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Evaluation of the Paleodenudation Rates in the Mountains: Main Approaches and Results

https://doi.org/10.31857/S2587556620050076

Abstract

The article systematizes methods for studying modern and paleodenudation rates and summarizes the published data on the paleodenudation intensity obtained using 10Be and a set of methods for studying lake sediments for mountainous areas of different regions of the world. It has been shown that currently the most studied territories in terms of assessing paleodenudation rates are the European Alps, Tibet, the Rocky Mountains, and the Andes. Paleodenudation rates determined for river and lake catchments in various parts of the world vary over a wide range in the interval 2–3240 m/106 years. Similarly to the regularities revealed for modern denudation, there is a high correlation between the paleodenudation rates and the catchments slopes. Nevertheless, the local landscape features of specific river basins and their changes during the Holocene determine the spatial variability and dynamics of changes in the denudation rate over time. The role of human activity intensifies and leads to a 10 to 100-fold increase in the denudation of mountainous areas, primarily within the foothills and low mountains.

About the Authors

A. M. Grachev
Institute of Geography, Russian Academy of Sciences
Russian Federation
Moscow


V. N. Golosov
Institute of Geography, Russian Academy of Sciences; Lomonosov Moscow State University
Russian Federation

Faculty of Geography

Moscow



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Grachev A.M., Golosov V.N. Evaluation of the Paleodenudation Rates in the Mountains: Main Approaches and Results. Izvestiya Rossiiskoi Akademii Nauk. Seriya Geograficheskaya. 2020;84(5):704–714. (In Russ.) https://doi.org/10.31857/S2587556620050076

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