2000
DOI: 10.1002/1099-1085(200011/12)14:16/17<2991::aid-hyp131>3.0.co;2-h
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Hydrology, geomorphology and vegetation of Coastal Plain rivers in the south-eastern USA

Abstract: Rivers of the Coastal Plain of the southeastern United States are characteristically low-gradient meandering systems that develop broad floodplains subjected to frequent and prolonged flooding. These floodplains support a relatively unique forested wetland (Bottomland Hardwoods), which have received considerable ecological study, but distinctly less hydrogeomorphic study. The hydroperiod, or annual period of inundation, largely controls the development of characteristic fluvial landforms, sediment deposition, … Show more

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Cited by 233 publications
(233 citation statements)
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“…scale by channel-floodplain geomorphology, which promotes spatial variability on sedimentation load and patterns for a given river section during a specific flood event (Hupp, 2000;Noe and Hupp, 2005;Piégay et al, 2008). At this scale, previous studies have indicated that distance from the main channel exerts more influence on spatial variability of overbank sedimentation than downstream variation (Walling and He, 1998;Middelkoop and Asselman, 1998;Thonon et al, 2007).…”
Section: Introductionmentioning
confidence: 99%
“…scale by channel-floodplain geomorphology, which promotes spatial variability on sedimentation load and patterns for a given river section during a specific flood event (Hupp, 2000;Noe and Hupp, 2005;Piégay et al, 2008). At this scale, previous studies have indicated that distance from the main channel exerts more influence on spatial variability of overbank sedimentation than downstream variation (Walling and He, 1998;Middelkoop and Asselman, 1998;Thonon et al, 2007).…”
Section: Introductionmentioning
confidence: 99%
“…The northern portion of the region is dominated by longleaf pine (Pinus palustris) and loblolly pine (Pinus taeda). The SAMBI is bounded on its western edge at the Fall Line where alluvial and marine sediments meet the exposed continental bedrock of the Piedmont region (Hupp 2000) and on the eastern edge by the Atlantic Ocean. The southern SAMBI is in a transitional zone of northeastern Florida where tropical mangroves meet coastal plain plant communities; this region is dominated by pond pine (Pinus serotina) and Atlantic white cedar (Chamaecyparis thyoides; Watson and McWilliams 2005).…”
Section: Study Areamentioning
confidence: 99%
“…The Coastal Plain physiographic region of the southeast USA (Fenneman, 1928(Fenneman, , 1938Vigil, 2000) covers more than 1 million km 2 , greater than the combined area of France, Germany, and the UK (Hupp, 2000). The Coastal Plain extends from New Jersey to eastern Texas and is primarily the result of alluvial (from adjacent mountain and Piedmont regions) and marine deposits of Late Cretaceous and Holocene age (Fenneman, 1928(Fenneman, , 1938Hupp, 2000;Vigil, 2000).…”
Section: Coastal Plain Geology and Hydrologic Implicationsmentioning
confidence: 99%