Informally named the Pringletown beds in the Charleston, SC area. Consists of dark-bluish-gray to dark-gray clayey sand, silty to sandy clay, and fine- to medium-grained sand. Also contains clay-rich and peat beds. Unit is present only in the subsurface. Thickness is 3 meters. Overlies the Raysor Formation and underlies the Waccamaw(?) Formation. The Pringletown is of late Pliocene and early Pleistocene age.
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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