Cuspate foreland
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Cuspate forelands, also known as cuspate barriers or nesses in Britain, are geographical features found on coastlines and lakeshores that are created primarily by longshore drift. Formed by accretion
A cuspate foreland in Chicago, stabilised by vegetation
Fernando noronha
Longshore drift
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Longshore drift from longshore current is a geological process that consists of the transportation of sediments along a coast parallel to the shoreline, which is dependent on the angle of incoming wav
Cuspate foreland
…forelands, also known as cuspate barriers or nesses in Britain, are geographical features found on coastlines and lakeshores that are created primarily by longshore drift. Formed by accretion and progradation of sand and shingle, they extend outwards from the shoreline in a triangular shape. Some cuspate forelands may…
Provincetown Spit, at the northern end of Cape Cod, was formed by longshore drift after the end of the last Ice age.
Kaitorete Spit in the Canterbury Region of New Zealand's southern island.
Arcachon Bay in Southwest France.
Timber groyne from Swanage Bay, UK