Definition
Holocene coastal geomorphology is a geoscience discipline dealing with materials (rock, sediments), forms, and forming processes (anorganic and organic) in the overlapping fringe between marine and terrestrial environments (called “littoral ”) during the Holocene period, in particular the time frame of a postglacial high sea level over the last about 7000 years to modern times. It is a wide field of science, with certainly tens of thousands of related publications. A text on this subject therefore has to be restricted to some general points.
Normally forming processes on Earth need time measured in geological scales (i.e., many thousands to millions of years) to show adequate results with mature forms. In contrast to this general rule, all coastal forms are not older than 6000–8000 years, when oceans again reached modern levels from a low-stand near −120 m during the last cold phase with extended glaciers (last glacial maximum (LGM) : Nicholls and Cazenave 2010; Scheffers...
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Kelletat, D.H. (2017). Holocene Coastal Geomorphology. 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_171-2
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DOI: https://doi.org/10.1007/978-3-319-48657-4_171-2
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