Halibut Bay 16G

The Halibut Bay 16G is a copper 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: Halibut Bay 16G  

State:  Alaska

County:  na

Elevation:

Commodity: Copper

Lat, Long: 57.35889, -154.59500

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 Halibut Bay 16G

Halibut Bay 16G MRDS details

Site Name

Primary: Halibut Bay 16G


Commodity

Primary: Copper


Location

State: Alaska
District: Kodiak


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: Synorogenic-synvolcanic Ni-Cu


Orebody

Not available


Structure

Not available


Alterations

Not available


Rocks

Not available


Analytical Data

Not available


Materials

Ore: Chalcopyrite
Ore: Pyrrhotite


Comments

Comment (Deposit): Model Name = Synorogenic-synvolcanic nickel-copper (Cox and Singer, 1986; model 7a?)

Comment (Reference): Primary Reference = Foley and Barker, 1985

Comment (Workings): Workings / Exploration = A grab sample contained 2000 ppm copper and traces of gold, platinum, and palladium.

Comment (Geology): Geologic Description = At this mineral occurrence, one of several within the Halibut Bay ultramafic complex, chalcopyrite and pyrrhotite are present within a 3-foot-wide zone of pyroxenite. A sample of this material contained 2,000 ppm copper and traces of gold, platinum, and palladium (Foley and Barker, 1985, table 14). Nickel content was not determined.? the Halibut Bay ultramafic complex, consisting mostly of dunite, gabbro, pyroxenite, and peridotite, occurs within sedimentary units of the Uyak formation of Cretaceous age.

Comment (Deposit): Other Comments = Site is located within Kodiak National Wildlife Refuge.

Comment (Exploration): Status = Inactive


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): Foley, J.Y., Burns, L.E., Schneider, C.L., and Forbes, R.B., 1989, Preliminary report of platinum group element occurrences in Alaska: Alaska Division of Geological and Geophysical Surveys Public Data File 89-20, 32 p., 1 map sheet, scale 1:2,500,000.


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