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...

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Bibliographic Details
Main Authors: Stoker, Benjamin J., Margold, Martin, Froese, Duane
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
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