Unnamed (northeast of Camelback Mountain)

Prospect, Inactive

Commodities and mineralogy

Main commodities Ag; As
Other commodities Cd; Ni; Pb; Sb; Zn
Ore minerals arsenopyrite; pyrite
Gangue minerals quartz

Geographic location

Quadrangle map, 1:250,000-scale ID
Quadrangle map, 1:63,360-scale C-3
Latitude 62.56679
Longitude -157.32656
Nearby scientific data Find additional scientific data near this location
Location and accuracy This prospect is about 1.7 mile north-northeast of Camelback Mountain on a broad summit of a northeast-trending ridge The occurrence is at an elevation of about 2,100 feet, about 0.5 mile north-northwest of the center of section 34, T. 29 N., R. 43 W., of the Seward Meridian. The location is accurate.

Geologic setting

Geologic description

This prospect consists of a zone of quartz-sulfide veins with gradational boundaries in hornfels. The occurrence is adjacent to a small monzonite body that intrudes both the Upper Cretaceous, Kuskokwim Group and andesitic flows of the Iditarod volcanics (Bundtzen, Laird, and Lockwood, 1988; Miller and Bundtzen, 1994; Miller, Bundtzen, and Gray, 2005). The size of the deposit is unknown. One grab sample of chips from a quartz-sulfide vein contained 12.0 parts per million (ppm) silver, 15.00 percent iron, 710 ppm arsenic, 600 ppm zinc, 500 ppm lead, 70 ppm antimony, 4,200 parts per billion (ppb) mercury, 35 ppm cadmium, and 300 ppm nickel (McGimsey and others, 1988).
Geologic map unit (-157.328927727301, 62.5661072050048)
Mineral deposit model Polymetallic vein (Cox and Singer, 1986; model 22c).
Mineral deposit model number 22c
Age of mineralization Unknown; the Camelback Mountain intrusion about a mile to the south is 73.2 Ma (Bundtzen, Laird, and Lockwood, 1988).
Alteration of deposit Silicification.

Production and reserves

Workings or exploration The area was sampled by the U.S. Geological Survey in the 1980s (McGimsey and others, 1988).
Indication of production None