geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-3497Research ArticleНаучные сообщенияShort communicationsО гляциальном термокарсте на севере Приенисейской СибириOn the glacial thermokarst at the North of Prienisey SiberiaКаплянскаяФ. А.KaplyanskayaF. A.ТарноградскийВ. Д.TarnogradskyV. D.ВСЕГЕИ им. А.П. КарпинскогоРоссия199821122023035259Copyright © Каплянская Ф.А., Тарноградский В.Д., 20232023Каплянская Ф.А., Тарноградский В.Д.Kaplyanskaya F.A., Tarnogradsky V.D.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/3497

In this region glacial thermokarstic relief is widespread and its formation is running on as may be seen from remote sensing materials and from analysis of late glaciation's relics in the cryolithozone. The structure of glacial forms stamps on lake distribution and shape. Thermokarst is generated by reducing of ablation protective cover, by growth of seasonal thawing layer, by thermal erosion, by influence of other water bodies which appear due to melting of other types of ice. It was especially intensified in the Early Holocene and during climatic optimum because of high level of insulation.

In this region glacial thermokarstic relief is widespread and its formation is running on as may be seen from remote sensing materials and from analysis of late glaciation's relics in the cryolithozone. The structure of glacial forms stamps on lake distribution and shape. Thermokarst is generated by reducing of ablation protective cover, by growth of seasonal thawing layer, by thermal erosion, by influence of other water bodies which appear due to melting of other types of ice. It was especially intensified in the Early Holocene and during climatic optimum because of high level of insulation.

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