Formation of crevasse-squeeze ridges at Trygghamna, Svalbard
Crevasse-squeeze ridges (CSRs) are landforms that have been unequivocally linked to surge-type glaciers. The formation of CSRs has been discussed since they were first defined in the mid-1980s. Here, we describe geometric CSR networks from the terrestrial glacier forefields of two glaciers in Tryggh...
Published in: | Earth Surface Processes and Landforms |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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2023
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Online Access: | https://curis.ku.dk/portal/da/publications/formation-of-crevassesqueeze-ridges-at-trygghamna-svalbard(9450a912-c5cf-4808-b6f5-14219ebdb881).html https://doi.org/10.1002/esp.5631 https://curis.ku.dk/ws/files/357188025/Earth_Surf_Processes_Landf_2023_Ben_Yehoshua_Formation_of_crevasse_squeeze_ridges_at_Trygghamna_Svalbard.pdf |
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ftcopenhagenunip:oai:pure.atira.dk:publications/9450a912-c5cf-4808-b6f5-14219ebdb881 2024-06-09T07:46:10+00:00 Formation of crevasse-squeeze ridges at Trygghamna, Svalbard Ben-Yehoshua, Daniel Aradóttir, Nína Farnsworth, Wesley R. Benediktsson, Ívar Örn Ingólfsson, Ólafur 2023 application/pdf https://curis.ku.dk/portal/da/publications/formation-of-crevassesqueeze-ridges-at-trygghamna-svalbard(9450a912-c5cf-4808-b6f5-14219ebdb881).html https://doi.org/10.1002/esp.5631 https://curis.ku.dk/ws/files/357188025/Earth_Surf_Processes_Landf_2023_Ben_Yehoshua_Formation_of_crevasse_squeeze_ridges_at_Trygghamna_Svalbard.pdf eng eng info:eu-repo/semantics/openAccess Ben-Yehoshua , D , Aradóttir , N , Farnsworth , W R , Benediktsson , Í Ö & Ingólfsson , Ó 2023 , ' Formation of crevasse-squeeze ridges at Trygghamna, Svalbard ' , Earth Surface Processes and Landforms , vol. 48 , no. 12 , pp. 2334-2348 . https://doi.org/10.1002/esp.5631 crevasse fill ridges crevasse-squeeze ridges glacier retreat landform formation ridge networks subglacial processes surging glacier Svalbard article 2023 ftcopenhagenunip https://doi.org/10.1002/esp.5631 2024-05-16T11:29:29Z Crevasse-squeeze ridges (CSRs) are landforms that have been unequivocally linked to surge-type glaciers. The formation of CSRs has been discussed since they were first defined in the mid-1980s. Here, we describe geometric CSR networks from the terrestrial glacier forefields of two glaciers in Trygghamna, Western Svalbard. No glacier surges have been observed in Trygghamna; however, the presence of the CSRs signifies past surge activity. Detailed geomorphological maps were constructed, and the spatial context of these landforms described. Cross-sections of several CSRs highlight ridge architecture, structure and relationships to surrounding landforms and sediments. Most CSRs are symmetrical in cross-profile, orientated perpendicular or oblique to the ice-flow direction. Like previous investigations, we observe these ridge networks on top of till and flutes. Additionally, we, for the first time, document CSRs deposited directly on non-glaciogenic subsurfaces, namely, beach gravels and bedrock. Our findings confirm previous CSR formation theories; basal sediments are squeezed into bottom-up crevasses during surges, which are subsequently transported englacially until surge termination and are finally released by melt out from stagnant ice. Consequently, a network of CSRs is the product of a significant reorganisation and down-glacier transport of basal sediment, exemplifying how single surges are agents of glacial sediment redistribution. These formation processes are illustrated in a refined schematic model. The results further contemporary understanding of CSRs in terrestrial surge-type glacier settings and may also apply to landforms and sediments in certain marine settings and palaeoglacial environments. Article in Journal/Newspaper glacier Svalbard University of Copenhagen: Research Svalbard Trygghamna ENVELOPE(13.819,13.819,78.246,78.246) Earth Surface Processes and Landforms 48 12 2334 2348 |
institution |
Open Polar |
collection |
University of Copenhagen: Research |
op_collection_id |
ftcopenhagenunip |
language |
English |
topic |
