Erin shale named. Described as black carbonaceous shale or slate exposed in vicinity of Erin, Clay Co., eastern AL. Weathers gray or dirty white. Thickness tentatively estimated as 2,000 ft. Contains fossil plants of Carboniferous (probably Pennsylvanian) age. Heretofore included in Talladega slate.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Author follows usage of Cook (1982) who uses the name as Erin Slate Member of Lay Dam Formation. Carboniferous lycopods reported by Smith (1903) have been re-examined and their ages confirmed; attempts to recollect the fossils have been unsuccessful (Gastaldo and Cook, 1982). Erin is thinly foliated, variably carbonaceous phyllite with dominant slaty cleavage (Gastaldo and Cook, 1982). Cook (1982) shows Erin almost entirely separated from rest of Lay Dam Formation by thrust fault. Author questions whether or not stratigraphic order may be reversed and whether metamorphism therefore is Alleghanian rather than Acadian.
Source: GNU records (USGS DDS-6; Reston GNULEX).
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