geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-3050Research ArticleСтатьиArticleРасчлененность рельефа как показатель интенсивности эрозионных процессов (на примере северных и восточных регионов Европейской России)Dissection of topography as an index of erosion rate (a case study of northern and eastern regions of European Russia)МаккавеевА. Н.MakkaveevA. N.СетунскаяЛ. Е.SetunskayaL. E.ВолховаИ. М.VolkovaM. I.Институт географии РАНRussian Federation19930202202302Геоморфология2231Copyright © Маккавеев А.Н., Сетунская Л.Е., Волхова И.М., 20232023Маккавеев А.Н., Сетунская Л.Е., Волхова И.М.Makkaveev A.N., Setunskaya L.E., Volkova M.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/3050

Cartometric measurements of depth and density of dissection revealed differentiation in the dissection character and intensity between main orographic elements of northern and eastern European Russia. Specific features of the dissection pattern have been linked to geology, elevation, history of development and degree of agricultural cultivation. An erosional hazard has been estimated from the relief's morphometric indices, which is important in particular for regions with insufficient observation data on erosion.

Cartometric measurements of depth and density of dissection revealed differentiation in the dissection character and intensity between main orographic elements of northern and eastern European Russia. Specific features of the dissection pattern have been linked to geology, elevation, history of development and degree of agricultural cultivation. An erosional hazard has been estimated from the relief's morphometric indices, which is important in particular for regions with insufficient observation data on erosion.

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