Unnamed (in Selawik Hills)

The Unnamed (in Selawik Hills) is a copper 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 (in Selawik Hills)  

State:  Alaska

County:  na

Elevation:

Commodity: Copper

Lat, Long: 66.16, -159.62000

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 (in Selawik Hills)

Unnamed (in Selawik Hills) MRDS details

Site Name

Primary: Unnamed (in Selawik Hills)


Commodity

Primary: Copper


Location

State: Alaska
District: Selawik


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

Model Name: Basaltic Cu (BC name is Volcanic redbed Cu)


Orebody

Not available


Structure

Not available


Alterations

Alteration Type: L
Alteration Text: Chlorite and epidote.


Rocks

Not available


Analytical Data

Not available


Materials

Ore: Pyrite
Ore: Chalcopyrite
Ore: Malachite
Gangue: Calcite
Gangue: Chlorite
Gangue: Epidote


Comments

Comment (Reference): Primary Reference = Barker, 1985

Comment (Deposit): Model Name = Basaltic Cu? (Cox and Singer, 1986; model 23)

Comment (Geology): Geologic Description = The country rocks at this occurrence consist of Jurassic metabasalt and metasedimentary rocks. The occurrence consists of pyrite, malachite, and minor chalcopyrite in calcite, chlorite and epidote veins in chlorite-altered basalt (greenstone) and in fine-grained banded metasedimentary rocks. Metallic minerals in the veins occur as veinlets and pods. Sulfide banding in the greenstone consists predominately of pyrite. Copper values in high-grade grab samples did not exceed 1,000 ppm. Copper values greater than 100 ppm were noted in a stream-sediment sample taken from a stream which drains the site (Barker, 1985).

Comment (Deposit): Other Comments = This occurrence is on the boundary of the Selawik National Wildlife Refuge.

Comment (Workings): Workings / Exploration = Site was sampled by the U.S. Bureau of Mines (Barker, 1985).

Comment (Geology): Age = Jurassic

Comment (Exploration): Status = Inactive


References

Reference (Deposit): Barker, J.C., 1985, Sampling and analytical results of a mineral reconnaissance in the Selawik Hills area, northwestern Alaska: U.S. Bureau of Mines Open-File Report 43-85, 67 p.


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