Unnamed (on Cascade Inlet)

The Unnamed (on Cascade Inlet) is a lead, copper, gold, and silver 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 (on Cascade Inlet)

State:  Alaska

County:  na

Elevation:

Commodity: Lead, Copper, Gold, Silver

Lat, Long: 55.174, -131.37300

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 (on Cascade Inlet)

Unnamed (on Cascade Inlet) MRDS details

Site Name

Primary: Unnamed (on Cascade Inlet)


Commodity

Primary: Lead
Primary: Copper
Primary: Gold
Primary: Silver


Location

State: Alaska
District: Ketchikan


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: Polymetallic veins


Orebody

Not available


Structure

Not available


Alterations

Alteration Type: L
Alteration Text: Sericitization of trondhjemite country rock.


Rocks

Not available


Analytical Data

Not available


Materials

Ore: Pyrite
Ore: Galena
Ore: Chalcopyrite
Gangue: Quartz


Comments

Comment (Deposit): Model Name = Polymetallic veins (Cox and Singer, 1986; model 22c)

Comment (Geology): Geologic Description = The country rock at this site is Silurian trondhjemite (Berg, 1972 [I 684]; Berg and others, 1988). In this area, the trondhjemite is schistose and sericitized, probably owing to regional greenschist-grade metamorphism in Late Cretaceous time. The occurrence consists of sulfide-bearing quartz fissure veins up to 6 feet thick in sheared, sericitized trondhjemite. Sulfide minerals include galena, and, based on sample analyses, probably chalcopyrite and pyrite. Samples of the sulfide-bearing quartz veins contained up to 14 ppm Au, 5 ppm Ag, 1500 ppm, Cu, and 300 ppm Pb (Karl, 1992, loc. 26).

Comment (Workings): Workings / Exploration = Samples of the sulfide-bearing quartz veins contained up to 14 ppm Au, 5 ppm Ag, 1500 ppm, Cu, and 300 ppm Pb (Karl, 1992, loc. 26).

Comment (Reference): Primary Reference = Karl, 1992

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


References

Reference (Deposit): Karl, S.M., 1992, Map and table of mineral deposits on Annette Island, Alaska: U.S. Geological Survey Open-File Report 92-690, 57 p., 1 map, scale 1:63,360.

Reference (Deposit): Berg, H.C., 1972, Geologic map of Annette Island, Alaska: U.S. Geological Survey Miscellaneous Geologic Investigations Map I-684, 8 p., 1 sheet, scale 1:63,360,


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