King Salmon River

The King Salmon River is a 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: King Salmon River  

State:  Alaska

County:  na

Elevation:

Commodity: Gold

Lat, Long: 60.31, -158.12000

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 King Salmon River

King Salmon River MRDS details

Site Name

Primary: King Salmon River


Commodity

Primary: Gold


Location

State: Alaska
District: Bristol Bay region


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: Placer Au-PGE


Orebody

Not available


Structure

Not available


Alterations

Not available


Rocks

Not available


Analytical Data

Not available


Materials

Ore: Gold


Comments

Comment (Geology): Age = Quaternary.

Comment (Geology): Geologic Description = Mertie (1938, p. 91) reported that coarse gold was found in the upper valley of the King Salmon River in1907. King Salmon River is a large west tributary to the Nushagak River. It flows east from headwaters along a low divide that separates it from the drainage of Tikchik River. Bedrock in the King Salmon River drainage is mid-Cretaceous clastic sedimentary rocks of the Kuskokwim Group locally intruded by Upper Cretaceous or Lower Tertiary granitic and hypabyssal felsic rocks. Clark and others (1970 [OF 438]) reported analytical data for stream sediments and one rock sample in the area of USGS benchmark King. Several of the stream-sediment samples in this area contained anomalous amounts of metals, including Ag, As, B, and Cu. The rock sample, from near the benchmark, contained weakly anomalous amounts of Ag and As. Bedrock in this area includes a small area of felsic intrusive rocks surrounded by hornfels (Clark and others, 1970 [OF 438]).

Comment (Deposit): Model Name = Placer Au-PGE (Cox and Singer, 1986; model 39a)

Comment (Reference): Primary Reference = Clark and others, 1970 (OF 438)

Comment (Exploration): Status = Inactive


References

Reference (Deposit): Cobb, E.H., 1976, Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Dillingham, Sleetmute, and Taylor Mountains quadrangles, Alaska: U.S. Geological Survey Open-File Report 76-606, 92 p.

Reference (Deposit): Mertie, J.B., Jr., 1938, The Nushagak district, Alaska: U.S. Geological Survey Bulletin 903, 96 p.

Reference (Deposit): Clark, A.L., Condon, W.H., Hoare, J.M., and Sorg, D.H., 1970, Analyses of rock and stream sediment samples from the Taylor Mountains C-8 quadrangle, Alaska: U.S. Geological Survey Open-File Report 438, 89 p.

Reference (Deposit): Cobb, E.H., 1972, Metallic mineral resources map of the Taylor Mountains quadrangle: U.S. Geological Survey Miscellaneous Field Studies Map MF-384, scale 1:250,000.

Reference (Deposit): Cobb, E.H., 1976, Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Dillingham, Sleetmute, and Taylor Mountain quadrangles, Alaska: U.S. Geological Survey Open-File Report 76-606, 92 p.


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