geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-3488Research ArticleНаучные сообщенияShort communicationsМеханизм овражной эрозии и динамика русловых формGully erosion mechanism and dynamics of channel formsВеретенниковаМ. В.VeretennikovaM. V.Московский государственный университет имени М.В.Ломоносова, географический факультетРоссия199818122023026675Copyright © Веретенникова М.В., 20232023Веретенникова М.В.Veretennikova M.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/3488

The results of multiannual investigations of water runoff and solid flow in the typical gylly catch basins are discussed. The test site was chosen in the central part of European Russia. Some regular features of gully channel process are established in the test site with the rocks of different density and granulometric composition. Quantitative characteristics of channels morphometry and ephemeral flood streams hydraulics are found. Some field data of gully's debris cone formation in the valley of Protva River are represented.

The results of multiannual investigations of water runoff and solid flow in the typical gylly catch basins are discussed. The test site was chosen in the central part of European Russia. Some regular features of gully channel process are established in the test site with the rocks of different density and granulometric composition. Quantitative characteristics of channels morphometry and ephemeral flood streams hydraulics are found. Some field data of gully's debris cone formation in the valley of Protva River are represented.

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