Diastrophism is considered an internal geomorphic process.

Name: Diastrophism is considered an internal geomorphic process.
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Diastrophism is a group of processes that involve the deformation, fracturing, and displacement of Earth's crust. These are internal processes that occur within the Earth's lithosphere and are responsible for the formation of mountain ranges, rift valleys, and other large-scale features. Therefore, diastrophism is considered an internal geomorphic process.

Diastrophism Is Considered an Internal Geomorphic Process