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TO PROBLEM OF PLEISTOCENE HISTORY OF FORMING OF VALLEY RELIEF ON LEFT BANK OF THE MIDDLE DNIEPER. Paper 1. System-geomorphological sights of two glacial transgressive stages

According to the features of the geomorphological structure of the valley of the middle Dnieper, some episodes of its Neo-Pleistocene history have been reconstructed.Presence of morphosedimentic signs of two glaciations at this area is shown

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Bibliographic Details
Date:	2018
Main Author:	Karpenko, A.
Format:	Article
Language:	Ukrainian
Published:	Institute of Geological Sciences, NAS of Ukraine 2018
Subjects:	river terrace lateral erosion glaciation kame terrace
Online Access:	http://geojournal.igs-nas.org.ua/article/view/133459
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Journal Title:	Geological journal

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Geological journal

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