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COASTAL DEPOSITIONAL FEATURES
GEOL 1033
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DEPOSITIONAL COASTAL LANDFORMS are varied and often associated with each other:
beaches sand bars sand spits tombolos beach ridges beach cusps cuspate forelands barrier islands coastal sand dunes washover fans salt marshes tidal flats lagoons and bays tidal deltas river deltas
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MAJOR OCEANIC MATERIAL INPUTS
Input source input amount Rivers % Glaciers % Windblown dust % Coastal erosion (higher than ave. locally) 1% Volcanic debris <1% Groundwater flow <2%
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A well-defined, lobate sediment plume is seen emerging from a river source on this stretch of wave-dominated (beach-fronted) Atlantic coastline. Currents are starting to carry some of the sediment northward in the offshore environment. Note the broad, well-"fed" beaches in the direction of sediment transport and narrower, retreated beaches in the opposite direction. Typically, river input and cliff erosion are the major sources of sediment for a coastline (Space Shuttle, March 1994).
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WAVE-DOMINATED NILE DELTA
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Maps of some US barrier island coastlines
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Plum Island, Mass. Plum Island, northeastern Massachusetts, low altitude, oblique, aerial view of barrier island with beach-dune ridge showing washovers, vegetated backdunes, & back-barrier marsh with tidal channels (16 July 1975).
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Sand Spits at the Down Drift ends of Barrier Islands
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Beach ridges on a barrier island
McLaughlin's Beach (southwest end of Ninety Mile Beach), Victoria, Australia Recent Low altitude, oblique, aerial view of low-angle truncation of multiple beach-dune ridges (chenier ridges). This once prograding coastline was retreating, at least locally when this picture was taken (1976).
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Development on a Barrier Island
Ocean City, Maryland, U.S.A. Modern Beach island modification: Ocean City, a developed barrier island. Host to 8 million visitors a year, this city (and others similarly situated) has no effective protection against flooding and damage from severe storms.
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