The mechanism of formation and degradation of the Chuya-Kuray ice-dammed lake

Авторы

  • Pupyshev, Yu.S. 1
  • Pozdnyakov, A.V. 1
    • 1 Institute of Monitoring of Climatic and Ecological Systems, Siberian Branch of the Russian Academy of Sciences, Academichesky ave., 10/3, Tomsk, 634055, Russia

DOI:

https://doi.org/10.31951/2658-3518-2022-A-4-1532

Ключевые слова:

ice-dammed lake, giant current ripples, Altai Mountains, paleoshoreline

Аннотация

The results of the study of the stratigraphic structure, granulometric composition of the sediments of the ridge relief, the heights of shorelines and the water balance of the Chuya-Kuray ice-dammed paleolake (Altai Mountains) are presented. It is established that the ridge relief is an alluvial fan of fluvioglacial temporary watercourses. The magnitude of floods during the drainage of the paleolake reached 800-2160 m3/s.

Загрузки

Опубликован

02.09.2022

Выпуск

2022: №4 (SI:Paleo2022)

Раздел

Статьи

Лицензия

Creative Commons License
Эта работа распространяется под международной лицензией Creative Commons Attribution-NonCommercial 4.0.