Keno

The Keno is a zinc, silver, lead, copper, and gold 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

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Site Name

Primary: Keno

Commodity

Primary: Zinc
Primary: Silver
Primary: Lead
Primary: Copper
Primary: Gold
Secondary: Barium-Barite

Location

State: Alaska
District: Hyder

Land Status

Not available

Holdings

Not available

Workings

Not available

Ownership

Not available

Production

Not available

Deposit

Record Type: Site
Operation Category: Prospect
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

Not available

Rocks

Not available

Analytical Data

Not available

Materials

Ore: Chalcopyrite
Ore: Galena
Ore: Pyrite
Ore: Sphalerite
Ore: Tetrahedrite
Gangue: Quartz

Comments

Comment (Deposit): Model Name = Polymetallic veins

Comment (Reference): Primary Reference = Buddington, 1929

Comment (Workings): Workings / Exploration = Early workings included a 50-foot adit.? An early assay, presumably of the best ore, showed 0.6 oz Au and 3 oz Ag per ton, and 48% Pb.

Comment (Geology): Geologic Description = The country rocks in the area of the Keno prospect are pelitic metasedimentary and subordinate andesitic metavolcanic strata of the Jurassic or older Mesozoic Hazelton, Group, which are underlain and locally intruded by the Triassic Texas Creek Granodiorite (Smith, 1977; Koch, 1996).? In 1925, Buddington (p. 94) described the deposit as quartz fissure veins 2-4 feet thick that cut granodiorite and contain galena and other sulfides. A specimen, presumably of the best ore, contained 0.6 oz Au and 3 oz Ag per ton, and 48% Pb. ? In 1929, Buddington (p. 108) reported an adit driven along a quartz vein up to 4.5 feet thick in Texas Creek Granodiorite. The vein had been traced on the surface for about 400 feet, and contained oreshoots of solid sulfides as much as 7 inches thick comprising galena, pyrite, chalcopyrite, sphalerite, and tetrahedrite. The quartz also carries disseminated pyrite and, locally, some barite.

Comment (Exploration): Status = Inactive

References

Reference (Deposit): Buddington, A.F., 1929, Geology of Hyder and vicinity, southeastern Alaska, with a reconnaissance of Chickamin River: U.S. Geological Survey Bulletin 807, 124 p.

Reference (Deposit): Smith, J.G., 1977, Geology of the Ketchikan D-1 and Bradfield Canal A-1 quadrangles, Alaska: U.S. Geological Survey Bulletin 1425, 49 p.

Reference (Deposit): Elliott, R.L., and Koch, R.D., 1981, Mines, prospects, and selected metalliferous mineral occurrences in the Bradfield Canal quadrangle, Alaska: U.S. Geological Survey Open-File Report 81-728-B, 23 p., 1 sheet, scales 1:250,000 and 1:63,360.

Reference (Deposit): Koch, R.D., 1996, Reconnaissance geologic map of the Bradfield Canal quadrangle, southeastern Alaska: U.S. Geological Survey Open-File Report 81-728-A, 35 p., 1 sheet, scale 1:250,000.

Reference (Deposit): Buddington, A.F., 1925, Mineral investigations in southeastern Alasaka: U.S. Geological Survey Bulletin 773, p. 71-139.

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