geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-2161Research ArticleНаучные сообщенияShort communicationsРоль овражной эрозии в формировании речных перекатовRole of gully erosion in the river shallows formationЗоринаЕ. Ф.ZorinaE. F.ПрохороваС. Д.ProkhorovaS. D.ЧаловР. С.ChalovR. S.Московский государственный университет имени М.В.Ломоносова, Географический факультетРоссия20001607202204Геоморфология7683Copyright © Зорина Е.Ф., Прохорова С.Д., Чалов Р.С., 20222022Зорина Е.Ф., Прохорова С.Д., Чалов Р.С.Zorina E.F., Prokhorova S.D., Chalov R.S.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/2161

The origin of river shallows due to sediment washout from the active gullybalka systems is under consideration. The opinion that linear erosion has strong negative influence on the channel conditions and navigation is based on the analysis of pilot maps and archive materials. The detailed description of shallows of the Middle Don and its depth dynamic is given.

The origin of river shallows due to sediment washout from the active gullybalka systems is under consideration. The opinion that linear erosion has strong negative influence on the channel conditions and navigation is based on the analysis of pilot maps and archive materials. The detailed description of shallows of the Middle Don and its depth dynamic is given.

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