Dean Swamp Member of Wicomico Formation. Upper Wicomico divided into five members: Toney Bay, Dean Swamp, Sandridge, Wassamassaw Swamp, and Four Hole. [Dean Swamp is] a clay member developed from northwest toward southeast with decreasing coarse- and medium-grained sand similar to that occurring in Toney Bay Member and then increasing fine sand. Drill-hole samples show definite thin laminations over about 10 to 20 feet of sample. Member represents lagoonal and tidal marsh sediments deposited after deposition of Sandridge Member. Age is early Pleistocene.
Named from Dean Swamp, Eutawville quadrangle, eastern SC.
Source: US geologic names lexicon (USGS Bull. 1350, p. 196).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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