The geomorphic imprint of glacier surges into open-marine waters: Examples from eastern Svalbard ...

Seafloor morphology beyond nine tidewater glaciers terminating in open-marine settings in eastern Svalbard has been investigated using multibeam swath-bathymetry. Historical information on tidewater glacier fluctuations over the past century or so shows that the seafloor offshore has been exposed on...

Full description

Bibliographic Details
Main Authors: Ottesen, D, Dowdeswell, JA, Bellec, VK, Bjarnadóttir, LR
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2017
Subjects:
Online Access:https://dx.doi.org/10.17863/cam.13691
https://www.repository.cam.ac.uk/handle/1810/267761
id ftdatacite:10.17863/cam.13691
record_format openpolar
spelling ftdatacite:10.17863/cam.13691 2024-02-04T10:00:37+01:00 The geomorphic imprint of glacier surges into open-marine waters: Examples from eastern Svalbard ... Ottesen, D Dowdeswell, JA Bellec, VK Bjarnadóttir, LR 2017 https://dx.doi.org/10.17863/cam.13691 https://www.repository.cam.ac.uk/handle/1810/267761 en eng Elsevier open.access Creative Commons Attribution Non Commercial No Derivatives 4.0 International Creative Commons Attribution Non Commercial No Derivatives 4.0 International Attribution-NonCommercial-NoDerivatives 4.0 International Attribution-NonCommercial-NoDerivatives 4.0 International https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode cc-by-nc-nd-4.0 https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode cc-by-nc-nd-4.0 http://purl.org/coar/access_right/c_abf2 37 Earth Sciences 3709 Physical Geography and Environmental Geoscience 3705 Geology 13 Climate Action 14 Life Below Water Article ScholarlyArticle JournalArticle article-journal 2017 ftdatacite https://doi.org/10.17863/cam.13691 2024-01-05T09:16:25Z Seafloor morphology beyond nine tidewater glaciers terminating in open-marine settings in eastern Svalbard has been investigated using multibeam swath-bathymetry. Historical information on tidewater glacier fluctuations over the past century or so shows that the seafloor offshore has been exposed only recently. Most glaciers have been observed to surge or have looped surface moraines indicating past surges. During these ice advances and subsequent retreat, a well-preserved submarine landform assemblage has been produced. (a) Subglacial landforms include: overridden moraine ridges, mega-scale glacial lineations (MSGLs), other streamlined lineations, elongate drumlins and medial moraines, small ridges forming a complex boxwork or rhombohedral pattern, and meltwater-related eskers and channels. (b) Ice-marginal landforms include: large terminal moraines with debris flow lobes on their outer flanks and indentations on their inner sides, small transverse retreat moraines, and crater-like kettle holes. (c) ... Article in Journal/Newspaper glacier Svalbard Tidewater DataCite Metadata Store (German National Library of Science and Technology) Svalbard
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic 37 Earth Sciences
3709 Physical Geography and Environmental Geoscience
3705 Geology
13 Climate Action
14 Life Below Water
spellingShingle 37 Earth Sciences
3709 Physical Geography and Environmental Geoscience
3705 Geology
13 Climate Action
14 Life Below Water
Ottesen, D
Dowdeswell, JA
Bellec, VK
Bjarnadóttir, LR
The geomorphic imprint of glacier surges into open-marine waters: Examples from eastern Svalbard ...
topic_facet 37 Earth Sciences
3709 Physical Geography and Environmental Geoscience
3705 Geology
13 Climate Action
14 Life Below Water
description Seafloor morphology beyond nine tidewater glaciers terminating in open-marine settings in eastern Svalbard has been investigated using multibeam swath-bathymetry. Historical information on tidewater glacier fluctuations over the past century or so shows that the seafloor offshore has been exposed only recently. Most glaciers have been observed to surge or have looped surface moraines indicating past surges. During these ice advances and subsequent retreat, a well-preserved submarine landform assemblage has been produced. (a) Subglacial landforms include: overridden moraine ridges, mega-scale glacial lineations (MSGLs), other streamlined lineations, elongate drumlins and medial moraines, small ridges forming a complex boxwork or rhombohedral pattern, and meltwater-related eskers and channels. (b) Ice-marginal landforms include: large terminal moraines with debris flow lobes on their outer flanks and indentations on their inner sides, small transverse retreat moraines, and crater-like kettle holes. (c) ...
format Article in Journal/Newspaper
author Ottesen, D
Dowdeswell, JA
Bellec, VK
Bjarnadóttir, LR
author_facet Ottesen, D
Dowdeswell, JA
Bellec, VK
Bjarnadóttir, LR
author_sort Ottesen, D
title The geomorphic imprint of glacier surges into open-marine waters: Examples from eastern Svalbard ...
title_short The geomorphic imprint of glacier surges into open-marine waters: Examples from eastern Svalbard ...
title_full The geomorphic imprint of glacier surges into open-marine waters: Examples from eastern Svalbard ...
title_fullStr The geomorphic imprint of glacier surges into open-marine waters: Examples from eastern Svalbard ...
title_full_unstemmed The geomorphic imprint of glacier surges into open-marine waters: Examples from eastern Svalbard ...
title_sort geomorphic imprint of glacier surges into open-marine waters: examples from eastern svalbard ...
publisher Elsevier
publishDate 2017
url https://dx.doi.org/10.17863/cam.13691
https://www.repository.cam.ac.uk/handle/1810/267761
geographic Svalbard
geographic_facet Svalbard
genre glacier
Svalbard
Tidewater
genre_facet glacier
Svalbard
Tidewater
op_rights open.access
Creative Commons Attribution Non Commercial No Derivatives 4.0 International
Creative Commons Attribution Non Commercial No Derivatives 4.0 International
Attribution-NonCommercial-NoDerivatives 4.0 International
Attribution-NonCommercial-NoDerivatives 4.0 International
https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode
cc-by-nc-nd-4.0
https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode
cc-by-nc-nd-4.0
http://purl.org/coar/access_right/c_abf2
op_doi https://doi.org/10.17863/cam.13691
_version_ 1789965986678439936