Beaches.formed.some.names
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Beaches are the result of wave action by which waves or currents move sand or other loose sediments of which the beach is made as these particles are held in suspension. Alternatively, sand may be moved by saltation (a bouncing movement of large particles).
Types:
Dissipative.
Longshore bar and trough.
Rhythmic bar and beach.
Transverse bar and rip (TBR)
Low tide terrace.
Reflective.
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