Farewell Mineral Licks

The Farewell Mineral Licks is a copper, manganese, and iron 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: Farewell Mineral Licks  

State:  Alaska

County:  na

Elevation:

Commodity: Copper, Manganese, Iron

Lat, Long: 62.495, -153.60600

Map: View on Google Maps

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Satelite image of the Farewell Mineral Licks

Farewell Mineral Licks MRDS details

Site Name

Primary: Farewell Mineral Licks


Commodity

Primary: Copper
Primary: Manganese
Primary: Iron
Secondary: Sodium
Secondary: Potassium


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

Not available


Orebody

Not available


Structure

Not available


Alterations

Alteration Type: L
Alteration Text: Silicrete and ferricrete.


Rocks

Not available


Analytical Data

Not available


Materials

Gangue: Dolomite


Comments

Comment (Reference): Primary Reference = Bundtzen and others, 1997

Comment (Workings): Workings / Exploration = One soil sample taken at the Farewell Mineral Licks was anomalous in copper (250 ppm), manganese (8,500 ppm), potassium (6.50 percent) and sodium (12.00 percent).

Comment (Exploration): Status = Inactive

Comment (Deposit): Other Comments = See White Mountain Mercury Mine (MG025) and the Peggy Barbara (MG026) and Mary Margaret (MG027) prospects.

Comment (Geology): Ore Material = Iron oxides

Comment (Geology): Age = Quaternary, based on C14 age data summarized by Kline and Bundtzen (1986).

Comment (Deposit): Model Name = Unknown; possibly hot springs related.

Comment (Geology): Geologic Description = The Farewell Mineral Licks are a series of three subcircular areas of dark yellow-brown soils frequently utilized as mineral licks and roll areas by buffalo (Bison bison), moose (Alces alces), and other ungulates. Each 'lick' is approximately 40 meters in diameter, and composed of distinctive yellow-brown residual soils in Quaternary drift directly overlying the active strand of the Denali-Farewell fault, a major transcurrent fault that forms an arc across central Alaska and Yukon (Bundtzen, Harris, and Gilbert, 1997). A distinct silicrete rind covers soil at the site. Dolomite fragments were recognized in one soil sample. . One soil sample taken at the Farewell Mineral licks was anomalous in copper (250 ppm), manganese (8,500 ppm), potassium (6.50 percent), and sodium (12.00 percent). The manganese may be the result of decomposed dolomite. The remaining elements may be the result of a hydrothermal plumbing system within the Denali fault system.


References

Reference (Deposit): Kline, J.T., and Bundtzen, T.K., 1986, Two glacial records from west-central Alaska, in Hamilton, T.D., Reed, K.M., and Thorson, Robert, eds., Glaciation in Alaska: Alaska Geological Society Special Volume, p. 123-150.

Reference (Deposit): Bundtzen, T.K., Kline, J.T., and Clough, J.G., 1982, Preliminary geologic map of the McGrath B-2 quadrangle, Alaska: Alaska Division of Geological and Geophysical Surveys Open-File report 149, 22 pages, one sheet, scale 1:63,360.

Reference (Deposit): Kline, J.T., and Pinney, D.S., 1997, Derivative map of geological materials and hazards in the eastern half, McGrath quadrangle, Alaska: Alaska Division of Geological and Geophysical Surveys Report of Investigations 97-14b, one sheet, scale, 1:125,000.

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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