Unnamed (north of the Tubutulik River)

The Unnamed (north of the Tubutulik River) is a bismuth mine located in Alaska.

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: Unnamed (north of the Tubutulik River)

State:  Alaska

County:  na

Elevation:

Commodity: Bismuth

Lat, Long: 65.25, -162.38000

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 Unnamed (north of the Tubutulik River)

Unnamed (north of the Tubutulik River) MRDS details

Site Name

Primary: Unnamed (north of the Tubutulik River)


Commodity

Primary: Bismuth
Secondary: Tungsten


Location

State: Alaska
District: Koyuk


Land Status

Not available


Holdings

Not available


Workings

Not available


Ownership

Not available


Production

Not available


Deposit

Record Type: Site
Operation Category: Occurrence
Operation Type: Unknown
Years of Production:
Organization:
Significant:


Physiography

Not available


Mineral Deposit Model

Not available


Orebody

Not available


Structure

Not available


Alterations

Not available


Rocks

Not available


Analytical Data

Not available


Materials

Ore: Galena
Gangue: Quartz
Gangue: Fluorite


Comments

Comment (Geology): Age = Cretaceous ; Epigenetic mineralization in metamorphic rocks of Seward Peninsula is primarily of Cretaceous age.

Comment (Exploration): Status = Inactive

Comment (Deposit): Model Name = Bismuth in metamorphic rocks

Comment (Geology): Geologic Description = This occurrence is in the eastern-most part of the Bendeleben Mountains in an area of high-grade metamorphic rocks intruded by many small granitic bodies (Till and others, 1986). A grab sample of gossanous schist contained greater than 10,000 ppm bismuth (Miller and Grybeck, 1973). Another grab sample of calc-silicate hornfels, schist, and granitic rock contained 68 ppm Bi and 100 ppm W (Gamble, 1988).

Comment (Reference): Primary Reference = Miller and Grybeck, 1973

Comment (Workings): Workings / Exploration = Exploration activities at this location are not known but are probably minimal.


References

Reference (Deposit): Miller, T.P., and Grybeck, D.J., 1973, Geochemical survey of the eastern Solomon and southeastern Bendeleben quadrangles, Seward Peninsula, Alaska: U.S. Geological Survey Open-File Report 553, 115 p.

Reference (Deposit): Till, A.B., Dumoulin, J.A., Gamble, B. ., Kaufman, D.S., and Carroll, P.I., 1986, Preliminary geologic map and fossil data, Soloman, Bendeleben, and southern Kotzebue quadrangles, Seward Peninsula, Alaska: U.S. Geological Survey Open-File Report 86-276, 10 p., 3 plates, scale 1:250,000.

Reference (Deposit): Gamble, B.M., 1988, Non-placer mineral occurrences in the Solomon, Bendeleben, and southern part of the Kotzebue quadrangles, western Alaska: U.S. Geological Survey Map MF-1838-B, 13 p., 1 sheet, scale 1:250,000.


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