Named for exposures in the lower part of Copper Creek, southwest corner Klondyke quad, Ts7 and 8S, R18E, Pinal Co, AZ in the Basin-and-Range province. Crops out over an area of about 2 sq mi in quad. Extends more than 3 mi farther south into Galiuro Mountains quad. No type locality designated. Forms slopes and smoothly rounded hills and ridges. Is a medium-grained greenish-gray to pale red granodiorite. Varies in mineralogical composition and appearance from place to place. Is porphyritic. Is composed of plagioclase feldspar, quartz, potassium feldspar, and biotite. Detailed petrographic description. Intrudes Precambrian?, Paleozoic, and Mesozoic rocks. Is unconformably overlain by Galiuro Volcanics. Of Late Cretaceous and early Tertiary age. K-Ar age on biotite yielded age of 68 m.y. Geologic map.
Source: GNU records (USGS DDS-6; Denver GNULEX).
Considered to be Late Cretaceous in age in this report, Pinal Co, AZ in the Basin-and-Range province, on basis of 68 m.y. K-Ar age reported earlier by Simons (1964).
Source: GNU records (USGS DDS-6; Denver GNULEX).
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