geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-3516Research ArticleСтатьиArticleЭрозия в аридных зонахErosion in the arid zonesДедковА. П.DedkovA. P.Казанский государственный университет, географический факультетРоссия19982512202304312Copyright © Дедков А.П., 20232023Дедков А.П.Dedkov A.P.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/3516

Little precipitation combines with abundance of different and fresh erosion forms in the arid countries. Global data analysis doesn't confirm the conclusion about semiarid maximum of solid run-off. Only rive erosion forms may be thought of as the relics of pluvial epochs. Numerous forms made by ephemeral channel and non-channel flows are the result of recent erosion of extreme intensity. Show outbreaks of erosion are succeeded by enduring dry periods of weak denudation. This provides good preservation and freshness of erosion forms in arid zones.

Little precipitation combines with abundance of different and fresh erosion forms in the arid countries. Global data analysis doesn't confirm the conclusion about semiarid maximum of solid run-off. Only rive erosion forms may be thought of as the relics of pluvial epochs. Numerous forms made by ephemeral channel and non-channel flows are the result of recent erosion of extreme intensity. Show outbreaks of erosion are succeeded by enduring dry periods of weak denudation. This provides good preservation and freshness of erosion forms in arid zones.

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