geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-2778Research ArticleНаучные сообщенияShort communicationsГеолого-геоморфологические признаки древних оледенений в бассейне среднего течения р. КолымыGeological and geomorphological indications of former glaciations within the middle part of the Kolyma drainage basinЧанышеваМ. Н.ChanyshevaM. N.Московский государственный университет имени М.В.Ломоносова, географический факультетРоссия19882011202203Геоморфология7782Copyright © Чанышева М.Н., 20222022Чанышева М.Н.Chanysheva M.N.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/2778

Extensive glaciations developed within the middle Kolyma drainage Basin during the Early and Middle Pleistocene. The glaciers type and extension are extablished on the basis of glacial and periglacial deposits distribution, position of glacial troughs and eroded glacial cirques and privation-solifluction hollows. The former glaciers developed under conditions of low' mountain and hilly topography.

Extensive glaciations developed within the middle Kolyma drainage Basin during the Early and Middle Pleistocene. The glaciers type and extension are extablished on the basis of glacial and periglacial deposits distribution, position of glacial troughs and eroded glacial cirques and privation-solifluction hollows. The former glaciers developed under conditions of low' mountain and hilly topography.

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