The glacial geomorphology of the Mackenzie Mountains region, Canada ...
During the Last Glacial Maximum, the Mackenzie Mountains region was glaciated by three distinct ice sources; the Laurentide Ice Sheet, the Cordilleran Ice Sheet, and independent montane glaciers. Rapid ice sheet thinning of the Laurentide-Cordilleran ice saddle in the south of this region contribute...
Main Authors: | , , |
---|---|
Format: | Dataset |
Language: | unknown |
Published: |
Taylor & Francis
2023
|
Subjects: | |
Online Access: | https://dx.doi.org/10.6084/m9.figshare.22791100 https://tandf.figshare.com/articles/dataset/The_glacial_geomorphology_of_the_Mackenzie_Mountains_region_Canada/22791100 |
id |
ftdatacite:10.6084/m9.figshare.22791100 |
---|---|
record_format |
openpolar |
spelling |
ftdatacite:10.6084/m9.figshare.22791100 2024-02-04T10:00:37+01:00 The glacial geomorphology of the Mackenzie Mountains region, Canada ... Stoker, Benjamin J. Margold, Martin Froese, Duane 2023 https://dx.doi.org/10.6084/m9.figshare.22791100 https://tandf.figshare.com/articles/dataset/The_glacial_geomorphology_of_the_Mackenzie_Mountains_region_Canada/22791100 unknown Taylor & Francis https://dx.doi.org/10.1080/17445647.2023.2203333 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Medicine Pharmacology Environmental Sciences not elsewhere classified Ecology FOS Biological sciences Astronomical and Space Sciences not elsewhere classified Biological Sciences not elsewhere classified Information Systems not elsewhere classified Cancer Computational Biology Dataset dataset 2023 ftdatacite https://doi.org/10.6084/m9.figshare.2279110010.1080/17445647.2023.2203333 2024-01-05T01:19:58Z During the Last Glacial Maximum, the Mackenzie Mountains region was glaciated by three distinct ice sources; the Laurentide Ice Sheet, the Cordilleran Ice Sheet, and independent montane glaciers. Rapid ice sheet thinning of the Laurentide-Cordilleran ice saddle in the south of this region contributed to rapid sea level rise events and influenced the style of deglaciation to the north. The current understanding of the glacial history of the broader region has been established through mapping from aerial imagery and early surveys between the early 1970s to the 2010s. The central portions of the Mackenzie Mountains have not yet been mapped. We present a new glacial geomorphological map for the Mackenzie Mountains region covering over 220,000 km 2 . This updated geomorphological map will form the basis of future work to reconstruct the former maximum ice extents, flow dynamics, and retreat pattern. ... Dataset glacier* Ice Sheet Mackenzie mountains DataCite Metadata Store (German National Library of Science and Technology) Canada |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
unknown |
topic |
Medicine Pharmacology Environmental Sciences not elsewhere classified Ecology FOS Biological sciences Astronomical and Space Sciences not elsewhere classified Biological Sciences not elsewhere classified Information Systems not elsewhere classified Cancer Computational Biology |
spellingShingle |
Medicine Pharmacology Environmental Sciences not elsewhere classified Ecology FOS Biological sciences Astronomical and Space Sciences not elsewhere classified Biological Sciences not elsewhere classified Information Systems not elsewhere classified Cancer Computational Biology Stoker, Benjamin J. Margold, Martin Froese, Duane The glacial geomorphology of the Mackenzie Mountains region, Canada ... |
topic_facet |
Medicine Pharmacology Environmental Sciences not elsewhere classified Ecology FOS Biological sciences Astronomical and Space Sciences not elsewhere classified Biological Sciences not elsewhere classified Information Systems not elsewhere classified Cancer Computational Biology |
description |
During the Last Glacial Maximum, the Mackenzie Mountains region was glaciated by three distinct ice sources; the Laurentide Ice Sheet, the Cordilleran Ice Sheet, and independent montane glaciers. Rapid ice sheet thinning of the Laurentide-Cordilleran ice saddle in the south of this region contributed to rapid sea level rise events and influenced the style of deglaciation to the north. The current understanding of the glacial history of the broader region has been established through mapping from aerial imagery and early surveys between the early 1970s to the 2010s. The central portions of the Mackenzie Mountains have not yet been mapped. We present a new glacial geomorphological map for the Mackenzie Mountains region covering over 220,000 km 2 . This updated geomorphological map will form the basis of future work to reconstruct the former maximum ice extents, flow dynamics, and retreat pattern. ... |
format |
Dataset |
author |
Stoker, Benjamin J. Margold, Martin Froese, Duane |
author_facet |
Stoker, Benjamin J. Margold, Martin Froese, Duane |
author_sort |
Stoker, Benjamin J. |
title |
The glacial geomorphology of the Mackenzie Mountains region, Canada ... |
title_short |
The glacial geomorphology of the Mackenzie Mountains region, Canada ... |
title_full |
The glacial geomorphology of the Mackenzie Mountains region, Canada ... |
title_fullStr |
The glacial geomorphology of the Mackenzie Mountains region, Canada ... |
title_full_unstemmed |
The glacial geomorphology of the Mackenzie Mountains region, Canada ... |
title_sort |
glacial geomorphology of the mackenzie mountains region, canada ... |
publisher |
Taylor & Francis |
publishDate |
2023 |
url |
https://dx.doi.org/10.6084/m9.figshare.22791100 https://tandf.figshare.com/articles/dataset/The_glacial_geomorphology_of_the_Mackenzie_Mountains_region_Canada/22791100 |
geographic |
Canada |
geographic_facet |
Canada |
genre |
glacier* Ice Sheet Mackenzie mountains |
genre_facet |
glacier* Ice Sheet Mackenzie mountains |
op_relation |
https://dx.doi.org/10.1080/17445647.2023.2203333 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.6084/m9.figshare.2279110010.1080/17445647.2023.2203333 |
_version_ |
1789966007355310080 |