geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-2265Research ArticleНаучные сообщенияShort communicationsСкорость роста оврагов (по наблюдениям в Курской области)Rate of gullies growth (a ease of Kursk region)СкомороховА. И.SkomorokhovA. I.Юго-Западная комплексная геологоразведочная экспедицияРоссия19810809202201Геоморфология97103Copyright © Скоморохов А.И., 20222022Скоморохов А.И.Skomorokhov A.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/2265

Studies of numerous gullies in the Kursk region and measurement of their annual growth revealed that their evolution was controlled by its own internal regularities. The external factors are only responsible for complex of favorable or unfavorable conditions. The following varieties of coastal gullies are distinguished: active, slowly growing, latent, activated. The active phase is only about 1/4 of the whole duration of the gully erosion cycle.

Studies of numerous gullies in the Kursk region and measurement of their annual growth revealed that their evolution was controlled by its own internal regularities. The external factors are only responsible for complex of favorable or unfavorable conditions. The following varieties of coastal gullies are distinguished: active, slowly growing, latent, activated. The active phase is only about 1/4 of the whole duration of the gully erosion cycle.

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