О гляциальном термокарсте на севере Приенисейской Сибири

Аннотация

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.