crevasse fill ridges crevasse-squeeze ridges glacier retreat landform formation ridge networks subglacial processes surging glacier Svalbard |
spellingShingle |
crevasse fill ridges crevasse-squeeze ridges glacier retreat landform formation ridge networks subglacial processes surging glacier Svalbard Ben-Yehoshua, Daniel Aradóttir, Nína Farnsworth, Wesley R. Benediktsson, Ívar Örn Ingólfsson, Ólafur Formation of crevasse-squeeze ridges at Trygghamna, Svalbard |
topic_facet |
crevasse fill ridges crevasse-squeeze ridges glacier retreat landform formation ridge networks subglacial processes surging glacier Svalbard |
description |
Crevasse-squeeze ridges (CSRs) are landforms that have been unequivocally linked to surge-type glaciers. The formation of CSRs has been discussed since they were first defined in the mid-1980s. Here, we describe geometric CSR networks from the terrestrial glacier forefields of two glaciers in Trygghamna, Western Svalbard. No glacier surges have been observed in Trygghamna; however, the presence of the CSRs signifies past surge activity. Detailed geomorphological maps were constructed, and the spatial context of these landforms described. Cross-sections of several CSRs highlight ridge architecture, structure and relationships to surrounding landforms and sediments. Most CSRs are symmetrical in cross-profile, orientated perpendicular or oblique to the ice-flow direction. Like previous investigations, we observe these ridge networks on top of till and flutes. Additionally, we, for the first time, document CSRs deposited directly on non-glaciogenic subsurfaces, namely, beach gravels and bedrock. Our findings confirm previous CSR formation theories; basal sediments are squeezed into bottom-up crevasses during surges, which are subsequently transported englacially until surge termination and are finally released by melt out from stagnant ice. Consequently, a network of CSRs is the product of a significant reorganisation and down-glacier transport of basal sediment, exemplifying how single surges are agents of glacial sediment redistribution. These formation processes are illustrated in a refined schematic model. The results further contemporary understanding of CSRs in terrestrial surge-type glacier settings and may also apply to landforms and sediments in certain marine settings and palaeoglacial environments. |
format |
Article in Journal/Newspaper |
author |
Ben-Yehoshua, Daniel Aradóttir, Nína Farnsworth, Wesley R. Benediktsson, Ívar Örn Ingólfsson, Ólafur |
author_facet |
Ben-Yehoshua, Daniel Aradóttir, Nína Farnsworth, Wesley R. Benediktsson, Ívar Örn Ingólfsson, Ólafur |
author_sort |
Ben-Yehoshua, Daniel |
title |
Formation of crevasse-squeeze ridges at Trygghamna, Svalbard |
title_short |
Formation of crevasse-squeeze ridges at Trygghamna, Svalbard |
title_full |
Formation of crevasse-squeeze ridges at Trygghamna, Svalbard |
title_fullStr |
Formation of crevasse-squeeze ridges at Trygghamna, Svalbard |
title_full_unstemmed |
Formation of crevasse-squeeze ridges at Trygghamna, Svalbard |
title_sort |
formation of crevasse-squeeze ridges at trygghamna, svalbard |
publishDate |
2023 |
url |
https://curis.ku.dk/portal/da/publications/formation-of-crevassesqueeze-ridges-at-trygghamna-svalbard(9450a912-c5cf-4808-b6f5-14219ebdb881).html https://doi.org/10.1002/esp.5631 https://curis.ku.dk/ws/files/357188025/Earth_Surf_Processes_Landf_2023_Ben_Yehoshua_Formation_of_crevasse_squeeze_ridges_at_Trygghamna_Svalbard.pdf |
long_lat |
ENVELOPE(13.819,13.819,78.246,78.246) |
geographic |
Svalbard Trygghamna |
geographic_facet |
Svalbard Trygghamna |
genre |
glacier Svalbard |
genre_facet |
glacier Svalbard |
op_source |
Ben-Yehoshua , D , Aradóttir , N , Farnsworth , W R , Benediktsson , Í Ö & Ingólfsson , Ó 2023 , ' Formation of crevasse-squeeze ridges at Trygghamna, Svalbard ' , Earth Surface Processes and Landforms , vol. 48 , no. 12 , pp. 2334-2348 . https://doi.org/10.1002/esp.5631 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1002/esp.5631 |
container_title |
Earth Surface Processes and Landforms |
container_volume |
48 |
container_issue |
12 |
container_start_page |
2334 |
op_container_end_page |
2348 |
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1801375927166304256 |