geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-3506Research ArticleНаучные сообщенияShort communicationsПроцессы рельеф образования в перигляциалах плейстоцена и современные формы эрозионного рельефаRelief formation processes in the periglacial zones of Pleistocene and recent forms of erosion reliefХруцкийС. В.KchroutskyS. V.СеменовО. П.SemenovO. P.КосцоваЭ. В.KostsovaE. V.Воронежский госагроуниверситет им. К.Д. ГлинкиРоссия19982112202303104108Copyright © Хруцкий С.В., Семенов О.П., Косцова Э.В., 20232023Хруцкий С.В., Семенов О.П., Косцова Э.В.Kchroutsky S.V., Semenov O.P., Kostsova E.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/3506

Gullys and balkas of European Middle Russia have many features of their distribution and structure, which are predefined by relief formation during multifold periglacial epochs of Pleistocene. Solifluction had especially large impact. It developed on the slopes of valleys and balkas, where erodible loams accrued, and resulted in asymmetric profile of erosion forms. Regeneration of normal erosion relief occurred at final stages of periglacial epochs.

Gullys and balkas of European Middle Russia have many features of their distribution and structure, which are predefined by relief formation during multifold periglacial epochs of Pleistocene. Solifluction had especially large impact. It developed on the slopes of valleys and balkas, where erodible loams accrued, and resulted in asymmetric profile of erosion forms. Regeneration of normal erosion relief occurred at final stages of periglacial epochs.

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