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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„Ștefan cel Mare” University Press
2016
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ftdoajarticles:oai:doaj.org/article:7a8e6640a407420fb0535744bf88ed1f 2023-05-15T16:36:52+02:00 Reflection of climatic changes during Interpleniglacial in geoecosystems of Southern Poland Danuta J. MICHCZYŃSKA 2016-06-01T00:00:00Z https://doaj.org/article/7a8e6640a407420fb0535744bf88ed1f EN eng „Ștefan cel Mare” University Press http://georeview.ro/ojs/index.php/revista/article/view/337 https://doaj.org/toc/1583-1469 1583-1469 https://doaj.org/article/7a8e6640a407420fb0535744bf88ed1f GEOREVIEW: Scientific Annals of Stefan cel Mare University of Suceava. Geography Series, Vol 26, Iss 2 (2016) Science Q Science (General) Q1-390 article 2016 ftdoajarticles 2022-12-31T05:28:50Z 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 Article in Journal/Newspaper Ice Ice Sheet permafrost Directory of Open Access Journals: DOAJ Articles |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Science Q Science (General) Q1-390 |
spellingShingle |
Science Q Science (General) Q1-390 Danuta J. MICHCZYŃSKA Reflection of climatic changes during Interpleniglacial in geoecosystems of Southern Poland |
topic_facet |
Science Q Science (General) Q1-390 |
description |
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 |
format |
Article in Journal/Newspaper |
author |
Danuta J. MICHCZYŃSKA |
author_facet |
Danuta J. MICHCZYŃSKA |
author_sort |
Danuta J. MICHCZYŃSKA |
title |
Reflection of climatic changes during Interpleniglacial in geoecosystems of Southern Poland |
title_short |
Reflection of climatic changes during Interpleniglacial in geoecosystems of Southern Poland |
title_full |
Reflection of climatic changes during Interpleniglacial in geoecosystems of Southern Poland |
title_fullStr |
Reflection of climatic changes during Interpleniglacial in geoecosystems of Southern Poland |
title_full_unstemmed |
Reflection of climatic changes during Interpleniglacial in geoecosystems of Southern Poland |
title_sort |
reflection of climatic changes during interpleniglacial in geoecosystems of southern poland |
publisher |
„Ștefan cel Mare” University Press |
publishDate |
2016 |
url |
https://doaj.org/article/7a8e6640a407420fb0535744bf88ed1f |
genre |
Ice Ice Sheet permafrost |
genre_facet |
Ice Ice Sheet permafrost |
op_source |
GEOREVIEW: Scientific Annals of Stefan cel Mare University of Suceava. Geography Series, Vol 26, Iss 2 (2016) |
op_relation |
http://georeview.ro/ojs/index.php/revista/article/view/337 https://doaj.org/toc/1583-1469 1583-1469 https://doaj.org/article/7a8e6640a407420fb0535744bf88ed1f |
_version_ |
1766027186212438016 |