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336 PROCESS AND FORM


























               Figure 13.15 Factors affecting dune morphology. For explanation, see text.
               Source: Adapted from Pye (1990)




              tide levels. As well as major tidal channels, tidal creeks  to form when tidal flats are high enough to permit col-
              flow across tidal flats.These are shallower than tidal chan-  onization by salt-tolerant terrestrial plants. Depending
              nelsandrundowntolow-tidelevel.Onmuddytidalflats,  on their degree of exposure, salt marshes stretch from
              tidal creeks often display a dendritic pattern with wind-  around the mean high-water, neap-tide level to a point
              ing courses and point bars. On sandy tidal flats, tidal  between the mean and extreme high-water, spring-tide
              creeks have ill-defined banks, straight courses, and few  levels. Their seaward edge abuts bare intertidal flats, and
              tributaries.                              their landward edge sits where salt-tolerant plants fail
                Tidal flats are built up from clay-sized and fine silt-  to compete with terrestrial plants. Salt marsh sediments
              sized sediments carried to the coast by rivers. On meeting  are typically heavy or sandy clay, silty sand, or silty peat.
              salt water, particles of clay and silt flocculate (form clot-  Many salt marshes contain numerous shallow depres-
              likeclusters)tobecomelargeraggregates.Theythensettle  sions, or pans, that are devoid of vegetation and fill with
              out as mud in quiet coastal waters such as lagoons and  water at high spring tides.
              sheltered estuaries.The mud is carried in by the incoming
              tide and deposited before the tide reverses. If the mud
              continues to build upwards, a part of the tidal flat will
              be exposed just above normal high-tide level. This area  Mangals
              is then open to colonization by salt-tolerant plants, and  ‘Mangrove’ is a general term for a variety of mainly
              salt marshes or mangroves may develop.    tropical and subtropical salt-tolerant trees and shrubs
                                                        inhabiting low inter-tidal areas. Mangals are communi-
              Salt marshes                              ties of mangroves – shrubs and long-lived trees and with
                                                        associated lianas, palms, and ferns – that colonize tidal
              Salt marshesarewidespreadintemperateregions,butare  flats in the tropics, and occur in river-dominated, tide-
              not uncommon in the tropics (Figure 13.19). They start  dominated, and wave-dominated coastal environments
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