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Continental shelves have been greatly influenced by Quaternary events, particularly those of the Pleistocene Epoch. Detailed United States Coast and Geodetic Survey shelf and slope soundings off eastern United States from Georges Bank to North Carolina made it possible for Veatch and Smith (1939) to direct attention to various geomorphic forms in this region. Veatch and Smith (1939, p. 13) found that generally the shelf surface showed northeast-southwest trending bars and lagoons with occasional prominent terraces all of which are of marine origin or altered by marine erosion. South of New York numerous shelf linear ridges and depressions have been described as comparable to the barrier islands and their inner lagoons that extend along much of the coast (Shepard, 1963, p. 213), to relict Pleistocene shoreline forms (Sanders, 1962, p. 278), and to sand swells forming at present during intense storms (Uchupi, 1968, p. C17) .

Probable Holocene Transgressive Effects on the Geomorphic Features of the Continental Shelf off New Jersey, United States