Borehole-Based Characterization of Deep Mixed-Mode Crevasses at a Greenlandic Outlet Glacier ...

Funder: Aberystwyth University Capital Equipment Fund ... : AbstractOptical televiewer borehole logging within a crevassed region of fast‐moving Store Glacier, Greenland, revealed the presence of 35 high‐angle planes that cut across the background primary stratification. These planes were composed o...

Full description

Bibliographic Details
Main Authors: Hubbard, Bryn, Christoffersen, Poul, Doyle, Samuel H, Chudley, Thomas R, Schoonman, Charlotte M, Law, Robert, Bougamont, Marion
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union (AGU) 2021
Subjects:
Online Access:https://dx.doi.org/10.17863/cam.70842
https://www.repository.cam.ac.uk/handle/1810/323384
id ftdatacite:10.17863/cam.70842
record_format openpolar
spelling ftdatacite:10.17863/cam.70842 2024-02-27T08:40:44+00:00 Borehole-Based Characterization of Deep Mixed-Mode Crevasses at a Greenlandic Outlet Glacier ... Hubbard, Bryn Christoffersen, Poul Doyle, Samuel H Chudley, Thomas R Schoonman, Charlotte M Law, Robert Bougamont, Marion 2021 https://dx.doi.org/10.17863/cam.70842 https://www.repository.cam.ac.uk/handle/1810/323384 en eng American Geophysical Union (AGU) borehole crevasse deep crevasse glacier Greenland Ice Sheet optical televiewer article-journal ScholarlyArticle JournalArticle Article 2021 ftdatacite https://doi.org/10.17863/cam.70842 2024-02-01T14:49:26Z Funder: Aberystwyth University Capital Equipment Fund ... : AbstractOptical televiewer borehole logging within a crevassed region of fast‐moving Store Glacier, Greenland, revealed the presence of 35 high‐angle planes that cut across the background primary stratification. These planes were composed of a bubble‐free layer of refrozen ice, most of which hosted thin laminae of bubble‐rich “last frozen” ice, consistent with the planes being the traces of former open crevasses. Several such last‐frozen laminae were observed in four traces, suggesting multiple episodes of crevasse reactivation. The frequency of crevasse traces generally decreased with depth, with the deepest detectable trace being 265 m below the surface. This is consistent with the extent of the warmer‐than‐modeled englacial ice layer in the area, which extends from the surface to a depth of ∼400 m. Crevasse trace orientation was strongly clustered around a dip of 63° and a strike that was offset by 71° from orthogonal to the local direction of principal extending strain. The traces’ antecedent crevasses ... Article in Journal/Newspaper glacier Greenland greenlandic Ice Sheet DataCite Metadata Store (German National Library of Science and Technology) Greenland
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic borehole
crevasse
deep crevasse
glacier
Greenland Ice Sheet
optical televiewer
spellingShingle borehole
crevasse
deep crevasse
glacier
Greenland Ice Sheet
optical televiewer
Hubbard, Bryn
Christoffersen, Poul
Doyle, Samuel H
Chudley, Thomas R
Schoonman, Charlotte M
Law, Robert
Bougamont, Marion
Borehole-Based Characterization of Deep Mixed-Mode Crevasses at a Greenlandic Outlet Glacier ...
topic_facet borehole
crevasse
deep crevasse
glacier
Greenland Ice Sheet
optical televiewer
description Funder: Aberystwyth University Capital Equipment Fund ... : AbstractOptical televiewer borehole logging within a crevassed region of fast‐moving Store Glacier, Greenland, revealed the presence of 35 high‐angle planes that cut across the background primary stratification. These planes were composed of a bubble‐free layer of refrozen ice, most of which hosted thin laminae of bubble‐rich “last frozen” ice, consistent with the planes being the traces of former open crevasses. Several such last‐frozen laminae were observed in four traces, suggesting multiple episodes of crevasse reactivation. The frequency of crevasse traces generally decreased with depth, with the deepest detectable trace being 265 m below the surface. This is consistent with the extent of the warmer‐than‐modeled englacial ice layer in the area, which extends from the surface to a depth of ∼400 m. Crevasse trace orientation was strongly clustered around a dip of 63° and a strike that was offset by 71° from orthogonal to the local direction of principal extending strain. The traces’ antecedent crevasses ...
format Article in Journal/Newspaper
author Hubbard, Bryn
Christoffersen, Poul
Doyle, Samuel H
Chudley, Thomas R
Schoonman, Charlotte M
Law, Robert
Bougamont, Marion
author_facet Hubbard, Bryn
Christoffersen, Poul
Doyle, Samuel H
Chudley, Thomas R
Schoonman, Charlotte M
Law, Robert
Bougamont, Marion
author_sort Hubbard, Bryn
title Borehole-Based Characterization of Deep Mixed-Mode Crevasses at a Greenlandic Outlet Glacier ...
title_short Borehole-Based Characterization of Deep Mixed-Mode Crevasses at a Greenlandic Outlet Glacier ...
title_full Borehole-Based Characterization of Deep Mixed-Mode Crevasses at a Greenlandic Outlet Glacier ...
title_fullStr Borehole-Based Characterization of Deep Mixed-Mode Crevasses at a Greenlandic Outlet Glacier ...
title_full_unstemmed Borehole-Based Characterization of Deep Mixed-Mode Crevasses at a Greenlandic Outlet Glacier ...
title_sort borehole-based characterization of deep mixed-mode crevasses at a greenlandic outlet glacier ...
publisher American Geophysical Union (AGU)
publishDate 2021
url https://dx.doi.org/10.17863/cam.70842
https://www.repository.cam.ac.uk/handle/1810/323384
geographic Greenland
geographic_facet Greenland
genre glacier
Greenland
greenlandic
Ice Sheet
genre_facet glacier
Greenland
greenlandic
Ice Sheet
op_doi https://doi.org/10.17863/cam.70842
_version_ 1792047865643663360