Name Eulie shale applied at Bransford to soft argillaceous shale in three gray, yellowish, or greenish layers within the Chattanooga shale. Top layer at this locality consists of nodules. It is a single layer of greenish shale with nodules at the base at Westmoreland. Thickness 6 to 9 in. Overlies Gassaway shale (new); underlies Westmoreland shale (new). The Eulie and Westmoreland are complementary in their stratigraphic relations. The absence of either would make determination of the status of the other difficult. Age assigned is Early Mississippian.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Campbell considered his Eulie shale to be of Early Mississippian age, but present author classifies this gray to greenish-gray mudstone with phosphatic nodules as very late Devonian. Name Eulie shale is not used in present report. Beds named Eulie by Campbell are placed in Maury formation and not named.
Source: GNU records (USGS DDS-6; Reston GNULEX).
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