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...

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Published in:Canadian Journal of Earth Sciences
Main Author: Klassen, R. W.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1978
Subjects:
Online Access:http://dx.doi.org/10.1139/e78-199
http://www.nrcresearchpress.com/doi/pdf/10.1139/e78-199
id crcansciencepubl:10.1139/e78-199
record_format openpolar
spelling 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
institution 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
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