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dc.contributor.advisorMcKenzie, Garry D.en_US
dc.creatorSchrock, Laura L.en_US
dc.date.accessioned2016-10-28T16:21:27Z
dc.date.available2016-10-28T16:21:27Z
dc.date.issued1986en_US
dc.identifier.urihttp://hdl.handle.net/1811/78838
dc.description.abstractShoals along the Middle Atlantic Bight are divided into two major groups, linear shoals and arcuate shoals. Linear shoals include shoreface-connected shoals and isolated shoals. Arcuate shoals are either cape-associated or inlet associated. Excellent examples of linear and cape-associated shoals are found off of the coast of North Carolina. Three hypotheses for the origin of shoals are presented. All are based on a rise in sea level and the subsequent shoreface retreat. Modern hydraulics, in the form of waves and currents, appear to influence the formation of shoals.en_US
dc.language.isoen_USen_US
dc.publisherThe Ohio State Universityen_US
dc.relation.ispartofseriesThe Ohio State University. Department of Geology and Mineralogy Senior Theses; 1986en_US
dc.titleAn expanded definition of shoals along the Middle Atlantic Bight, North Americaen_US
dc.typeThesisen_US
dc.description.embargoNo embargoen_US


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