Wide Bay

The Wide Bay 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: Wide Bay  

State:  Alaska

County:  na

Elevation:

Commodity: Copper

Lat, Long: 53.91667, -166.65000

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 Wide Bay

Wide Bay MRDS details

Site Name

Primary: Wide Bay


Commodity

Primary: Copper


Location

State: Alaska
District: Aleutians


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: Silicification is the only form of alteration other than oxidation described. Leaching ranges from moderate to intense.


Rocks

Not available


Analytical Data

Not available


Materials

Ore: Chalcopyrite
Ore: Pyrite


Comments

Comment (Reference): Primary Reference = Christie, 1974

Comment (Workings): Workings / Exploration = Brief reconnaissance mapping and collection of one silt sample yielding background results for copper, molybdenum, zinc, silver, and gold.

Comment (Geology): Geologic Description = This is a very small (100 by 200 ft, 30 by 60 m) color anomaly localized along andesite dikes that cut volcanic flows and pyroclastic rocks of the Unalaska Formation (see Drewes and others, 1961). Chalcopyrite and pyrite occurs as disseminations in narrow envelopes in wall rocks surrounding the dikes which trend 300x (N30xE) and dip steeply south. Oxidation obscures original textures and may have obliterated evidence of primary chalcopyrite. Very minor chalcopyrite remains. Fracturing is moderately developed.

Comment (Exploration): Status = Inactive

Comment (Geology): Age = Miocene or younger


References

Reference (Deposit): Drewes, Harold, Fraser, G.D., Snyder, G.L., and Barnett, H.F., Jr., 1961, Geology of Unalaska Island and adjacent insular shelf, Aleutian Islands, Alaska: U.S. Geological Survey Bulletin 1028-S, p. 583-676.

Reference (Deposit): Christie, J.S., 1974, Aleut-Quintana-Duval 1974 joint venture, final report: Unpublished Quintana Minerals Corporation report, 24 p., 3 appendices, 2 maps. (Report held by the Aleut Corporation, Anchorage, Alaska.)


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