Unnamed (summit of The Cone)

Occurrence, Probably inactive

Commodities and mineralogy

Main commodities Fe
Other commodities Ti
Ore minerals magnetite

Geographic location

Quadrangle map, 1:250,000-scale IL
Quadrangle map, 1:63,360-scale C-3
Latitude 59.5313
Longitude -153.8437
Nearby scientific data Find additional scientific data near this location
Location and accuracy This occurrence is centered on the 3,028-foot summit of The Cone west of Ursus Cove. The occurrence is in the NE1/4 sec. 34, T. 7 S., R. 27 W., Seward Meridian, and the location is accurate within about 0.5 mile. The occurrence is number 31 of MacKevett and Holloway (1977).

Geologic setting

Geologic description

This occurrence consists of magnetite(?) in Jurassic quartz diorite (Detterman and Reed, 1980). Immediately north and west of The Cone, the quartz diorite intrudes the Permian(?) to Jurassic Kakhonak metamorphic complex and Upper Triassic Cottonwood Bay Greenstone. Locally, the quartz diorite includes phases as mafic as diorite. Numerous claims were staked in the area, but there is no information about the claims other than that they appear to have been located for a magnetic iron deposit.
Geologic map unit (-153.845839557862, 59.5306357116697)
Age of mineralization Jurassic or younger (Detterman and Reed, 1980).

Production and reserves

Workings or exploration Exploration probably is limited to reconnaissance geologic mapping and collecting surface samples. Numerous claims were staked in the area (U.S. Bureau of Mines, 1973; MacKevett and Holloway, 1977).
Indication of production None

References

References

Reporters C.C. Hawley, Hawley Resource Group, Anchorage, Alaska
Last report date 6/7/2003