geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-3523Research ArticleНаучные сообщенияShort communicationsМорфодинамические типы и эволюция русел рек Патомского нагорья в плейстоценеMorphodynamic types and evolution of river mouths at Patomskoye upland during PleistoceneВиноградоваО. В.VinogradovaO. V.МаорсЛ. В.MaorsL. V.Московский государственный университет имени М.В.Ломоносова, географический факультетРоссия199826122023044854Copyright © Виноградова О.В., Маорс Л.В., 20232023Виноградова О.В., Маорс Л.В.Vinogradova O.V., Maors L.V.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://geomorphology.igras.ru/jour/article/view/3523

Morphodymanic types of mountain and semi-mountain river channels, depend on complex of geologic-geomorphologic factors. The stability of the latter during several Pleistocene erosion cycles in those parts of river valleys, which have not undergone restructuring, has led to strong inheritance in the development of morphodynamic types of channels. The stability of tributary mouth zones and their evolution are controlled by morphodynamic type and lateral deformations of main river channel. The evolution of tributary mouths and their vicinity effects the morphology of the main river and confluence points.

Morphodymanic types of mountain and semi-mountain river channels, depend on complex of geologic-geomorphologic factors. The stability of the latter during several Pleistocene erosion cycles in those parts of river valleys, which have not undergone restructuring, has led to strong inheritance in the development of morphodynamic types of channels. The stability of tributary mouth zones and their evolution are controlled by morphodynamic type and lateral deformations of main river channel. The evolution of tributary mouths and their vicinity effects the morphology of the main river and confluence points.

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The authors declare that there are no conflicts of interest present.