Do Periglacial Landscapes Exist? A Discussion of the Upland Landscapes of Northern Interior Yukon, Canada
Abstract Much of the northern interior Yukon was never‐glaciated during the Quaternary. It has experienced cold and arid conditions for several millions of years. It represents one of the closest approximations that exist today of a periglacial landscape and provides an opportunity to assess concept...
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Online Access: | http://dx.doi.org/10.1002/ppp.1866 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.1866 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.1866 |
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crwiley:10.1002/ppp.1866 2024-10-20T14:11:14+00:00 Do Periglacial Landscapes Exist? A Discussion of the Upland Landscapes of Northern Interior Yukon, Canada French, Hugh M. 2015 http://dx.doi.org/10.1002/ppp.1866 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.1866 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.1866 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 27, issue 2, page 219-228 ISSN 1045-6740 1099-1530 journal-article 2015 crwiley https://doi.org/10.1002/ppp.1866 2024-10-07T04:30:38Z Abstract Much of the northern interior Yukon was never‐glaciated during the Quaternary. It has experienced cold and arid conditions for several millions of years. It represents one of the closest approximations that exist today of a periglacial landscape and provides an opportunity to assess conceptual models of periglacial landscape evolution. The terrain of two upland areas, Eagle Plain and the Barn Mountains foothills, casts doubt upon the widely‐assumed rapidity of periglacial landscape modification and suggests that the complete footprint of periglaciation is rarely achieved in upland terrain. Copyright © 2015 John Wiley & Sons, Ltd. Article in Journal/Newspaper Permafrost and Periglacial Processes Yukon Wiley Online Library Yukon Canada Permafrost and Periglacial Processes 27 2 219 228 |
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language |
English |
description |
Abstract Much of the northern interior Yukon was never‐glaciated during the Quaternary. It has experienced cold and arid conditions for several millions of years. It represents one of the closest approximations that exist today of a periglacial landscape and provides an opportunity to assess conceptual models of periglacial landscape evolution. The terrain of two upland areas, Eagle Plain and the Barn Mountains foothills, casts doubt upon the widely‐assumed rapidity of periglacial landscape modification and suggests that the complete footprint of periglaciation is rarely achieved in upland terrain. Copyright © 2015 John Wiley & Sons, Ltd. |
format |
Article in Journal/Newspaper |
author |
French, Hugh M. |
spellingShingle |
French, Hugh M. Do Periglacial Landscapes Exist? A Discussion of the Upland Landscapes of Northern Interior Yukon, Canada |
author_facet |
French, Hugh M. |
author_sort |
French, Hugh M. |
title |
Do Periglacial Landscapes Exist? A Discussion of the Upland Landscapes of Northern Interior Yukon, Canada |
title_short |
Do Periglacial Landscapes Exist? A Discussion of the Upland Landscapes of Northern Interior Yukon, Canada |
title_full |
Do Periglacial Landscapes Exist? A Discussion of the Upland Landscapes of Northern Interior Yukon, Canada |
title_fullStr |
Do Periglacial Landscapes Exist? A Discussion of the Upland Landscapes of Northern Interior Yukon, Canada |
title_full_unstemmed |
Do Periglacial Landscapes Exist? A Discussion of the Upland Landscapes of Northern Interior Yukon, Canada |
title_sort |
do periglacial landscapes exist? a discussion of the upland landscapes of northern interior yukon, canada |
publisher |
Wiley |
publishDate |
2015 |
url |
http://dx.doi.org/10.1002/ppp.1866 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.1866 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.1866 |
geographic |
Yukon Canada |
geographic_facet |
Yukon Canada |
genre |
Permafrost and Periglacial Processes Yukon |
genre_facet |
Permafrost and Periglacial Processes Yukon |
op_source |
Permafrost and Periglacial Processes volume 27, issue 2, page 219-228 ISSN 1045-6740 1099-1530 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/ppp.1866 |
container_title |
Permafrost and Periglacial Processes |
container_volume |
27 |
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2 |
container_start_page |
219 |
op_container_end_page |
228 |
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1813451510536732672 |