geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-3585Research ArticleНаучные сообщенияShort communicationsНекоторые аспекты развития рельефа в позднем Валдае в восточной части Баренцева моря и прилегающей сушиSome aspects of Late Valdai relief formation in the East part of Barents Sea and adjacent landАвенариусИ. Г.AvenariusI. G.ДунаевН. Н.DunaevN. N.Институт океанологии им. П.П. ШиршоваРоссияНПП "Аэрогеология"Россия199915012024035762Copyright © Авенариус И.Г., Дунаев Н.Н., 20242024Авенариус И.Г., Дунаев Н.Н.Avenarius I.G., Dunaev N.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/3585

Paleoclimatic reconstructions and relief analysis were fulfilled, using the large-scale topographic maps and space images for the land and bathymetric and seismic data - two types of mountain and valley glaciers of different thickness and activity were distinguished in the region for the Late Valdai Age. Paleoclimatic and geomorphologic data indicate the absence of continuous thick ice cover on the Pechora lowland during this time.

Paleoclimatic reconstructions and relief analysis were fulfilled, using the large-scale topographic maps and space images for the land and bathymetric and seismic data - two types of mountain and valley glaciers of different thickness and activity were distinguished in the region for the Late Valdai Age. Paleoclimatic and geomorphologic data indicate the absence of continuous thick ice cover on the Pechora lowland during this time.

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