three classification of internal movement
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On the basis of their velocity, the internal movements are classified as follows: a. Slow movements: The movements which occur continuously and lead to the formation of mountains and continents are known as slow movements.
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Explanation: Endogenic movements are divided into diastrophic movements and sudden movements. ... Diastrophic movements are further classified into epeirogenic movements (continent forming ― subsidence, upliftment) and orogenic movements (mountain building ― folding, faulting).
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