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  • of the tributary influence on the trunk stream etc.). Delta formation in the junctions appeared to be controlled by solid runoff and backwater phenomena. Specific conditions are required to form fill-in delta, prograding delta or other morphological types of river
  • The paper discusses the mountain streams channels formation at the Western Tien Shan, differing in mudflow frequency, channel morphology, alluvium composition and biogenous factor contribution to rock particles destruction. Biogenous destruction
  • Mudflows' impact on the mountain rivers channel processes is discussed, the processes' features proved to be different within the zones of mudflows formation, transit and deposition| the channel morphology depends on the form of the mudflow deposits