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diastrophism

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di⋅as⋅tro⋅phism

[dahy-as-truh-fiz-uhm]
–noun Geology.
1. Also called tectonism. the action of the forces that cause the earth's crust to be deformed, producing continents, mountains, changes of level, etc.
2. any such resulting deformation.

Origin:
1880–85; < Gk diastroph() a distortion (see dia-, strophe ) + -ism


di⋅a⋅stroph⋅ic [dahy-uh-strof-ik, -stroh-fik] , adjective
di⋅a⋅stroph⋅i⋅cal⋅ly, adverb
Dictionary.com Unabridged
Based on the Random House Dictionary, © Random House, Inc. 2009.
Cite This Source Link To diastrophism
di·as·tro·phism   (dī-ās'trə-fĭz'əm)   
n.  The process of deformation by which the major features of the earth's crust, including continents, mountains, ocean beds, folds, and faults, are formed.

[From Greek diastrophē, distortion, from diastrephein, to distort : dia-, apart; see dia- + strephein, to twist; see streb(h)- in Indo-European roots.]
di'a·stroph'ic (dī'ə-strŏf'ĭk, -strō'fĭk) adj.
The American Heritage® Dictionary of the English Language, Fourth Edition
Copyright © 2009 by Houghton Mifflin Company.
Published by Houghton Mifflin Company. All rights reserved.
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