Avan River

The Avan River is a chromium 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: Avan River

State:  Alaska

County:  na

Elevation:

Commodity: Chromium

Lat, Long: 68.24, -161.93000

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 Avan River

Avan River MRDS details

Site Name

Primary: Avan River


Commodity

Primary: Chromium
Secondary: Nickel


Location

State: Alaska
District: Noatak


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: Podiform chromite (minor)


Orebody

Not available


Structure

Not available


Alterations

Not available


Rocks

Not available


Analytical Data

Not available


Materials

Ore: Chromite


Comments

Comment (Exploration): Status = Inactive

Comment (Geology): Age = Jurassic

Comment (Workings): Workings / Exploration = None

Comment (Reference): Primary Reference = Degenhart and others (1978)

Comment (Geology): Geologic Description = The geology at the Avan River occurrence is dominated by a Jurassic? ultramafic complex approximately 300 square miles in area, that structurally overlies a variety of Paleozoic and Mesozoic marine sedimentary rocks. The assemblages are characterized by extremely complex folding and faulting. The chromite occurs as small layers or bands and as disseminated grains in the north-central part of ultramafic complex. Pyrrhotite and pentlandite have been identified in polished sections of a few samples of chromite-bearing rocks.

Comment (Deposit): Model Name = Lode; podiform chromite


References

Reference (Deposit): Foley, J.Y., and Barker, J.C., 1985, Chromite deposits along the Border Ranges fault, part 1, Field investigations and descriptions of chromite deposits: U.S. Bureau of Mines Information Circular 8990, 58 p.

Reference (Deposit): Cobb, E.H., Mayfield, C.F., and Brosge, W.P., 1981, Summaries of data on and lists of references to metallic and selected nonmetallic mineral occurrences in eleven quadrangles in northern Alaska (Arctic, Baird Mountains, Chandler Lake, DeLong Mountains, Demarcation Point, Howard Pass, Misheguk Mountain, Mount Michelson, Noatak, Point Lay, and Table Mountain); Supplement to Open-File Report 75-628; Part A, Summaries of data to January 1, 1981: U.S. Geological Survey Open-File Report 81-767-A, 25 p.

Reference (Deposit): Grybeck, D.J., 1977, Known mineral deposits of the Brooks Range, Alaska: US Geological Survey Open-File Report 77-166C, 41 p., 1 sheet, scale 1:1,000,000.

Reference (Deposit): Degenhart, C.E., Griffis, R.J., McQuat, J.F., and Bigelow, C.G., 1978, Mineral studies of the western Brooks Range performed under contract to the U.S. Bureau of Mines, Contract #JO155089: U.S. Bureau of Mines Open-File Report 103-78, 529 p., 11 sheets.


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