Palaeofluvial and subglacial channel networks beneath Humboldt Glacier, Greenland
The identification of subglacial drainage systems can inform our understanding of past and present hydrological processes, landscape evolution, and ice dynamics. Here, we present evidence from satellite imagery, digital elevation models, and radio-echo sounding data for a series of channelized netwo...
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Geological Society of America
2017
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ftleedsuniv:oai:eprints.whiterose.ac.uk:113109 2023-05-15T16:20:59+02:00 Palaeofluvial and subglacial channel networks beneath Humboldt Glacier, Greenland Livingstone, S.J. Chu, W. Ely, J.C. Kingslake, J. 2017 text https://eprints.whiterose.ac.uk/113109/ https://eprints.whiterose.ac.uk/113109/9/Geology-2017-Livingstone-551-4.pdf https://doi.org/10.1130/G38860.1 en eng Geological Society of America https://eprints.whiterose.ac.uk/113109/9/Geology-2017-Livingstone-551-4.pdf Livingstone, S.J. orcid.org/0000-0002-7240-5037 , Chu, W., Ely, J.C. et al. (1 more author) (2017) Palaeofluvial and subglacial channel networks beneath Humboldt Glacier, Greenland. Geology, 45 (6). pp. 551-554. ISSN 0091-7613 Article PeerReviewed 2017 ftleedsuniv https://doi.org/10.1130/G38860.1 2023-01-30T21:52:21Z The identification of subglacial drainage systems can inform our understanding of past and present hydrological processes, landscape evolution, and ice dynamics. Here, we present evidence from satellite imagery, digital elevation models, and radio-echo sounding data for a series of channelized networks with contrasting paleofluvial and subglacial origins beneath Humboldt Glacier, northern Greenland. A >250-km-long, dendritic paleofluvial channel network beneath the northern portion of Humboldt is interpreted as a preglacial feature. Roughly linear channels beneath the southern portion of Humboldt, which display a similar distribution to tunnel valleys found on the beds of former ice sheets, are likely to have been eroded by subglacial meltwater routed along the ice-sheet bed. We suggest that basal meltwater is actively being routed down both the paleofluvial and subglacially formed channel networks to the coast. Inheritance of the preglacial channel network may have influenced the present-day location and dynamics of Humboldt Glacier and enhanced selective erosion at its down-glacier end. Article in Journal/Newspaper glacier Greenland Humboldt Glacier Ice Sheet White Rose Research Online (Universities of Leeds, Sheffield & York) Greenland Geology 45 6 551 554 |
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Open Polar |
collection |
White Rose Research Online (Universities of Leeds, Sheffield & York) |
op_collection_id |
ftleedsuniv |
language |
English |
description |
The identification of subglacial drainage systems can inform our understanding of past and present hydrological processes, landscape evolution, and ice dynamics. Here, we present evidence from satellite imagery, digital elevation models, and radio-echo sounding data for a series of channelized networks with contrasting paleofluvial and subglacial origins beneath Humboldt Glacier, northern Greenland. A >250-km-long, dendritic paleofluvial channel network beneath the northern portion of Humboldt is interpreted as a preglacial feature. Roughly linear channels beneath the southern portion of Humboldt, which display a similar distribution to tunnel valleys found on the beds of former ice sheets, are likely to have been eroded by subglacial meltwater routed along the ice-sheet bed. We suggest that basal meltwater is actively being routed down both the paleofluvial and subglacially formed channel networks to the coast. Inheritance of the preglacial channel network may have influenced the present-day location and dynamics of Humboldt Glacier and enhanced selective erosion at its down-glacier end. |
format |
Article in Journal/Newspaper |
author |
Livingstone, S.J. Chu, W. Ely, J.C. Kingslake, J. |
spellingShingle |
Livingstone, S.J. Chu, W. Ely, J.C. Kingslake, J. Palaeofluvial and subglacial channel networks beneath Humboldt Glacier, Greenland |
author_facet |
Livingstone, S.J. Chu, W. Ely, J.C. Kingslake, J. |
author_sort |
Livingstone, S.J. |
title |
Palaeofluvial and subglacial channel networks beneath Humboldt Glacier, Greenland |
title_short |
Palaeofluvial and subglacial channel networks beneath Humboldt Glacier, Greenland |
title_full |
Palaeofluvial and subglacial channel networks beneath Humboldt Glacier, Greenland |
title_fullStr |
Palaeofluvial and subglacial channel networks beneath Humboldt Glacier, Greenland |
title_full_unstemmed |
Palaeofluvial and subglacial channel networks beneath Humboldt Glacier, Greenland |
title_sort |
palaeofluvial and subglacial channel networks beneath humboldt glacier, greenland |
publisher |
Geological Society of America |
publishDate |
2017 |
url |
https://eprints.whiterose.ac.uk/113109/ https://eprints.whiterose.ac.uk/113109/9/Geology-2017-Livingstone-551-4.pdf https://doi.org/10.1130/G38860.1 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
glacier Greenland Humboldt Glacier Ice Sheet |
genre_facet |
glacier Greenland Humboldt Glacier Ice Sheet |
op_relation |
https://eprints.whiterose.ac.uk/113109/9/Geology-2017-Livingstone-551-4.pdf Livingstone, S.J. orcid.org/0000-0002-7240-5037 , Chu, W., Ely, J.C. et al. (1 more author) (2017) Palaeofluvial and subglacial channel networks beneath Humboldt Glacier, Greenland. Geology, 45 (6). pp. 551-554. ISSN 0091-7613 |
op_doi |
https://doi.org/10.1130/G38860.1 |
container_title |
Geology |
container_volume |
45 |
container_issue |
6 |
container_start_page |
551 |
op_container_end_page |
554 |
_version_ |
1766009000684421120 |