Effects of rock avalanches on glacier behaviour and moraine formation

Although large rock avalanches are infrequent, sediment production in active orogens is dominated by such events, which may strongly influence geomorphic processes. Where rock avalanches fall onto glaciers, they may affect glacier behaviour and moraine formation. We outline the processes of rock ava...

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Published in:Geomorphology
Main Authors: Reznichenko, Natalya V., Davies, Tim R. H., Alexander, David J.
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2011
Subjects:
Online Access:https://espace.library.uq.edu.au/view/UQ:247025
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spelling ftunivqespace:oai:espace.library.uq.edu.au:UQ:247025 2023-05-15T16:22:27+02:00 Effects of rock avalanches on glacier behaviour and moraine formation Reznichenko, Natalya V. Davies, Tim R. H. Alexander, David J. 2011-09-15 https://espace.library.uq.edu.au/view/UQ:247025 eng eng Elsevier doi:10.1016/j.geomorph.2011.05.019 issn:0169-555X issn:1872-695X Rock avalanches Supraglacial debris Ice-surface ablation Glacier advances Terminal moraines Paleoclimatology and hazards Central Southern Alps New-Zealand Debris layer Karakoram Himalaya Climate-change Catastrophic landslides Balance model Denali fault Earthquake Canada 1904 Earth-Surface Processes Journal Article 2011 ftunivqespace https://doi.org/10.1016/j.geomorph.2011.05.019 2020-10-27T01:02:17Z Although large rock avalanches are infrequent, sediment production in active orogens is dominated by such events, which may strongly influence geomorphic processes. Where rock avalanches fall onto glaciers, they may affect glacier behaviour and moraine formation. We outline the processes of rock avalanche initiation and motion, and show that supraglacial deposits of rock avalanche debris have distinct sedimentological and thermal properties. Laboratory experiments on the effects of such debris on ice ablation are supplemented by field data from two rock avalanches in the Southern Alps, New Zealand. Their effects are compared with those of the thinner supraglacial debris that results from small rockfalls and melt-out of englacial debris. Implications of rock-avalanche debris cover for glacier behaviour are explored using a mass-balance model of the Franz Josef Glacier in New Zealand, demonstrating a likely supraglacial rock avalanche origin for the Waiho Loop moraine, and considering the potential hazard of a large rock avalanche onto the present-day glacier. Article in Journal/Newspaper glacier* The University of Queensland: UQ eSpace Canada New Zealand Geomorphology 132 3-4 327 338
institution Open Polar
collection The University of Queensland: UQ eSpace
op_collection_id ftunivqespace
language English
topic Rock avalanches
Supraglacial debris
Ice-surface ablation
Glacier advances
Terminal moraines
Paleoclimatology and hazards
Central Southern Alps
New-Zealand
Debris layer
Karakoram Himalaya
Climate-change
Catastrophic landslides
Balance model
Denali fault
Earthquake
Canada
1904 Earth-Surface Processes
spellingShingle Rock avalanches
Supraglacial debris
Ice-surface ablation
Glacier advances
Terminal moraines
Paleoclimatology and hazards
Central Southern Alps
New-Zealand
Debris layer
Karakoram Himalaya
Climate-change
Catastrophic landslides
Balance model
Denali fault
Earthquake
Canada
1904 Earth-Surface Processes
Reznichenko, Natalya V.
Davies, Tim R. H.
Alexander, David J.
Effects of rock avalanches on glacier behaviour and moraine formation
topic_facet Rock avalanches
Supraglacial debris
Ice-surface ablation
Glacier advances
Terminal moraines
Paleoclimatology and hazards
Central Southern Alps
New-Zealand
Debris layer
Karakoram Himalaya
Climate-change
Catastrophic landslides
Balance model
Denali fault
Earthquake
Canada
1904 Earth-Surface Processes
description Although large rock avalanches are infrequent, sediment production in active orogens is dominated by such events, which may strongly influence geomorphic processes. Where rock avalanches fall onto glaciers, they may affect glacier behaviour and moraine formation. We outline the processes of rock avalanche initiation and motion, and show that supraglacial deposits of rock avalanche debris have distinct sedimentological and thermal properties. Laboratory experiments on the effects of such debris on ice ablation are supplemented by field data from two rock avalanches in the Southern Alps, New Zealand. Their effects are compared with those of the thinner supraglacial debris that results from small rockfalls and melt-out of englacial debris. Implications of rock-avalanche debris cover for glacier behaviour are explored using a mass-balance model of the Franz Josef Glacier in New Zealand, demonstrating a likely supraglacial rock avalanche origin for the Waiho Loop moraine, and considering the potential hazard of a large rock avalanche onto the present-day glacier.
format Article in Journal/Newspaper
author Reznichenko, Natalya V.
Davies, Tim R. H.
Alexander, David J.
author_facet Reznichenko, Natalya V.
Davies, Tim R. H.
Alexander, David J.
author_sort Reznichenko, Natalya V.
title Effects of rock avalanches on glacier behaviour and moraine formation
title_short Effects of rock avalanches on glacier behaviour and moraine formation
title_full Effects of rock avalanches on glacier behaviour and moraine formation
title_fullStr Effects of rock avalanches on glacier behaviour and moraine formation
title_full_unstemmed Effects of rock avalanches on glacier behaviour and moraine formation
title_sort effects of rock avalanches on glacier behaviour and moraine formation
publisher Elsevier
publishDate 2011
url https://espace.library.uq.edu.au/view/UQ:247025
geographic Canada
New Zealand
geographic_facet Canada
New Zealand
genre glacier*
genre_facet glacier*
op_relation doi:10.1016/j.geomorph.2011.05.019
issn:0169-555X
issn:1872-695X
op_doi https://doi.org/10.1016/j.geomorph.2011.05.019
container_title Geomorphology
container_volume 132
container_issue 3-4
container_start_page 327
op_container_end_page 338
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