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J Chapter 2 The Littoral Power Gradient and Shoreline
Probable Causes of Shoreline Recession
11 other sections not shown
accretion barrier island barrier system beach face beach profiles berm Bermuda calcarenite Cape Hatteras changes channel cliffs coastal plain slope coastline continental shelf continental shelf slope Core Banks crest currents delta deposits developed discharge dune dune ridge early Paget environment eolian eroded erosion estuary facies Figure Fire Island flood foresets foreshore geomorphic geomorphology gradient Holocene indicate Inlet Johnson lagoon landward littoral drift Long Island longshore longshore drift Lucia marine material maximum migration morphology nearshore occur ocean offshore Outer Banks overwash Paget eolianites period Pleistocene present progradation reefs Richards Bay River salt marsh scarps sea level seaward sediment sedimentary segment sequence shoreline South Shore Spice Hill spit stabilized storm study area sub-Paget submerged surface surveys terrace tide transgression transport transverse bars unit velocity vertical wave action wind zone Zululand Zululand coast