geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-2684Research ArticleНаучные сообщенияShort communicationsСовременная овражная эрозия на востоке Русской равниныRecent gully erosion at the east of the Russian PlainБутаковГ. П.ButakovG. P.ДвинскихА. П.DvinskikhA. P.НазаровН. Н.NazarovN. N.РысинИ. И.RysinI. I.Казанский государственный университетРоссия19871511202202Геоморфология4347Copyright © Бутаков Г.П., Двинских А.П., Назаров Н.Н., Рысин И.И., 20222022Бутаков Г.П., Двинских А.П., Назаров Н.Н., Рысин И.И.Butakov G.P., Dvinskikh A.P., Nazarov N.N., Rysin I.I.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/2684

Long-term stationary observation and aerial photos interpretation as well as the analysis of earlier published data revealed pulsating-decaying character of the gullies growth at the eastern Russian Plain during 1954 to 1985 yrs. Mean annual growth rate varies from 0.40 to 4.20 meters per year depending on rocks lithology. 70 to 80% of total growth occurs during the spring. Gullies within the region remain active for about 15 to 20 yars.

Long-term stationary observation and aerial photos interpretation as well as the analysis of earlier published data revealed pulsating-decaying character of the gullies growth at the eastern Russian Plain during 1954 to 1985 yrs. Mean annual growth rate varies from 0.40 to 4.20 meters per year depending on rocks lithology. 70 to 80% of total growth occurs during the spring. Gullies within the region remain active for about 15 to 20 yars.

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