geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-3160Research ArticleНаучные сообщенияShort communicationsКоличественная оценка современной интенсивности овражной эрозии в бассейне ВолгиQuantitative estimation of the recent gully erosion rate in the Volga drainage basinЗоринаЕ. Ф.ZorinaE. F.ЛюбимовБ. П.LyubimovB. P.НикольскаяИ. И.NikolskayaI. I.ПрохороваС. Д.ProkhorovaS. D.Московский государственный университет имени М.В.Ломоносова, географический факультетРоссия199404032023046470Copyright © Зорина Е.Ф., Любимов Б.П., Никольская И.И., Прохорова С.Д., 20232023Зорина Е.Ф., Любимов Б.П., Никольская И.И., Прохорова С.Д.Zorina E.F., Lyubimov B.P., Nikolskaya I.I., Prokhorova S.D.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/3160

The work is the first attempt to present a cartographic interpretation and analysis of slope deposits yield by gully network within the Volga drainage basin. The material yield was calculated from the data on gully growth rate, their density and average dimensions. The obtained values of the gully network growth rate are of considerable interest, as one of principal components of erosion-accumulation process within drainage basin of different order.

The work is the first attempt to present a cartographic interpretation and analysis of slope deposits yield by gully network within the Volga drainage basin. The material yield was calculated from the data on gully growth rate, their density and average dimensions. The obtained values of the gully network growth rate are of considerable interest, as one of principal components of erosion-accumulation process within drainage basin of different order.

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