geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-2279Research ArticleНаучные сообщенияShort communicationsКраевые ледниковые образования бассейна ДесныMarginal glacial features at the Desna drainage basinЧеботареваН. С.ChebotarevaN. S.ГаврюшинаЕ. А.GavryushovaE. A.

Московская комплексная геолого-гидрогеологическая экспедиция ГУЦР

ЛехтЭ. Е.LehtE. E.Институт географии АН СССРРоссия19810809202202Геоморфология9198Copyright © Чеботарева Н.С., Гаврюшина Е.А., Лехт Э.Е., 20222022Чеботарева Н.С., Гаврюшина Е.А., Лехт Э.Е.Chebotareva N.S., Gavryushova E.A., Leht E.E.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/2279

The marginal glacial zones are established to be more widespread in the region than they were thought before. Local moraines are proved to exist almost all over the southern part of the region. The data allow changing the boundary of the Dnieper glaciation.

The marginal glacial zones are established to be more widespread in the region than they were thought before. Local moraines are proved to exist almost all over the southern part of the region. The data allow changing the boundary of the Dnieper glaciation.

References

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