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The debate involving how cuspate forelands form is ongoing.<ref name="McNinch and Luettich, 2000 ">McNinch, J. E., and Luettich, R. A., 2000. Physical processes around a cuspate foreland: implications to the evolution and long-term maintenance of a cape-associated shoal. ''Continental Shelf Research. '' 20, pp. 2367–2389.</ref> However, the most widely accepted process of formation involves [[long shore drift]].<ref name="Craig-Smith, 2005"/> Where longshore drift occurs in opposite directions, two [[Spit (landform)|spit]]s merge into a triangular protrusion along a coastline or lakeshore.<ref name="Craig-Smith, 2005"/> Their formation is also dependent on dominant and prevailing winds working in opposite directions.<ref name="Craig-Smith, 2005"/> Formation can also occur when waves are [[diffract]]ed around a barrier.<ref>Woodroffe, C. D., 2002. ''Coasts: form, process and evolution.'' UK: Cambridge University Press.</ref> |
The debate involving how cuspate forelands form is ongoing.<ref name="McNinch and Luettich, 2000 ">McNinch, J. E., and Luettich, R. A., 2000. Physical processes around a cuspate foreland: implications to the evolution and long-term maintenance of a cape-associated shoal. ''Continental Shelf Research. '' 20, pp. 2367–2389.</ref> However, the most widely accepted process of formation involves [[long shore drift]].<ref name="Craig-Smith, 2005"/> Where longshore drift occurs in opposite directions, two [[Spit (landform)|spit]]s merge into a triangular protrusion along a coastline or lakeshore.<ref name="Craig-Smith, 2005"/> Their formation is also dependent on dominant and prevailing winds working in opposite directions.<ref name="Craig-Smith, 2005"/> Formation can also occur when waves are [[diffract]]ed around a barrier.<ref>Woodroffe, C. D., 2002. ''Coasts: form, process and evolution.'' UK: Cambridge University Press.</ref> |
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Cuspate forelands can form both along coastlines and along lakeshores. Those formed along coastlines can be in the lee of an offshore island, along a coastline that has no islands in the vicinity, or at a stream mouth where disposition occurs.<ref name="Bird, 2008 ">Bird, E., 2008 ''Coastal geomorphology: an introduction.'' 2nd ed. England: John Wiley & Sons Ltd.</ref> |
Cuspate forelands can form both along coastlines and along lakeshores, hehe. Those formed along coastlines can be in the lee of an offshore island, along a coastline that has no islands in the vicinity, or at a stream mouth where disposition occurs.<ref name="Bird, 2008 ">Bird, E., 2008 ''Coastal geomorphology: an introduction.'' 2nd ed. England: John Wiley & Sons Ltd.</ref> |
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===Formation in narrow straits or on open coastlines=== |
===Formation in narrow straits or on open coastlines=== |
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Greek: Ά ά Έ έ Ή ή Ί ί Ό ό Ύ ύ Ώ ώ Α α Β β Γ γ Δ δ Ε ε Ζ ζ Η η Θ θ Ι ι Κ κ Λ λ Μ μ Ν ν Ξ ξ Ο ο Π π Ρ ρ Σ σ ς Τ τ Υ υ Φ φ Χ χ Ψ ψ Ω ω {{Polytonic|}}
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