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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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 |
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ftciteseerx |
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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. |
_version_ |
1766381774687961088 |