Kav

The Kav is a silver, copper, and antimony 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: Kav

State:  Alaska

County:  na

Elevation:

Commodity: Silver, Copper, Antimony

Lat, Long: 67.81, -156.76000

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Satelite View

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Satelite image of the Kav

Kav MRDS details

Site Name

Primary: Kav


Commodity

Primary: Silver
Primary: Copper
Primary: Antimony


Location

State: Alaska
District: Noatak


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: Kipushi Cu-Pb-Zn (BC name is Carbonate-hosted Cu)


Orebody

Not available


Structure

Not available


Alterations

Alteration Type: L
Alteration Text: Fe-staining


Rocks

Not available


Analytical Data

Not available


Materials

Ore: Azurite
Ore: Chalcopyrite
Ore: Malachite
Ore: Tennantite
Ore: Tetrahedrite


Comments

Comment (Reference): Primary Reference = Degenhart and others, 1978

Comment (Workings): Workings / Exploration = Two samples representative of mineralized dolomite breccia contained 18.6% Cu over 36 ft. (12 m) length, and 33.8% Cu over 50 ft. (17 m) length. One 4 to 6 in. (8 cm to 12 cm) wide quartz vein assayed 6.2% Cu, 0.62% Zn, 4.9 oz/ton (152g/ton) Ag, and 3.2% Sb. Another 40 ft. (13 m) chip sample across a stringer zone assayed 0.8% Cu, 0.48 oz/ton (15g/ton) Ag (Degenhart and others, 1978, p. 351-371).

Comment (Geology): Geologic Description = Four occurrences of Cu-Ag mineralization over 0.15 sq. mi. (200 m sq.) area. Most interesting occurrence is a fan-shaped area of mineralized talus ranging from 5 ft. to 10 ft. (1.3 m to 3 m) wide over a slope distance of 300 ft. (100 m) that consists of dolomite breccia containing masses of tetrahedrite, tennantite, chalcopyrite, malachite and azurite, mixed with fragments of quartz-vein material containing chalcopyrite. Other three occurrences are quartz veins generally 0.5 to 6 in. (1 cm to 12 cm) wide (one vein 1.5 ft. (0.3 m) wide) having strike lengths up to 75 ft. (15 m), and quartz stringer zones 40 ft. to 100 ft. (10.5 m to 30 m) wide, carrying tetrahedrite, chalcopyrite and malachite. Host rock is brecciated dolomite overlain by limestone and underlain by limestone, marble, and a sequence of phyllites; dolomite breccia forms prominent rust-colored hills (Degenhart and others, 1978, p.351-371)

Comment (Deposit): Other Comments = Three minor occurrences of malachite are present along the north slope of the mountain immediately southwest of Kav occurrence.?All occurrences are located within Noatak National Preserve.

Comment (Deposit): Model Name = Kipushi?

Comment (Exploration): Status = Inactive


References

Reference (Deposit): Degenhart, C.E., Griffis, R.J., McQuat, J.F., and Bigelow, C.G., 1978, Mineral studies of the western Brooks Range performed under contract to the U.S. Bureau of Mines, Contract #JO155089: U.S. Bureau of Mines Open-File Report 103-78, 529 p., 11 sheets.


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