Three-Dimensional Differentiation of Geological Medium is a Basis of the United System of the Exogenous Geological Processes
In the article is discussed the idea of the creation of the united system of the exogenous geological processes of the relief formation of land as the functional integrity of the infinite number of different-scale asynchronous displacements of the limited volumes of the rocks. On the base of general methodological approaches where analyzed the fundamental properties of geological medium for the logical comparison of the levels of the organization of the substance of lithosphere with the hierarchy of the contemporary landscapes of the within the framework specific three-dimensional limits (10-8-107 m) and the time intervals (10-7-1011 s). In the established time-spatial limits is proposed the content of the levels of the manifestation of the exogenous geological processes in the form of the integral co-subordinate system of the elements of the exogeodynamics.