Sedimentological study of glacimarginal forms near Zamoście (Volhynian Polesie, NW Ukraine)

Near Zamostya in the Volhynian Polesie (NW Ukraine) a first sedimentological attempt was made to explain the origin of glacimarginal forms forming sub-parallel trains. They belong to themost typical elements of the Polesie glacial relief from the Dnieper Glaciation. Lithofacial analysis was used dur...

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Bibliographic Details
Main Author: Renda, Andrij
Format: Article in Journal/Newspaper
Language:Polish
Published: www.wydawnictwo.umcs.lublin.pl 2015
Subjects:
glacimarginal forms
lithofacial analysis
end moraines
Dnieper Glaciation
Volhynian Polesie
NW Ukraine
formy glacimarginalne
analiza litofacjalna
moreny czołowe
zlodowacenie dniepru
Polesie Wołyńskie
Ukraina NW
Ice Sheet
Online Access:https://journals.umcs.pl/b/article/view/1251
https://doi.org/10.17951/b.2013.68.2.7
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Summary:Near Zamostya in the Volhynian Polesie (NW Ukraine) a first sedimentological attempt was made to explain the origin of glacimarginal forms forming sub-parallel trains. They belong to themost typical elements of the Polesie glacial relief from the Dnieper Glaciation. Lithofacial analysis was used during the research. Based on geomorphological situation of the glacimarginal forms andlithofacial features of their deposits, the forms were classified as end moraines documenting one of the stagnation phases of ice-sheet recession during the Dnieper Glaciation. Artykuł nie zawiera abstraktu w języku polskim

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