Unnamed (near summit of Gold Hill)

The Unnamed (near summit of Gold Hill) is a molybdenum 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 (near summit of Gold Hill)

State:  Alaska

County:  na

Elevation:

Commodity: Molybdenum

Lat, Long: 63.096, -147.75000

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 (near summit of Gold Hill)

Unnamed (near summit of Gold Hill) MRDS details

Site Name

Primary: Unnamed (near summit of Gold Hill)


Commodity

Primary: Molybdenum


Location

State: Alaska
District: Valdez Creek


Land Status

Not available


Holdings

Not available


Workings

Not available


Ownership

Not available


Production

Not available


Deposit

Record Type: Site
Operation Category: Prospect
Operation Type: Unknown
Years of Production:
Organization:
Significant:


Physiography

Not available


Mineral Deposit Model

Model Name: Porphyry Mo, low-F


Orebody

Not available


Structure

Not available


Alterations

Not available


Rocks

Not available


Analytical Data

Not available


Materials

Ore: Molybdenite
Gangue: Quartz


Comments

Comment (Deposit): Model Name = Porphyry Mo(?) (Cox and Singer, 1986; model 21b)

Comment (Deposit): Other Comments = See also HE172 and HE173.

Comment (Geology): Geologic Description = The country rocks in the area of this prospect are deformed and metamorphosed Lower Cretaceous and Upper Jurassic turbidites (Wilson and others, 1998) cut by Lower Tertiary to Upper Cretaceous(?) diorite and quartz monzonite (Smith and others, 1988). The deposit is in metasedimentary and altered intrusive rocks, and consists of widely-spaced zones of disseminated molybdenite. This deposit probably is related to other porphyry-type deposits in the Gold Hill area (HE172 and HE173).

Comment (Workings): Workings / Exploration = This prospect has been explored by soil sampling and trenching. At least two shallow drill holes totaling 220 feet, were completed in the 1970's (D.L. Stevens, oral communication, 1999). Geophysical exploration has included a regional aeromagnetic survey over the prospect and surrounding area, as well as ground magnetics, IP, and EM.

Comment (Geology): Age = Probably Late Cretaceous or younger.

Comment (Reference): Primary Reference = Balen and others, 1991

Comment (Exploration): Status = Inactive


References

Reference (Deposit): Balen, M.D., and others, 1991, Executive summary of the Bureau of Mines investigations in the Valdez Creek mining district, Alaska: U.S. Bureau of Mines Special Publication, 43 p.

Reference (Deposit): Kurtak, J.M., Southworth, D.D., Balen, M.D., and Clautice, K.H., 1992, Mineral investigations in the Valdez Creek mining district, south-central Alaska: U.S. Bureau of Mines Open-File Report 1-92, 659 p., 2 plates, scale 1:250,000.

Reference (Deposit): Smith, T.E., Kline, G.L., Kline, J.T., and Coursey, N.D., 1975, Analyses of rock and stream-sediment samples, Healy A-2 quadrangle, south-central Alaska: Alaska Division of Geological and Geophysical Surveys Open-File Report AOF69, 2 sheets, scale 1:63,360.

Reference (Deposit): Balen, M.D., 1990, Geochemical sampling results from the Bureau of Mines Investigations in the Valdez Creek mining district, Alaska: U.S. Bureau of Mines Open-File Report 34-90, 218 p., 2 plates, scale 1:250,000.

Reference (Deposit): Wilson, F.H., Dover, J.H., Bradley, D.C., Weber, F.R., Bundtzen, T.K., and Haeussler, P.J., 1998, Geologic map of central (interior) Alaska: U.S. Geological Survey Open-File Report 98-133, 17 p., 2 sheetsm, scale 1:500,000.


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