Teay formation described as gravel, sand, and finely laminated clay deposited by ancient Kanawha River. Thickness 0 to 600 ft. Forms floor of Teay Valley, Cabell Co., WV.
Source: GNU records (USGS DDS-6; Reston GNULEX).
"Since both the Gallia Sand and the Minford Clay were deposited prior to or during the Lake Tight period in the Teays Valley, they are commonly grouped and classified as Teays Formation."
Source: GNU records (USGS DDS-6; Reston GNULEX).
Authors state that term Teay is considered archaic and that the preferred term is Teays. Teays Formation consists of the lower Gallia Sand Member and the upper Minford Silt Member. Paleomagnetic and stratigraphic data indicate that Minford is early Pleistocene. Fullerton (1986) also placed the Minford and other members of the Teays Formation in the early Pleistocene.
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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