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SummaryIn states bordering the Gulf of Mexico and the Atlantic Ocean, vast areas of coastal land have been destroyed since the mid 1800s as a result of natural processes and human activities. The physical factors that have the greatest influence on coastal land loss are reductions in sediment supply, relative sea level rise, and frequent storms, whereas the most important human activities are sediment excavation, river modification, and coastal construction. As a result of these agents and activities, coastal land loss is manifested most commonly as beach/bluff erosion and coastal submergence. Wetlands are a unique class of coastal lands so they are considered independent of upland coastal areas. Wetlands are subjected to the same physical process and activities as other coastal lands, but they are also susceptible to deterioration as a result of biogeochemical processes. Failed reclamation projects and induced subsidence also contribute locally to wetland losses in the southeastern US. |
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