Unconformable on all underlying units, fluvial sand and gravel at base, grading upwards into fine sands and silts, local peat. May be overrun with recent sediments from forest cutting and agriculture.
One of the older coastal terrace sequences in the Carolinas. Equivalent to Windsor Fm.
Similar to Cape May, broad lateral extent underlying terraces in the Carolinas; swamps and ridges on terrace surface were originally barrier islands and back bays. Superimposed on these landforms are swarms of Carolina bays.
Low coastal formation in Carolinas like Penholoway but younger and lower in altitude.
Another Carolina costalized terrace of early-middle Pleistocene age. Deeply weathered.