Introduction
The south coast of Cornwall is more subdued and indented than the north coast, and receives waves generated by winds across the English Channel as well as south-westerly ocean swell from the Atlantic (Bird 1998). Wave action is generally light to moderate, with large storm waves arriving only occasionally. Mean spring tide range averages 4.7–4.8 m.
Slope-over-wall profiles have steep vegetated slopes descending to rocky cliffs that are usually less than 10 m high (Arber 1949). The proportion of rocky cliff to coastal slope is less than on much of the north coast, but on the western side of the Lizard Peninsula, exposed to Atlantic swell and storm waves, vertical cliffs rise locally to 50–70 m. Headlands and promontories correspond with higher ground or harder outcrops, the intervening bays and coves occupying lower ground or softer outcrops. The coastline runs in along the sides of several large branching inlets known as rias, formed where the sea has invaded the lower...
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Arber M (1949) Cliff profiles of Devon and Cornwall. Geogr J 114:191–197
Bird ECF (1998) The coasts of Cornwall. Alexander Publications, Fowey, Cornwall
Everard CE (1960) Mining and shoreline evolution near St. Austell, Cornwall. Trans Roy Geol Soc Cornwall 19:199–219
Ranwell DS (1974) The salt marsh to tidal woodland transition. Hydrobiol Bull 8:139–151
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(2010). Cornwall: The South Coast of Cornwall. In: Bird, E.C.F. (eds) Encyclopedia of the World's Coastal Landforms. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-8639-7_68
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DOI: https://doi.org/10.1007/978-1-4020-8639-7_68
Publisher Name: Springer, Dordrecht
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