Pennsylvania Mine

The Pennsylvania Mine is a lead and zinc mine located in Santa Fe county, New Mexico at an elevation of 6,460 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: Pennsylvania Mine  

State:  New Mexico

County:  Santa Fe

Elevation: 6,460 Feet (1,969 Meters)

Commodity: Lead, Zinc

Lat, Long: 35.49306, -106.13250

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 Pennsylvania Mine

Pennsylvania Mine MRDS details

Site Name

Primary: Pennsylvania Mine
Secondary: Patented Claims 1906:J.B. Weaver
Secondary: Bob Ingersoll
Secondary: Bertha Mabel
Secondary: Owl
Secondary: Sure Winner


Commodity

Primary: Lead
Primary: Zinc
Secondary: Gold
Secondary: Silver


Location

State: New Mexico
County: Santa Fe
District: Cerrillos 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.


Holdings

Not available


Workings

Type: Surface/Underground


Ownership

Owner Name: Verne Byrne
Home Office: Santa Fe, N.M.
Years: 1957 -


Production

Not available


Deposit

Record Type: Site
Operation Category: Past Producer
Deposit Type: Vein
Operation Type: Unknown
Year First Production: 1950
Year Last Production: 1952
Discovery Year: 1950
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: IRREGULAR


Structure

Type: R
Description: Faults And Shear Zones

Type: L
Description: Shear Zone


Alterations

Alteration Type: L
Alteration Text: Sericitization And Chloritization


Rocks

Name: Monzonite
Role: Associated
Age Type: Associated Rock
Age Young: Oligocene

Name: Monzonite
Role: Associated
Age Type: Associated Rock Unit
Age Young: Oligocene

Name: Monzonite
Role: Associated
Age Type: Host Rock
Age Young: Oligocene

Name: Monzonite
Role: Associated
Age Type: Host Rock Unit
Age Young: Oligocene


Analytical Data

Not available


Materials

Ore: Galena
Ore: Sphalerite
Ore: Gold
Ore: Silver
Gangue: Quartz
Gangue: Limonite
Gangue: Smithsonite


Comments

Comment (Production): DURING 1917-1918 THERE WERE REPORTEDLY SEVERAL CARLOADS OF ORE SHIPPED. APPROXIMATELY 900 TONS OF LEAD-ZINC ORE OF GOOD GRADE WAS PRODUCED BETWEEN 1942 AND 1952.

Comment (Workings): WORKINGS CONSIST OF A 300-FOOT SHAFT AND A 405-FOOT DRIFT ON THE 189-FOOT LEVEL. THERE ARE SEVERAL PITS ON THE SURFACE.

Comment (Deposit): ON THE SURFACE THE PENNSYLVANIA VEIN IS TRACEABLE FOR ABOUT 650 FEET. THE VEIN STRIKES ABOUT DUE NORTH ON THE AVERAGE AND DIPS 70 TO 80 W. NEAR THE PENNSYLVANIA SHAFT IT BENDS ABRUPTLY AND THE BEND IS REFLECTED ALSO IN THE COURSE IN THE VEIN UNDERGROUND. IN THE SADDLE SOUTH OF THE MINE, A CONSPICUOUS VEIN IS EXPOSED IN PITS DUG ON THE EAST FLANK OF LUCERAS HILL; THIS MAY BE A FAULTED SEGMENT OF THE PENNSYLVANIA OR A SECOND VEIN. IN THE SURFACE WORKINGS THE VEIN IS A BEND OF LIGHT-COLORED, SOFT, ALTERED, AUGITE-BIOTITE MONZONITE, 1.5 TO 7 FEET WIDE, CONTAINING STREAKS OF LIMONITE AND STRINGERS OF QUARTZ. GREEN BOTRYOIDAL SMITHSONITE WAS FOUND IN THE WEATHERED CAPPING OF THE VEIN. UNDERGROUND, ON THE 189-FOOT LEVEL, THE VEIN IS A THIN, SINUOUS ZONE OF SHEARING AND ALTERATION CONTAINS A BAND OF MASSIVE SPHALERITE AND GALENA LYING IN THE MIDDLE OR ON THE FOOTWALL OR HANGING WALL. STREAKS OF MASSIVE OPALINE QQARTZ ARE LOCALLY INTERLAYERED WITH ORE. IN THE SHAFT BETWEEN THE 189 AND 300-FOOT

Comment (Deposit): LEVELS THE VEIN CONTAINS AN ALMOST CONTINUOUS BAND OF MASSIVE ORE RANGING 6-18 INCHES THICK. THE VEIN IS COVERED BY MINERAL SURVEY 1325 AND FIVE PATENTED CLAIMS (1906) - THE J.B. WEAVER, BOB INGERSOLL, BERTHA MABLE, OWL, AND SURE WINNER.

Comment (Location): LOCATION IS ACCURATE FOR THE SHAFT. ; INFO FROM LAND.ST :1979

Comment (Deposit): Discovery Year: 1900'S


References

Reference (Deposit): DISBROW, A.E., AND W.C. STOLL, 1957, NMBMMR BULL 48, P. 55-57

Reference (Deposit): ELSTON, W.E., 1967, NMBMMR BULL 81, P. 30-33

Reference (Deposit): NMBMMR GENERAL FILE DATA


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