Diastrophism is considered a set of internal geomorphic processes.

Name: Diastrophism is considered a set of internal geomorphic processes.
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Diastrophism refers to the processes of deforming or uplifting the earth's crust through internal forces such as tectonic activity, volcanism, and earthquakes. These processes are internal to the earth and involve movements of rock and sediment within its layers. Therefore, diastrophism is regarded as a set of internal geomorphic processes.

Diastrophism Is Considered a Set of Internal Geomorphic Processes