Yukon River: Evidence for Extensive Migration during the Holocene Transgression
The shift of the Yukon River, during the Holocene sea-level transgression, from south of Nunivak Island during the Wisconsin maximum to its present location (a distance greater than 300 kilometers) is indicated by remanent channels, distinct subbottom structures, deltaic sediments, and anomalous rat...
Published in: | Science |
---|---|
Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Association for the Advancement of Science (AAAS)
1973
|
Subjects: | |
Online Access: | http://dx.doi.org/10.1126/science.179.4079.1230 https://www.science.org/doi/pdf/10.1126/science.179.4079.1230 |
id |
craaas:10.1126/science.179.4079.1230 |
---|---|
record_format |
openpolar |
spelling |
craaas:10.1126/science.179.4079.1230 2024-06-09T07:45:06+00:00 Yukon River: Evidence for Extensive Migration during the Holocene Transgression Knebel, Harley J. Creager, Joe S. 1973 http://dx.doi.org/10.1126/science.179.4079.1230 https://www.science.org/doi/pdf/10.1126/science.179.4079.1230 en eng American Association for the Advancement of Science (AAAS) Science volume 179, issue 4079, page 1230-1232 ISSN 0036-8075 1095-9203 journal-article 1973 craaas https://doi.org/10.1126/science.179.4079.1230 2024-05-16T12:55:30Z The shift of the Yukon River, during the Holocene sea-level transgression, from south of Nunivak Island during the Wisconsin maximum to its present location (a distance greater than 300 kilometers) is indicated by remanent channels, distinct subbottom structures, deltaic sediments, and anomalous rates of sediment accumulation on the continental shelf of the east-central Bering Sea. These features were produced as the ancestral river migrated northward across the easternmost part of this area before 11,000 years ago. Article in Journal/Newspaper Bering Sea Nunivak Nunivak Island Yukon river Yukon AAAS Resource Center (American Association for the Advancement of Science) Bering Sea Yukon Science 179 4079 1230 1232 |
institution |
Open Polar |
collection |
AAAS Resource Center (American Association for the Advancement of Science) |
op_collection_id |
craaas |
language |
English |
description |
The shift of the Yukon River, during the Holocene sea-level transgression, from south of Nunivak Island during the Wisconsin maximum to its present location (a distance greater than 300 kilometers) is indicated by remanent channels, distinct subbottom structures, deltaic sediments, and anomalous rates of sediment accumulation on the continental shelf of the east-central Bering Sea. These features were produced as the ancestral river migrated northward across the easternmost part of this area before 11,000 years ago. |
format |
Article in Journal/Newspaper |
author |
Knebel, Harley J. Creager, Joe S. |
spellingShingle |
Knebel, Harley J. Creager, Joe S. Yukon River: Evidence for Extensive Migration during the Holocene Transgression |
author_facet |
Knebel, Harley J. Creager, Joe S. |
author_sort |
Knebel, Harley J. |
title |
Yukon River: Evidence for Extensive Migration during the Holocene Transgression |
title_short |
Yukon River: Evidence for Extensive Migration during the Holocene Transgression |
title_full |
Yukon River: Evidence for Extensive Migration during the Holocene Transgression |
title_fullStr |
Yukon River: Evidence for Extensive Migration during the Holocene Transgression |
title_full_unstemmed |
Yukon River: Evidence for Extensive Migration during the Holocene Transgression |
title_sort |
yukon river: evidence for extensive migration during the holocene transgression |
publisher |
American Association for the Advancement of Science (AAAS) |
publishDate |
1973 |
url |
http://dx.doi.org/10.1126/science.179.4079.1230 https://www.science.org/doi/pdf/10.1126/science.179.4079.1230 |
geographic |
Bering Sea Yukon |
geographic_facet |
Bering Sea Yukon |
genre |
Bering Sea Nunivak Nunivak Island Yukon river Yukon |
genre_facet |
Bering Sea Nunivak Nunivak Island Yukon river Yukon |
op_source |
Science volume 179, issue 4079, page 1230-1232 ISSN 0036-8075 1095-9203 |
op_doi |
https://doi.org/10.1126/science.179.4079.1230 |
container_title |
Science |
container_volume |
179 |
container_issue |
4079 |
container_start_page |
1230 |
op_container_end_page |
1232 |
_version_ |
1801374040335581184 |