geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-3526Research ArticleНаучные сообщенияShort communicationsРеконструкция северо-восточной краевой области Скандинавского ледникового покрова в поздневалдайское времяReconstruction of north-eastern margin of the Scandinavian ice sheet in Late Valdaian timeЕвзеровВ. Я.YevserovV. Ya.СамойловичЮ. Г.SamoilovitchYu. G.Геологический институт Кольского научного центра РАНРоссия199826122023046570Copyright © Евзеров В.Я., Самойлович Ю.Г., 20232023Евзеров В.Я., Самойлович Ю.Г.Yevserov V.Y., Samoilovitch Y.G.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/3526

The paper summarizes fieldwork data on glacio-marginal formations in the Kola Peninsula and adjoining areas of the Barents and the White Seas (an empiricalmodel). The spatial reconstruction-of the Kolian Glacial Lobe off the Scandinavian ice sheet during the Last Glacial Maximum is performed by means of math modelling. On the base of these models the authors suggest that Scandinavian ice sheet under its own physical parameters did not spread farther than the Kanin Peninsular to the east and the Murman near-by offshore (Kola shelf of the Barents Sea) to the north.

The paper summarizes fieldwork data on glacio-marginal formations in the Kola Peninsula and adjoining areas of the Barents and the White Seas (an empiricalmodel). The spatial reconstruction-of the Kolian Glacial Lobe off the Scandinavian ice sheet during the Last Glacial Maximum is performed by means of math modelling. On the base of these models the authors suggest that Scandinavian ice sheet under its own physical parameters did not spread farther than the Kanin Peninsular to the east and the Murman near-by offshore (Kola shelf of the Barents Sea) to the north.

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