The Antarctic coast may be classified as glacial tectonic and glacial erosional, because in its genesis the ice action was more important than the marine influence.
Many works have been written on Antarctic geology, but only a few have coastal morphologic importance. Among the first were Cailleux (1963), Adie (1964), and Markov et al. (1968–70); sea-level changes were studied by Adie (1964). An attempt at reconstitution of ancient coastal environments has been made by Araya and Hervé (1966).
Principal Parts of the Antarctic Coasts
Two principal parts are separated by means of a line that follows the Transantarctic Mountains lineament (Fig. 1). This lineament coincides with the eastern coast of the Weddell Sea and the western coast of the Ross Sea. The West Antarctic coast is strongly indented and delimited by the Ross and the Weddell seas. Three parts distinguish this coast: the Antarctic Peninsula is the most prominent and indented part of the coast. The coast of the Amundsen Sea, at...
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References
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Araya-Vergara, J.F. (1982). Antarctica, coastal morphology . In: Beaches and Coastal Geology. Encyclopedia of Earth Sciences Series. Springer, New York, NY. https://doi.org/10.1007/0-387-30843-1_16
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