El Paso

Prospect, Undetermined

Commodities and mineralogy

Main commodities Cu; Ni

Geographic location

Quadrangle map, 1:250,000-scale TR
Quadrangle map, 1:63,360-scale C-6
Latitude 58.5453
Longitude -133.7002
Nearby scientific data Find additional scientific data near this location
Location and accuracy This prospect is on the south flank of Kluchman Mountain near the Taku River. It is near the center of the S1/2 section 28, T.38 S., R.71 E. of the Copper River Meridian. The prospect was originally described in MAS/MILS record 0021130008; it is also listed as Alaska Kardex file number 113-011. This is location T004 of Wells and others (1986). The location is accurate within 1 mile.

Geologic setting

Geologic description

The El Paso prospect is in the Coast Range plutonic-metamorphic complex which consists of high-grade schist and gneiss intruded by Cretaceous and Tertiary granodiorite (Brew and Ford, 1984). Brew and Ford (1974) indicate that rocks at the prospect are shallow, tonalitic to granitic plutons that intrude and contact metamorphose high-grade, regionally metamorphosed, rocks derived from volcanic, pelitic and minor carbonate strata of unknown protolith age. Roof pendants of the metamorphic rocks are common, as are mafic and aplite dikes (Miller and others, 1997).
Wells, and others, 1986, report this as a Ni-Cu prospect. No other information is available. Claims were active from 1970 to 1976 (Wells and others, 1986).
Geologic map unit (-133.701943470636, 58.5449873979471)
Mineral deposit model Possible synorogenic-synvolcanic Ni-Cu (Cox and Singer, 1986; model 7a)
Mineral deposit model number 7a

Production and reserves

Workings or exploration Claims were active in 1970-1976 (Wells and others, 1986).
Indication of production None

References