Evolution of the Upper Reaches of Fluvial Systems within the Area of the East European Plain Glaciated during MIS 6
The headwaters of fluvial systems on the East European Plain between the boundaries of the Marine Isotope Stage 2 (MIS Right Pedal Pad 2) and MIS 6 glaciations evolved during the last 150,000 years.At least three main events of high surface runoff caused intensive erosion: at the end of MIS 6, at the end of MIS 2 and in the Middle Holocene.Erosion