Mannie shale or shaly clay forms top of Richmond group in Tennessee River Valley. Is upper part of Fernvale formation. Described as brownish and bluish fossiliferous shaly clays, 16 to 35 ft thick. Overlies Leipers Creek limestone. Age is Late Ordovician.
Source: GNU records (USGS DDS-6; Reston GNULEX).
In GA, Mannie Member of Sequatchie Formation is only present along Taylor Ridge-Whiteoak Mountain where it is 27 m thick. Seems to occupy an erosional depression in the Shellmound Member. Consists of shales and bioturbated shaly sandstones, which are characterized by abundant trace fossils--CHONDRITES, TRICHOPHYCUS, SKOLITHOS, MONOCRATERION, and DIPLOCRATERION--and phosphatic granules. Unconformably underlies Red Mountain Formation. Depositional environment probably a quiet subtidal embayment.
Source: GNU records (USGS DDS-6; Reston GNULEX).
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