geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-3503Research ArticleНаучные сообщенияShort communicationsОвражная эрозия в межгорных котловинах Юго-Западного ПрибайкальяGully erosion in the intermountain basins of South-West PribaikalyeРыжовЮ. В.RyzhovYu. V.Институт географии СО РАН, ИркутскРоссия199821122023038592Copyright © Рыжов Ю.В., 20232023Рыжов Ю.В.Ryzhov Y.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/3503

Gully's dissection in the depressions of the region is weak to moderate. Farming land of the piedmont tilt plains and slopes of the mountain spurs are most erodible. Four types of gully's evolution are established: l - hasty growth during short period of time and rapid decrease of the rate of development, 2 - active growth during several decades, 3 - thickening of gully because of growth of branches (gully's system formation), 4 - changeover from regressive stage of development to active one.

Gully's dissection in the depressions of the region is weak to moderate. Farming land of the piedmont tilt plains and slopes of the mountain spurs are most erodible. Four types of gully's evolution are established: l - hasty growth during short period of time and rapid decrease of the rate of development, 2 - active growth during several decades, 3 - thickening of gully because of growth of branches (gully's system formation), 4 - changeover from regressive stage of development to active one.

References

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