Plunging cliffs, so called by Davis (1928, pp.151–154, 247, 272-274), are sea cliffs drowned at the base by rapid rise of sea level, which may be due in some cases to sinking of the land, but in most cases are the result of postglacial transgression. While this was generally not rapid enough to drown cliffs of soft materials, which would undergo erosion contemporaneously, hard-rock cliffs have commonly become plunging.
Davis included in this category examples in which the cliffs had been reduced in steepness by subaerial processes prior to drowning (Tutuila and Tahiti Islands, in the tropical Pacific). Subsequently to drowning, such cliffs, though initially plunging, have been notched by marine erosion. When, however, unmodified cliffs on rocks so hard that the cliffs are nearly vertical are drowned, the plunging cliffs are immune from attack by the sea at the new level, at any rate under certain conditions.
“It is clear that the persistence or survival of plunging cliffs in the shore...
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References
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Cotton, C.A. (1968). Plunging cliffs . In: Geomorphology. Encyclopedia of Earth Science. Springer, Berlin, Heidelberg. https://doi.org/10.1007/3-540-31060-6_293
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