Parker

The Parker 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: Parker

State:  Alaska

County:  na

Elevation:

Commodity: Gold

Lat, Long: 64.89, -148.05806

Map: View on Google Maps

Satelite View

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Satelite image of the Parker

Parker MRDS details

Site Name

Primary: Parker


Commodity

Primary: Gold


Location

State: Alaska
District: Fairbanks


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

Not available


Rocks

Not available


Analytical Data

Not available


Materials

Ore: Gold


Comments

Comment (Exploration): Status = Inactive

Comment (Reference): Primary Reference = Stewart, 1933

Comment (Workings): Workings / Exploration = The Parker vein was developed by a number of open cuts and by a 70-foot-deep inclined shaft (Stewart, 1933, p. 145). In 1933, drifting along the vein began, both to the north and south, on the 50-foot level below the shaft (Stewart, 1933, p. 145).

Comment (Deposit): Other Comments = Also see the Blue Bonanza mine (FB006).

Comment (Geology): Geologic Description = This occurrence consists of an irregular, 1- to 6-inch-thick, gold-bearing quartz vein oriented N. 15 E., dipping 55 W. (Chapman and Foster, 1969, p. D19; Stewart, 1933, p. 145). The quartz is coarsely crystalline and contains small amounts of metallic sulfides (Stewart, 1933, p. 145). Bedrock in this area, on the northern flanks of Ester Dome, consists of two units of the Fairbanks Schist: a quartz-muscovite schist and an amphibolite-biotite schist (Newberrry and others, 1996). The vein was developed by a number of open cuts and by a 70-foot-deep inclined shaft (Stewart, 1933, p. 145).

Comment (Deposit): Model Name = Schist-hosted gold-quartz vein


References

Reference (Deposit): Chapman, R.M., and Foster, R.L., 1969, Lode mines and prospects in the Fairbanks district, Alaska: U.S. Geological Survey Professional Paper 625-D, 25 p., 1 plate.

Reference (Deposit): Newberry, R.J., Bundtzen, T.K., Clautice, K.C., Combellick, R.A., Douglas, T., Laird, G.M., Liss, S.A., Pinney, D.S., Reifenstuhl, R.R., and Solie, D.N., 1996, Preliminary geologic map of the Fairbanks mining district, Alaska: Alaska Division of Geological and Geophysical Surveys Public Data File 96-16, 17 p., 2 sheets, scale 1:63,360.

Reference (Deposit): Cobb, E.H., 1972, Metallic mineral resources map of the Fairbanks quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-410, 1 sheet, scale 1:250,000.

Reference (Deposit): Stewart, B.D., 1933, Mining investigations and mine inspection in Alaska, Biennium ending March 31, 1933: Alaska Territorial Department of Mines Annual Report 1933B, 196 p.

Reference (Deposit): Cobb, E.H., 1976, Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Fairbanks quadrangle, Alaska: U.S. Geological Survey Open-File Report 76-662, 174 p.


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