Quaternary Deposits Undivided - Undifferentiated gray to buff sand and gravel, gray to brown lignitic silt and clay, occasional boulders, and rare shell beds. Surficial deposits occur as intercalated fluvial sands and marsh muds (e.g. in upstream floodplain of the Wicomico and Nanticoke Rivers), well-sorted, stablized dune sands (e.g. eastern Wicomico County), shell-bearing estuarine clays and silts (e.g. lower Dorchester County) and Pocomoke River basin of Worcester County), and beach zone sands (e.g. Fenwick and Assateague Islands). Wisconsin to Holocene in age. Subsurface deposits of pre-Wisconsin age consist of buff to reddish-brown sand and gravel locally incised into Miocene sediments (e.g. Salisbury area), estuarine to marine white to gray sands, and gray to blue, shell-bearing clays (e.g. Worcester County).
Kent Island Formation - Medium- to coarse-grained sand and sandy gravel grading upward into poorly- to well-sorted fine- to medium-grained sand, in part clayey and silty, at altitudes from sea level to about 20 ft. (top of unit).
Wachapreague Formation - Coarsening-upward sequence from lower muddy fine-grained sand to upper medium- to coarse-grained gravelly sand, at altitudes from sea level to about 15 ft. (top of unit).