Unnamed (on tributary to South Fork of Kuskokwim River)

The Unnamed (on tributary to South Fork of Kuskokwim River) is a arsenic and gold 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 (on tributary to South Fork of Kuskokwim River)  

State:  Alaska

County:  na

Elevation:

Commodity: Arsenic, Gold

Lat, Long: 62.014, -153.40900

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 (on tributary to South Fork of Kuskokwim River)

Unnamed (on tributary to South Fork of Kuskokwim River) MRDS details

Site Name

Primary: Unnamed (on tributary to South Fork of Kuskokwim River)


Commodity

Primary: Arsenic
Primary: Gold
Secondary: Tungsten


Location

State: Alaska
District: McGrath


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: Polymetallic veins


Orebody

Not available


Structure

Not available


Alterations

Not available


Rocks

Not available


Analytical Data

Not available


Materials

Ore: Pyrite
Gangue: Quartz


Comments

Comment (Exploration): Status = Inactive

Comment (Geology): Geologic Description = This unnamed occurrence is a series of sheeted quartz-pyrite veins in Lower Cretaceous Kahiltna flysch adjacent to several, east-west-trending rhyolite dikes cutting the flysch (Bundtzen, Harris, and Gilbert, 1997). The quartz veins dip south and are parallel to the east-west-trending dikes. The Kahiltna flysch is locally thermally upgraded to slate. One sample contained 830 ppm arsenic, 180 ppb gold, and 710 ppm tungsten. A panned concentrate taken just below the mineralized dike swarm contained 1.00 percent tin and 1,400 ppm tungsten.

Comment (Reference): Primary Reference = This description

Comment (Workings): Workings / Exploration = The reporter visited and sampled the site in 1988; anomalous pan concentrate samples were collected by Ellen E. Harris. One sample of sheeted veining contained 830 ppm arsenic, 180 ppb gold, and 710 ppm tungsten. A panned concentrate taken just below the mineralized dike swarm contained 1.00 percent tin and 1,400 ppm tungsten (Bundtzen, Harris, and Gilbert, 1997).

Comment (Deposit): Model Name = Polymetallic vein (Cox and Singer, 1986; model 22c).


References

Reference (Deposit): Bundtzen, T.K., Harris, E.E., and Gilbert, W.G., 1997, Geologic Map of the eastern McGrath quadrangle, Alaska: Alaska Division of Geological and Geophysical Surveys Report of Investigations 97-14, 34 pages, one sheet, scale 1:125,000.


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