Kennedy Mine

The Kennedy Mine is a iron mine located in Santa Fe county, New Mexico at an elevation of 7,461 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: Kennedy Mine

State:  New Mexico

County:  Santa Fe

Elevation: 7,461 Feet (2,274 Meters)

Commodity: Iron

Lat, Long: 35.51972, -105.74889

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 Kennedy Mine

Kennedy Mine MRDS details

Site Name

Primary: Kennedy Mine
Secondary: Mine: Kennedy Iron Ore Mine
Secondary: Kennedy Limonite
Secondary: San Jose
Secondary: Patented Claims 1905: Iron King
Secondary: Iron Queen
Secondary: Moniter


Commodity

Primary: Iron


Location

State: New Mexico
County: Santa Fe
District: Glorieta 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

Not available


Ownership

Owner Name: Grubnau, V. C.
Years: 1923 -


Production

Not available


Deposit

Record Type: Site
Operation Category: Past Producer
Operation Type: Unknown
Discovery Year: 1900
Discovery Method: Ore-Mineral In Place
Years of Production:
Organization:
Significant: N
Deposit Size: S


Physiography

General Physiographic Area: Rocky Mountain System
Physiographic Province: Southern Rocky Mountains


Mineral Deposit Model

Not available


Orebody

Form: LENS


Structure

Type: R
Description: Glorieta Creek Antcline; Glorieta Syncline


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

Analytical Data: A COMPOSITE CHARACTER SAMPLE CONTAINED 53.4% FE, 0.13% P, 0.14% S, 3.2% SIOZ, 0.1% TI, & 5.8% MN.


Materials

Ore: Hematite
Ore: Limonite


Comments

Comment (Location): LOCATION IS ESTIMATED FROM KELLEY'S (1949, P. 195) DIRECTIONS. ; INFO FROM LAND.ST :1979

Comment (Commodity): THE LIMONITE IS SOFT, POROUS, AND OCHERY IN SEVERAL SHADES OF YELLOW, RED AND BROWN

Comment (Production): LINDGREN (1910, P. 112) STATES THAT SEVERAL THOUSAND TONS WERE PRODUCED. ELSTON (1967, P. 33) STATES THAT 3500 TONS OF ORE WAS SHIPPED, MOSTLY BEFORE 1905, TO LEAD SMELTERS AT SOCORRO AND EL PASO FOR FLUX.

Comment (Development): THE MINE WAS BEING HELD UNDER THE SAN JOSE CLAIM IN 1943 BUT KELLEY (1949, P. 195) DOES NOT GIVE AN OWNER'S NAME.

Comment (Deposit): THE ORE BED IS A LENS OF SOFT, POROUS, OCHERY, IMPURE, SUPERGENE LIMONITE 3 TO 5 FEET THICK. THE BED COVERS AN IRREGULAR ELLIPTICAL AREA EXTENDING 300 FEET NORTH, UP-CHANNEL, ABOUT 150 FEET WIDE. THE LIMONITE PARTLY REPLACES FINE-GRAINED CLASTIC ROCKS OF THE SAN ANDRES FORMATION ALONG BEDDING PLANES. THE ROCKS STRIKE N 15 W AND DIP 7 W.

Comment (Workings): WORKINGS CONSIST OF UNDERGROUND WORKINGS EXTENDING 300-FT. ALONG STRIKE AND 150 FEET UPDIP. THERE ARE ALSO SEVERAL OPENCUTS.


References

Reference (Deposit): KELLEY, V.C., 1949, UNIV. OF NEW MEXICO PUBLICATIONS IN GEOL., NO. 2, P. 195-197.

Reference (Deposit): HARRER, C.M. AND F.J. KELLY, 1963, USBM IC 8190, P. 63

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

Reference (Deposit): NMBMMR GENERAL FILE DATA

Reference (Deposit): LINDGREN, W., L.C. GRATON AND C.H. GORDON, 1910, USGS PP 68, P. 112


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