Named presumably for Modoc Mountain near Morenci, Greenlee Co, AZ in Basin-and-Range province. No type locality designated. Occurs locally in the southern two-thirds of the Clifton quad, AZ. Rocks equivalent to Modoc are in the lower part of Tule Spring limestone. Overlies the Morenci formation (Devonian?). Dominantly gray, cliff-forming limestone. Some white or reddish calcareous quartzite and dolomite. Two measured sections. Petrologic analyses. Geologic map. About 170 ft thick. Fossils (corals, brachiopods) indicate an Early Carboniferous (Mississippian) age.
Source: GNU records (USGS DDS-6; Denver GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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