Geomorphological correlation of the Late Pleistocene glacial complexes of

Many fundamental problems exist in comparing the chronology and correlation of Late Pleistocene glaciations between Western and Eastern Beringia. However, geomorphological analysis, complemented by palynological studies and radiocarbon age estimates of glacial complexes found in the Ulakhan-Chistai,...

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Main Author: O. Yu. Glushkova
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2001
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.500.171
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.500.171 2023-05-15T15:46:58+02:00 Geomorphological correlation of the Late Pleistocene glacial complexes of O. Yu. Glushkova The Pennsylvania State University CiteSeerX Archives 2001 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.500.171 en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.500.171 Metadata may be used without restrictions as long as the oai identifier remains attached to it. https://notendur.hi.is/~oi/AG-326 2006 readings/Beringia and Alaska/F. More Berigian stuff/Glushkova_QSR2001.pdf text 2001 ftciteseerx 2016-01-08T09:04:59Z Many fundamental problems exist in comparing the chronology and correlation of Late Pleistocene glaciations between Western and Eastern Beringia. However, geomorphological analysis, complemented by palynological studies and radiocarbon age estimates of glacial complexes found in the Ulakhan-Chistai, Bolshoi Annachag, and Pekulney ranges, northeastern Russia, and the Kigluaik Mountains and Brooks Range, Alaska, allow for broad comparisons. The data clearly con"rm that in all regions the latest late Pleistocene glaciation (24.0}10.5 ka) was restricted in extent and characterized by well-de"ned valley glaciers and coalescing valley glacier complexes emanating from local mountain centers. Di!erences in glacier size were due to local orographic and climatological Text Brooks Range glacier glacier glaciers Alaska Beringia Unknown
institution Open Polar
collection Unknown
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language English
description Many fundamental problems exist in comparing the chronology and correlation of Late Pleistocene glaciations between Western and Eastern Beringia. However, geomorphological analysis, complemented by palynological studies and radiocarbon age estimates of glacial complexes found in the Ulakhan-Chistai, Bolshoi Annachag, and Pekulney ranges, northeastern Russia, and the Kigluaik Mountains and Brooks Range, Alaska, allow for broad comparisons. The data clearly con"rm that in all regions the latest late Pleistocene glaciation (24.0}10.5 ka) was restricted in extent and characterized by well-de"ned valley glaciers and coalescing valley glacier complexes emanating from local mountain centers. Di!erences in glacier size were due to local orographic and climatological
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author O. Yu. Glushkova
spellingShingle O. Yu. Glushkova
Geomorphological correlation of the Late Pleistocene glacial complexes of
author_facet O. Yu. Glushkova
author_sort O. Yu. Glushkova
title Geomorphological correlation of the Late Pleistocene glacial complexes of
title_short Geomorphological correlation of the Late Pleistocene glacial complexes of
title_full Geomorphological correlation of the Late Pleistocene glacial complexes of
title_fullStr Geomorphological correlation of the Late Pleistocene glacial complexes of
title_full_unstemmed Geomorphological correlation of the Late Pleistocene glacial complexes of
title_sort geomorphological correlation of the late pleistocene glacial complexes of
publishDate 2001
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.500.171
genre Brooks Range
glacier
glacier
glaciers
Alaska
Beringia
genre_facet Brooks Range
glacier
glacier
glaciers
Alaska
Beringia
op_source https://notendur.hi.is/~oi/AG-326 2006 readings/Beringia and Alaska/F. More Berigian stuff/Glushkova_QSR2001.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.500.171
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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