Reflection of climatic changes during Interpleniglacial in geoecosystems of Southern Poland

The central part of Europe during the last cold stage was occupied by permafrost and twice invaded by the Scandinavian ice sheet, but about 70% of time was taken by transitional phases of continuous fluctuations of permafrost, which are reflected especially in type and thickness of slope, fluvial an...

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Bibliographic Details
Main Author: Danuta J. MICHCZYŃSKA
Format: Article in Journal/Newspaper
Language:English
Published: „Ștefan cel Mare” University Press 2016
Subjects:
Q
Ice
Online Access:https://doaj.org/article/7a8e6640a407420fb0535744bf88ed1f
Description
Summary:The central part of Europe during the last cold stage was occupied by permafrost and twice invaded by the Scandinavian ice sheet, but about 70% of time was taken by transitional phases of continuous fluctuations of permafrost, which are reflected especially in type and thickness of slope, fluvial and aeolian deposits