: Host
Age Type: Host Rock
Age Young: Late Permian


Analytical Data

Not available


Materials

Ore: Chalcocite
Ore: Malachite
Gangue: Gypsum


Comments

Comment (Deposit): THE ORE IS LOCATED IN RELATIVELY FLAT-LYING, FINE-GRAINED SANDSTONE. THE MINERALIZATION APPEARS TO BE DISTRIBUTED IN THREE WELL-DEFINED BEDS WITH A TOTAL THICKNESS OF 10-20 FEET. A GYPSUM BED THAT OVERLIES THE TOP SANDSTONE MEMBER IS USED AS AN INDICATOR TO POSITION THE COPPER-BEARING BEDS. THE ORE MINERAL IS FINELY DISSEMINATED CHALCOCITE IN A FINELY GRANULATED, WELL CEMENTED SANDSTONE. CHALCOCITE IS PRESENT IN THE ORE AS DARK PATCHES AND STREAKS IN THE LIGHT-GRAY SANDSTONE. ALTERATION TO MALACHITE IS PROMINENT IN BEDDING PLANES AND FRACTURES.

Comment (Workings): WORKINGS CONSIST OF A MAIN PIT THAT COVERS AN AREA 200 FEET LONG AND 50 TO 60 FEET WIDE AND 30 FEET DEEP AND LIMITS OF THE OREBODY WERE TESTED BY 6 SMALL, SHALLOW SHAFTS.

Comment (Location): LOCATION IS ACCURATE FOR THE PINTADA MINE SHOWN ON THE SAN IGNACIO QUADRANGLE. ; INFO FROM LAND.ST :1979

Comment (Production): THE PINTADA MINE HAS HAD PRODUCTION SPORADICALLY SINCE 1939. NO OTHER FIGURES ARE AVAILABLE.

Comment (Deposit): Discovery Year: 1890'S


References

Reference (Deposit): HARLEY, G.T., 1940, NMBMMR BULL 15, P. 66.

Reference (Deposit): SOULE, J.H., 1956, USBM IC 7740, P. 29-30

Reference (Deposit): SANDUSKY, C.L. AND KAUFMAN, W.H., 1972, NMGS GUIDEBOOK, 23RD FIELD CONFERENCE, P. 176-177

Reference (Deposit): NMBMMR GENERAL FILE DATA

Reference (Production): SANDUSKY, C.L., AND KAUFMAN, W.H., 1972, NMGS GUIDEBOOK, 23RD FIELD CONFERENCE, P. 176-177


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