Kami

Prospect, Inactive

Commodities and mineralogy

Main commodities Cu
Ore minerals chalcopyrite
Gangue minerals quartz

Geographic location

Quadrangle map, 1:250,000-scale MK
Quadrangle map, 1:63,360-scale D-2
Latitude 58.8759
Longitude -154.5552
Nearby scientific data Find additional scientific data near this location
Location and accuracy The Kami prospect is at an elevation of about 2,750 feet on a glacier-covered mountaintop about two miles southeast of lake 1410 at the head of Little Kamishak River. This is location 3 of MacKevett and Holloway (1977). The site is in the NE1/4 sec. 14, T. 15 S., R. 32 W., of the Seward Meridian; the location is accurate to within one-quarter mile.

Geologic setting

Geologic description

The Kami prospect consists of chalcopyrite-bearing quartz veins in a roof pendant of sedimentary rocks of the Jurassic Naknek Formation that are above a Tertiary(?) quartz diorite stock. There is little information on the mineralization but there is a geochemical anomaly in copper (values unknown) in stream sediment and rock samples (MacKevett and Holloway, 1977; Cobb, 1980; Church and others, 1992). Bear Creek Mining Company investigated claims in 1971.
Geologic map unit (-154.557262885213, 58.8752117935946)
Mineral deposit model Polymetallic vein (Cox and Singer, 1986; model 22c).
Mineral deposit model number 22c
Age of mineralization Late Jurassic or younger; chalcopyrite-bearing quartz veins cut the Naknek Formation.

Production and reserves

Workings or exploration Bear Creek Mining Company investigated claims in 1971.
Indication of production None

References