geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-1618Research ArticleНаучные сообщенияShort communicationsОб интенсивности позднеголоценового склонового смыва на Среднерусской возвышенностиOn the slope wash intensity at the Middle Russian Heights in Late HoloceneСеребряннаяТ. А.SerebryannayaT. A.

SPIN-код: 6826-7046

sheremetskaya@gmail.comИнститут географии АН СССРРоссия19761504202201Геоморфология9498Copyright © Серебрянная Т.А., 20222022Серебрянная Т.А.Serebryannaya T.A.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/1618

The complex analysis of paleobotanic and radiocarbon data confirms the erosion processes (slope wash in particular) to be intensified at the central part of the Middle Russian Heights in t-he last centuries due to human economic activity together with recent tectonic uplift. The factors resulted in drainage of swamp (existed since sub-boreal time) and their covering with deluvial mantle, the age of the latter is estimated at 200 years, the deluvial wash rate being about 4-6 mm per year.

The complex analysis of paleobotanic and radiocarbon data confirms the erosion processes (slope wash in particular) to be intensified at the central part of the Middle Russian Heights in t-he last centuries due to human economic activity together with recent tectonic uplift. The factors resulted in drainage of swamp (existed since sub-boreal time) and their covering with deluvial mantle, the age of the latter is estimated at 200 years, the deluvial wash rate being about 4-6 mm per year.

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