Mcnutt Brothers Property

The Mcnutt Brothers Property is a manganese mine located in San Miguel county, Colorado at an elevation of 6,624 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: Mcnutt Brothers Property

State:  Colorado

County:  San Miguel

Elevation: 6,624 Feet (2,019 Meters)

Commodity: Manganese

Lat, Long: 38.13083, -108.53889

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 Mcnutt Brothers Property

Mcnutt Brothers Property MRDS details

Site Name

Primary: Mcnutt Brothers Property


Commodity

Primary: Manganese


Location

State: Colorado
County: San Miguel
District: Naturita Ridge Area


Land Status

Land ownership: BLM Administrative Area
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: Mcnutt Brothers
Home Office: Naturita, Co.
Years: 1917 -


Production

Not available


Deposit

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


Physiography

General Physiographic Area: Intermontane Plateaus
Physiographic Province: Colorado Plateaus
Physiographic Section: Canyon Lands


Mineral Deposit Model

Not available


Orebody

Not available


Structure

Type: R
Description: Paradox Basin Fold And Fault Belt

Type: L
Description: Dry Creek Anticline, Hamilton Creek Anticline, Nucla Syncline


Alterations

Not available


Rocks

Name: Sandstone
Role: Host
Age Type: Host Rock
Age Young: Early Cretaceous


Analytical Data

Analytical Data: ORE SAMPLE CONTAINED 37.95 % MN, 4.24% SIO2, 23.40% FE, 1.61% S, 0.33%


Materials

Ore: Wad
Ore: Pyrolusite


Comments

Comment (Location): MUILENBURG (1919) CITES GENERAL LOCATION OF CLAIM AS ABOUT 5 MILES SE OF NATURITA NEAR TOP OF DIVIDE (NATURAL RIDGE) BETWEEN SAN MUGUEL RIVER AND DRY CREEK DRAINAGE. DESCRIPTION OF EXPOSURE ON RESISTANT RIM ABOVE STREAM VALLEY SUGGESTS POSSIBLE LOCATION ALONG LONG DRAW OR BROAD CANYON. ELEV AND LAT-LONG GIVEN ARE FOR COMMON SECTION CORNER ALONG DRAWNEAR DEEP EXOSURE ON NE SIDE OF DIVIDE. ; INFO FROM LAND.ST :1975

Comment (Deposit): TOP OF NATURITA RIDGE CORRESPONDS TO NW-SE TREND OF DRY CREEK ANTICLINE AND HAMILTON CREEK ANTICLINE, THE SE EXTENSIONS OF PARADOX VALLEY ANTICLINE. ROCKS EXPOSED ACROSS CREST OF ANTICLINES ARE LOWER CRETACEOUS BURRO CANYON FM AND DAKOTA SANDSTONE. MUILENBURG (1919) DESCRIBES OCCURENCE AS THIN SEAM QUARTER OF INCH TO FOUR INCHES THICK SEPARATING TWO BEDS OF SANDSTONE OR REPRESENTING PARTING IN SANDSTONE. SEVERAL OTHER SEAMS LIE ABOVE AND BELOW, SEPARATING THIN BEDS OF SANDSTONE. WEIR ANDPUFFETT (1981) STUDIED LISBON VALLEY AREA MN DEPOSITS AND FOUND COMMON OCCURRENCE IN NONCARBONACEOUS SANDSTONE AND SUGGESTED THAT THEIR ASSOCIATION WITH LISBON VALLEY FAULT SYSTEM MAY HAVE REPRESENTED LATE-STAGE LOW-TEMPERATURE MINERALIZATION IN AREA. IT IS CONCEIVABLE THAT MCNUTT DEPOSIT COULD HAVE SIMILAR ORIGIN WITH RESPECT TO STRUCTURE ALONG PARADOX VALLEY ANTICLINE.


References

Reference (Deposit): MUILENBURG, G.A., 1919, MANGANESE DEPOSITS OF COLORADO: CGS BULL. 15, P. 53.

Reference (Deposit): WEIR, G.W., AND PUFFETT, W.P., 1981, INCOMPLETE MANUSCRIPT OF STRATIGRAPHY AND STRUCTURAL GEOLOGY AND URANIUM-VANADIUM AND COPPER DEPOSITS OF THE LISBON VALLEY AREA, UTAH-COLORADO: USGS OPEN-FILE REPT. OF-81-39, P. 271.

Reference (Deposit): WILLIAMS, P.L., 1964, GEOLOGY, STRUCTURE, AND URANIUM DEPOSITS OF THE MOAB QUADRANGLE, COLORADO AND UTAH: USGS MAP I-360.


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