geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-3524Research ArticleНаучные сообщенияShort communicationsГеоморфологическая индикация мерзлотных и немерзлотных ландшафтов средней тайги Центральной СибириGeomorphological indication of cryogenic and not cryogenic middle-taiga landscapes in Central SiberiaГоршковС. П.GorshkovS. P.КаррашХ.KarrashH.ПарамоновА. В.ParamonovA. V.Московский государственный университет имени М.В.Ломоносова, географический факультетРоссия199826122023045561Copyright © Горшков С.П., Карраш Х., Парамонов А.В., 20232023Горшков С.П., Карраш Х., Парамонов А.В.Gorshkov S.P., Karrash H., Paramonov A.V.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/3524

The region of permafrost in the downstream of Podkamennaya Tunguska is under consideration. Indication of cryogenic and not cryogenic landscapes was fulfilled on the basis of data on geomorphological structure and recent geomorphological processes. The distribution of cryogenic landscapes, frozen rocks and thaw rocks, and therefore the landscape structure of the ecotone zone depend mostly on macrogeomorphologic pattern of the territory - planation belt and cutting belt of relief. Each of them has specific combination of natural factors, including geomorphological ones, which determine the exact distribution of cryogenic and not cryogenic landscapes.

The region of permafrost in the downstream of Podkamennaya Tunguska is under consideration. Indication of cryogenic and not cryogenic landscapes was fulfilled on the basis of data on geomorphological structure and recent geomorphological processes. The distribution of cryogenic landscapes, frozen rocks and thaw rocks, and therefore the landscape structure of the ecotone zone depend mostly on macrogeomorphologic pattern of the territory - planation belt and cutting belt of relief. Each of them has specific combination of natural factors, including geomorphological ones, which determine the exact distribution of cryogenic and not cryogenic landscapes.

References

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