geosciences Article The Functioning of Erosion-channel Systems of the River Basins of the South of Eastern Siberia Olga I. Bazhenova 1,*, Aleksandr V. Bardash 1, Stanislav A. Makarov 1, Marina Yu. Opekunova 1, Sergei A. Tukhta 1 and Elizaveta M. Tyumentseva 2 1 V.B. Sochava Institute of Geography SB RAS, Irkutsk 664033, Russia;
[email protected] (A.V.B.);
[email protected] (S.A.M.);
[email protected] (M.Y.O.);
[email protected] (S.A.T.) 2 Geographical Department, Pedagogical Institute of Irkutsk State University, Irkutsk 664033, Russia;
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[email protected]; Tel.: +7-3952426920 Received: 23 March 2020; Accepted: 6 May 2020; Published: 11 May 2020 Abstract: We revealed the regional features of the functioning of the erosion-channel systems of the Angara, Upper Lena, Selenga, and Upper Amur basins in the south of Eastern Siberia and examined the action of sloping non-channel, temporary, and permanent channel water flows, and presented the patterns of the spatial distribution of soil and gully erosion belts. The development conditions and factors of fluvial processes are considered and the role of cryogenic processes in the increasing activity of water flows is emphasized. The interdecadal dynamic cycles of the erosion-accumulative processes are revealed. A quantitative assessment of soil loss from erosion on agricultural land in the forest-steppe basins was carried out. We made an assessment of the plane deformation of the upper course of the Lena river (Siberian platform) and Irkut (Baikal rift zone and the Irkutsk-Cheremkhovo plain) using cartographic sources of different times, aerial photographs, and satellite imagery.