New Middle Pleistocene records from the North-East foothills of Carpathian Mountains

<p>Two kinds of paleogeographic records from the Middle Pleistocene were recently first discovered in the Bukovinian foothills of the Carpathian Mountains, not far downstream from the confluence of the Prut and Cheremosh Rivers.</p>The area of investigation is associated with the lower B...

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Main Author: Bogdan RIDUSH et al.
Format: Article
Language:English
Published: „Ștefan cel Mare” University Press 2016-06-01
Series:GEOREVIEW: Scientific Annals of Stefan cel Mare University of Suceava. Geography Series
Online Access:http://georeview.ro/ojs/index.php/revista/article/view/347
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spelling doaj-97c069855d444454a4dc9ffd5f7948d42021-06-02T14:27:41Zeng„Ștefan cel Mare” University PressGEOREVIEW: Scientific Annals of Stefan cel Mare University of Suceava. Geography Series1583-14692016-06-012627577387New Middle Pleistocene records from the North-East foothills of Carpathian MountainsBogdan RIDUSH et al.<p>Two kinds of paleogeographic records from the Middle Pleistocene were recently first discovered in the Bukovinian foothills of the Carpathian Mountains, not far downstream from the confluence of the Prut and Cheremosh Rivers.</p>The area of investigation is associated with the lower Brusnytsia River, the right tributary of the Prut River (fig. 1). Due to the active tectonic uplift, wide spread of dispersal Neogenic and Quaternary sediments, and comparatively wet climate, the whole area of the Prut and Siret rivers’ interfluve is strongly damaged by landslides. Therefore it is quit problematic to find undisturbed Quaternary river terrace sequences in the area. Generally, the territory is characterized by the lack of Quaternary records at all. Only few Late Paleolithic sites without geological sequence were known few kilometers downstream the Prut R. Moreover it was important to look for the evidence of the Middle Pleistocene therehttp://georeview.ro/ojs/index.php/revista/article/view/347
collection DOAJ
language English
format Article
sources DOAJ
author Bogdan RIDUSH et al.
spellingShingle Bogdan RIDUSH et al.
New Middle Pleistocene records from the North-East foothills of Carpathian Mountains
GEOREVIEW: Scientific Annals of Stefan cel Mare University of Suceava. Geography Series
author_facet Bogdan RIDUSH et al.
author_sort Bogdan RIDUSH et al.
title New Middle Pleistocene records from the North-East foothills of Carpathian Mountains
title_short New Middle Pleistocene records from the North-East foothills of Carpathian Mountains
title_full New Middle Pleistocene records from the North-East foothills of Carpathian Mountains
title_fullStr New Middle Pleistocene records from the North-East foothills of Carpathian Mountains
title_full_unstemmed New Middle Pleistocene records from the North-East foothills of Carpathian Mountains
title_sort new middle pleistocene records from the north-east foothills of carpathian mountains
publisher „Ștefan cel Mare” University Press
series GEOREVIEW: Scientific Annals of Stefan cel Mare University of Suceava. Geography Series
issn 1583-1469
publishDate 2016-06-01
description <p>Two kinds of paleogeographic records from the Middle Pleistocene were recently first discovered in the Bukovinian foothills of the Carpathian Mountains, not far downstream from the confluence of the Prut and Cheremosh Rivers.</p>The area of investigation is associated with the lower Brusnytsia River, the right tributary of the Prut River (fig. 1). Due to the active tectonic uplift, wide spread of dispersal Neogenic and Quaternary sediments, and comparatively wet climate, the whole area of the Prut and Siret rivers’ interfluve is strongly damaged by landslides. Therefore it is quit problematic to find undisturbed Quaternary river terrace sequences in the area. Generally, the territory is characterized by the lack of Quaternary records at all. Only few Late Paleolithic sites without geological sequence were known few kilometers downstream the Prut R. Moreover it was important to look for the evidence of the Middle Pleistocene there
url http://georeview.ro/ojs/index.php/revista/article/view/347
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