Definition
The term “coastal zone” is used in scientific papers to describe the coastal environment or the region between the foreshore and the upper supratidal along a coastline. “Zones” in geoscience, however, are latitude-parallel belts between the equator and the poles, established in the first order by the different radiation/insolation on our globe.
Nearly all macro-patterns on Earth, which depend on climatic influences, like vegetation, soil formation, or forms of relief and inherent processes, show a zonal distribution. For the latter, including both relic and contemporary systems, this has been accepted for decades (Murphy 1968), and the term “climatic geomorphology” has therefore been established. Regarding coastal features and processes, however, these are looked upon for a long time mostly as a zonal , because cliffs, beaches, lagoons and barriers, deltas, etc. can be found in all latitudes; and rock-depending forms are regarded as a zonal,...
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Kelletat, D.H. (2017). Geographical Coastal Zonality. In: Finkl, C., Makowski, C. (eds) Encyclopedia of Coastal Science . Encyclopedia of Earth Sciences Series. Springer, Cham. https://doi.org/10.1007/978-3-319-48657-4_150-2
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