Горные реки и реки в горах: продольный профиль, морфология и динамика русел

Аннотация

Formation of the longitudinal river profile in the mountain regions and the causes and mechanisms of its deformation are under consideration. The formulas of equilibrium profile are given. According to the types of channel processes the mountain rivers in the strict sense may be distinguished from some large rivers in the mountain regions which are of plain type. Variants of channel processes zonality are described.