Unnamed (north of Glacier Bay Monument)

The Unnamed (north of Glacier Bay Monument) 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 (north of Glacier Bay Monument)

State:  Alaska

County:  na

Elevation:

Commodity: Molybdenum

Lat, Long: 59.21, -136.07000

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 (north of Glacier Bay Monument)

Unnamed (north of Glacier Bay Monument) MRDS details

Site Name

Primary: Unnamed (north of Glacier Bay Monument)


Commodity

Primary: Molybdenum


Location

State: Alaska
District: Juneau (Skagway subdistrict)


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

Name: Diorite
Role: Associated
Age Type: Associated Rock
Age Young: Late Cretaceous


Analytical Data

Not available


Materials

Ore: Molybdenite


Comments

Comment (Reference): Primary Reference = Winkler and MacKevett, 1970

Comment (Exploration): Status = Inactive

Comment (Geology): Geologic Description = Samples BD 548A and BD 548B of Winkler and MacKevett (1970) are described as 'Biotite granodiorite (?) with molybdenite disseminations'. Sample BD 548B contained 15 ppm Mo. The Cretaceous age of the host intrusive (Gilbert, 1988) establishes a maximum age for the deposit.

Comment (Deposit): Model Name = This is only an occurrence and there is very little information on it. The mineralization may be related to a porphyry copper system. The description from Winkler and MacKevett (1970) appears to be too mafic an association for a Climax type Mo deposit.

Comment (Geology): Age = The age is Cretaceous or younger, based upon the age of the host intrusive (Gilbert, 1988).


References

Reference (Deposit): Gilbert, W.G., 1988, Preliminary geology and geochemistry of the north Chilkat Range: Alaska Division of Geological and Geophysical Surveys Report of Investigations 88-8, 2 sheets, scale 1:36,200.

Reference (Deposit): Cobb, E.H., 1972, Metallic mineral resources map of the Skagway quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-424, 1 sheet, scale 1:250,000.

Reference (Deposit): Winkler, G.R., and MacKevett, E.M., Jr., 1970, Analyses of bedrock and stream-sediment samples from the Haines-Porcupine region, southeastern Alaska: U.S. Geological Survey Open-File Report 369, 91 p., 1 sheet, scale 1:125,000.

Reference (Deposit): Berg, H.C., 1984, Regional geologic summary, metallogenesis, and mineral resources of southeastern Alaska: U.S. Geological Survey Open-file Report 84-572, 298 p., 1 plate, scale approx. 1:600,000.


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