Short communication: Runout of rock avalanches limited by basal friction but controlled by fragmentation
<p>Rock avalanches produce exceptionally long run-outs that correlate with their rock volume. This relationship has been attributed to the size-dependent dynamic lowering of the effective basal friction. However, it has also been observed that run-outs of rock avalanches with similar volumes c...
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Copernicus Publications
2021-06-01
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Series: | Earth Surface Dynamics |
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doaj-849285fc857243dd90271c85bbdbbb472021-06-23T07:41:33ZengCopernicus PublicationsEarth Surface Dynamics2196-63112196-632X2021-06-01966567210.5194/esurf-9-665-2021Short communication: Runout of rock avalanches limited by basal friction but controlled by fragmentationØ. T. Haug0Ø. T. Haug1M. Rosenau2M. Rudolf3K. Leever4K. Leever5O. Oncken6GFZ German Research Centre for Geosciences, Helmholtz Centre Potsdam, Telegrafenberg, 14473 Potsdam, GermanyNjord centre, Department of Geosciences, University of Oslo, P.O. Box 1048, 0316 Oslo, NorwayGFZ German Research Centre for Geosciences, Helmholtz Centre Potsdam, Telegrafenberg, 14473 Potsdam, GermanyGFZ German Research Centre for Geosciences, Helmholtz Centre Potsdam, Telegrafenberg, 14473 Potsdam, GermanyGFZ German Research Centre for Geosciences, Helmholtz Centre Potsdam, Telegrafenberg, 14473 Potsdam, GermanyVan Hall Larenstein University of Applied Sciences, Larensteinselaan 26a, 6882 Velp, the NetherlandsGFZ German Research Centre for Geosciences, Helmholtz Centre Potsdam, Telegrafenberg, 14473 Potsdam, Germany<p>Rock avalanches produce exceptionally long run-outs that correlate with their rock volume. This relationship has been attributed to the size-dependent dynamic lowering of the effective basal friction. However, it has also been observed that run-outs of rock avalanches with similar volumes can span several orders of magnitude, suggesting additional controlling factors. Here, we analyse analogue models of rock avalanches, with the experiments designed to test the role of dynamic fragmentation. We show that for a fixed low basal friction, the run-out of experimental rock avalanches varies over 2 orders of magnitude and is determined by their degree of fragmentation, while the basal friction acts only as an upper limit on run-out. We interpret the run-out's dependence on fragmentation as being controlled by the competition between mobility enhancing spreading and energy-consuming fragmentation limited by basal friction. We formalize this competition into a scaling law based on energy conservation, which shows that the variation in the degree of fragmentation can contribute to the large variation in run-out of rock avalanches seen in nature.</p>https://esurf.copernicus.org/articles/9/665/2021/esurf-9-665-2021.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Ø. T. Haug Ø. T. Haug M. Rosenau M. Rudolf K. Leever K. Leever O. Oncken |
spellingShingle |
Ø. T. Haug Ø. T. Haug M. Rosenau M. Rudolf K. Leever K. Leever O. Oncken Short communication: Runout of rock avalanches limited by basal friction but controlled by fragmentation Earth Surface Dynamics |
author_facet |
Ø. T. Haug Ø. T. Haug M. Rosenau M. Rudolf K. Leever K. Leever O. Oncken |
author_sort |
Ø. T. Haug |
title |
Short communication: Runout of rock avalanches limited by basal friction but controlled by fragmentation |
title_short |
Short communication: Runout of rock avalanches limited by basal friction but controlled by fragmentation |
title_full |
Short communication: Runout of rock avalanches limited by basal friction but controlled by fragmentation |
title_fullStr |
Short communication: Runout of rock avalanches limited by basal friction but controlled by fragmentation |
title_full_unstemmed |
Short communication: Runout of rock avalanches limited by basal friction but controlled by fragmentation |
title_sort |
short communication: runout of rock avalanches limited by basal friction but controlled by fragmentation |
publisher |
Copernicus Publications |
series |
Earth Surface Dynamics |
issn |
2196-6311 2196-632X |
publishDate |
2021-06-01 |
description |
<p>Rock avalanches produce exceptionally long run-outs that correlate with their rock volume. This relationship has been attributed to the size-dependent dynamic lowering of the effective basal friction. However, it has also been observed that run-outs of rock avalanches with similar volumes can span several orders of magnitude, suggesting additional controlling factors. Here, we analyse analogue models of rock avalanches, with the experiments designed to test the role of dynamic fragmentation. We show that for a fixed low basal friction, the run-out of experimental rock avalanches varies over 2 orders of magnitude and is determined by their degree of fragmentation, while the basal friction acts only as an upper limit on run-out. We interpret the run-out's dependence on fragmentation as being controlled by the competition between mobility enhancing spreading and energy-consuming fragmentation limited by basal friction. We formalize this competition into a scaling law based on energy conservation, which shows that the variation in the degree of fragmentation can contribute to the large variation in run-out of rock avalanches seen in nature.</p> |
url |
https://esurf.copernicus.org/articles/9/665/2021/esurf-9-665-2021.pdf |
work_keys_str_mv |
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