Catastrophism, a term invented by William Whewell in 1832, is a school of thought that stands in antithesis to gradualism (q.v.). Itsproponents claim that the rates of geological and biological processes have in the past differed significantly from current rates, on occasions suddenly and violently assuming magnitudes not seen today and in doing so causing catastrophes.
In the inorganic world, it is expedient to recognize two brands of catastrophism: the old and the new. The old catastrophism was the ruling theory of Earth history before about 1830. It embodied many different ideas, but a common thread running through them was the recognition of one or more global, or nearly global, revolutions in Earth history, usually associated with world-wide floods and the collapse and crumpling of the Earth's crust. As gradualism waned in the middle of the 19th century, so catastrophist views became rather disreputable (Rudwick, 1992). During the present century, catastrophism has made a...
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Huggett, R. (1999). Catastrophism. In: Environmental Geology. Encyclopedia of Earth Science. Springer, Dordrecht. https://doi.org/10.1007/1-4020-4494-1_51
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