geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-2193Research ArticleНаучные сообщенияShort communicationsПроцессы современной денудации в Восточных КарпатахPresent-day denudation processes at the Eastern CarpathiansАнаньевГ. С.AnanyevG. S.Московский государственный университет имени М.В.Ломоносова, Географический факультетРоссия19803008202201Геоморфология6371Copyright © Ананьев Г.С., 20222022Ананьев Г.С.Ananyev G.S.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/2193

Many paleo-geomorphological concepts (including conclusions on origin and age of planation sutfaces, interfluvial areas etc.) are based on some ideas about importance and type of denudation processes. In the Eastern Carpathians like in most part of middle mountains a set of denudation processes works: water stream and mudflows, mass movement, avalanches, biogenic processes, wind action, splash erosion, chemical denudation. Stationary observations of the processes during several years allowed to estimate the processes intensity and total value of the material removed by denudation.

Many paleo-geomorphological concepts (including conclusions on origin and age of planation sutfaces, interfluvial areas etc.) are based on some ideas about importance and type of denudation processes. In the Eastern Carpathians like in most part of middle mountains a set of denudation processes works: water stream and mudflows, mass movement, avalanches, biogenic processes, wind action, splash erosion, chemical denudation. Stationary observations of the processes during several years allowed to estimate the processes intensity and total value of the material removed by denudation.

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