A unique stratigraphic record of late Tertiary–Quaternary events in southeastern Yukon
A succession of fluvial sediments with minor coal, basaltic lava, five tills, and fossiliferous intertill sediments exposed along the Liard River where it crosses the Liard Plain provides a remarkably continuous record of geologic–climatic events in this region. The coal bearing sediments and lava w...
Published in: | Canadian Journal of Earth Sciences |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Canadian Science Publishing
1978
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Online Access: | http://dx.doi.org/10.1139/e78-199 http://www.nrcresearchpress.com/doi/pdf/10.1139/e78-199 |
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crcansciencepubl:10.1139/e78-199 2024-09-15T18:17:50+00:00 A unique stratigraphic record of late Tertiary–Quaternary events in southeastern Yukon Klassen, R. W. 1978 http://dx.doi.org/10.1139/e78-199 http://www.nrcresearchpress.com/doi/pdf/10.1139/e78-199 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 15, issue 11, page 1884-1886 ISSN 0008-4077 1480-3313 journal-article 1978 crcansciencepubl https://doi.org/10.1139/e78-199 2024-07-25T04:10:06Z A succession of fluvial sediments with minor coal, basaltic lava, five tills, and fossiliferous intertill sediments exposed along the Liard River where it crosses the Liard Plain provides a remarkably continuous record of geologic–climatic events in this region. The coal bearing sediments and lava were previously described and interpreted as Tertiary–Quaternary in age. The Quaternary sediments record four major intervals of glaciation and three nonglacial intervals not previously recognized in this region. Article in Journal/Newspaper Liard River Yukon Canadian Science Publishing Canadian Journal of Earth Sciences 15 11 1884 1886 |
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Open Polar |
collection |
Canadian Science Publishing |
op_collection_id |
crcansciencepubl |
language |
English |
description |
A succession of fluvial sediments with minor coal, basaltic lava, five tills, and fossiliferous intertill sediments exposed along the Liard River where it crosses the Liard Plain provides a remarkably continuous record of geologic–climatic events in this region. The coal bearing sediments and lava were previously described and interpreted as Tertiary–Quaternary in age. The Quaternary sediments record four major intervals of glaciation and three nonglacial intervals not previously recognized in this region. |
format |
Article in Journal/Newspaper |
author |
Klassen, R. W. |
spellingShingle |
Klassen, R. W. A unique stratigraphic record of late Tertiary–Quaternary events in southeastern Yukon |
author_facet |
Klassen, R. W. |
author_sort |
Klassen, R. W. |
title |
A unique stratigraphic record of late Tertiary–Quaternary events in southeastern Yukon |
title_short |
A unique stratigraphic record of late Tertiary–Quaternary events in southeastern Yukon |
title_full |
A unique stratigraphic record of late Tertiary–Quaternary events in southeastern Yukon |
title_fullStr |
A unique stratigraphic record of late Tertiary–Quaternary events in southeastern Yukon |
title_full_unstemmed |
A unique stratigraphic record of late Tertiary–Quaternary events in southeastern Yukon |
title_sort |
unique stratigraphic record of late tertiary–quaternary events in southeastern yukon |
publisher |
Canadian Science Publishing |
publishDate |
1978 |
url |
http://dx.doi.org/10.1139/e78-199 http://www.nrcresearchpress.com/doi/pdf/10.1139/e78-199 |
genre |
Liard River Yukon |
genre_facet |
Liard River Yukon |
op_source |
Canadian Journal of Earth Sciences volume 15, issue 11, page 1884-1886 ISSN 0008-4077 1480-3313 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/e78-199 |
container_title |
Canadian Journal of Earth Sciences |
container_volume |
15 |
container_issue |
11 |
container_start_page |
1884 |
op_container_end_page |
1886 |
_version_ |
1810455929242517504 |