Abstract

The inner continental shelf off northern South Carolina is a sediment-limited environment characterized by extensive hardground areas, where coastal plain strata and ancient channel-fill deposits are exposed at the sea floor. Holocene sand is concentrated in large shoals associated with active tidal inlets, an isolated shore-detached sand body, and a widespread series of low-relief sand ridges. The regional geologic framework is a strong control on the production, movement and deposition of sediment. High-resolution geologic mapping of the sea floor supports conceptual models indicative of net southwestward sediment transport along the coast.

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Published In

Go to Coastal Sediments '07
Coastal Sediments '07
Pages: 2151 - 2160

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Published online: Apr 26, 2012

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Walter Barnhardt [email protected]
U.S. Geological Survey, 384 Woods Hole Rd, Woods Hole, MA 02543. E-mail: [email protected]
U.S. Geological Survey, 384 Woods Hole Rd, Woods Hole, MA 02543. E-mail: [email protected]
Wayne Baldwin [email protected]
U.S. Geological Survey, 384 Woods Hole Rd, Woods Hole, MA 02543. E-mail: [email protected]
William Schwab [email protected]
U.S. Geological Survey, 384 Woods Hole Rd, Woods Hole, MA 02543. E-mail: [email protected]
Robert Morton [email protected]
U.S. Geological Survey, 600 4th Street South, St. Petersburg, FL 33701. E-mail: [email protected]
Coastal Carolina University, 1270 Atlantic Avenue, Conway, SC 29526. E-mail: [email protected]
Neal Driscoll [email protected]
Scripps Institution of Oceanography, La Jolla, CA 92093. E-mail: [email protected]

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