Abstract
The theory of geomorphology is much more stable than those of other earth sciences. There are two ways of the Earth surface presentation in geomorphology: (a) mathematical image as a two-dimensional plane with deformations in the third dimension; and (b) physical image as an intermediate layer between the lithosphere and mobile geospheres. The Earth relief includes a great deal of convergent forms. An elaboration of the origin of landforms would be of use for better understanding of the modern state and prospects for its future evolution.
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