Chapter
Apr 26, 2012
Geologic Framework of the Long Bay Inner Shelf: Implications for Coastal Evolution in South Carolina
Authors: Walter Barnhardt [email protected], Jane Denny [email protected], Wayne Baldwin [email protected], William Schwab [email protected], Robert Morton [email protected], Paul Gayes [email protected], and Neal Driscoll [email protected]Author Affiliations
Publication: Coastal Sediments '07
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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© 2007 American Society of Civil Engineers.
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Published online: Apr 26, 2012
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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]
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]
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]
Scripps Institution of Oceanography, La Jolla, CA 92093. E-mail: [email protected]
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