Final answer:
Diastrophism is considered true as a set of internal geomorphic processes, involved in shaping the Earth's crust and influencing its topography. It is linked with the movements and forces within the Earth's tectonic plates, contributing to the geological activity observed today and in the geological past.
Step-by-step explanation:
Diastrophism is indeed considered a set of internal geomorphic processes. This relates to how the Earth's crust is shaped and re-shaped by internal forces, such as the movements of the Earth's tectonic plates. Diastrophism includes processes like folding, faulting, warping, and volcanism that can alter the Earth's topography over time. The main answer to the question is that the statement is True. Diastrophism contributes to the geological activity, such as the formation of mountains, valleys, and other significant geological structures.Explanation in more than 100 words: Using the principle of uniformitarianism, geologists can interpret ancient plate tectonic activity by studying Earth's topography, since the processes that shape our planet today are the same that occurred in the past. Diastrophism is a result of plate tectonics and involves the deformation of the Earth's crust due to tectonic forces. This concept explains not only the present formation of geological features but also allows us to infer past geological events and formations associated with plate tectonics. Therefore, diastrophism is connected with both plate tectonics and the resulting topography.Conclusion Diastrophism encompasses the various slow-moving internal processes that continually reshape the Earth's surface. It is a key concept in understanding the geological structures we observe today, as well as those from the geologic past. As such, stating that diastrophism is a set of internal geomorphic processes is accurate.