Lithodynamic basins of different rank on the earth surface

The article is devoted to the problem of structuring the earth's surface, taking into account the local denudation basis functioning in the thalwegs nodes, and the limits of the hydro- and lithodynamic flows action. Using this information litodynamic basins are identified, which are morphologically expressed by funnels of different ranks. There are two types of their ranking. Each lithodynamic basin has two slope coordinates. One of them is the main one, and the other is dependent. At the same time, the transit flow has the ability to rebuild if necessary. A unified system of lithodynamic basins developing on the earth's surface is shown. The practical importance their is reflects.