Name Pinchoulee Gneiss of Hatchet Creek Group applied to feldspathic and migmatitic biotite gneiss exposed along shores of Lake Jordan, Chilton Co., east-central AL. Unit forms narrow lithologic belt between Wedowee Group and Elkahatchee Quartz Diorite. Age is early and middle Paleozoic.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Pinchoulee Gneiss of the Hatchet Creek Group occurs in the northern Piedmont of east-central AL. Unit is a fine- to medium-grained feldspathic biotite gneiss, locally garnetiferous and commonly saturated with leucocratic granitoid dikes, sills, and plutons. Contains occasional zones of graphite-sericite-feldspar schist, hornblende quartzite, garnet quartzite, and thin amphibolite. Migmatitic along southeastern margin and along Coosa river. Overlies Hanover Schist, also of Hatchet Creek Group.
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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