Microseismic activity within a serac zone in an alpine glacier (Glacier d'Argentieire, Mont Blanc, France)

International audience A passive seismic study was carried out underneath Glacier d'Argentiere, Mont Blanc, France, where an array of seismometers was installed in a subglacial access tunnel. The data show a very high emissivity from the glacier. Fracturing can be discriminated from serac falls...

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Published in:Journal of Glaciology
Main Authors: Roux, P., Marsan, David, Metaxian, J. P., O'Brien, G., Moreau, Luc
Other Authors: Laboratoire de Géophysique Interne et Tectonophysique (LGIT), Observatoire des Sciences de l'Univers de Grenoble (OSUG), Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Laboratoire Central des Ponts et Chaussées (LCPC)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS), University College Dublin Dublin (UCD), Environnements, Dynamiques et Territoires de Montagne (EDYTEM), Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2008
Subjects:
ICE
Online Access:https://insu.hal.science/insu-00343887
https://insu.hal.science/insu-00343887/document
https://insu.hal.science/insu-00343887/file/microseismic-activity-within-a-serac-zone-in-an-alpine-glacier-glacier-dargentiere-mont-blanc-france.pdf
https://doi.org/10.3189/002214308784409053
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record_format openpolar
spelling ftunigrenoble:oai:HAL:insu-00343887v1 2024-04-28T08:26:50+00:00 Microseismic activity within a serac zone in an alpine glacier (Glacier d'Argentieire, Mont Blanc, France) Roux, P. Marsan, David Metaxian, J. P. O'Brien, G. Moreau, Luc Laboratoire de Géophysique Interne et Tectonophysique (LGIT) Observatoire des Sciences de l'Univers de Grenoble (OSUG) Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Laboratoire Central des Ponts et Chaussées (LCPC)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS) University College Dublin Dublin (UCD) Environnements, Dynamiques et Territoires de Montagne (EDYTEM) Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS) 2008 https://insu.hal.science/insu-00343887 https://insu.hal.science/insu-00343887/document https://insu.hal.science/insu-00343887/file/microseismic-activity-within-a-serac-zone-in-an-alpine-glacier-glacier-dargentiere-mont-blanc-france.pdf https://doi.org/10.3189/002214308784409053 en eng HAL CCSD International Glaciological Society info:eu-repo/semantics/altIdentifier/doi/10.3189/002214308784409053 insu-00343887 https://insu.hal.science/insu-00343887 https://insu.hal.science/insu-00343887/document https://insu.hal.science/insu-00343887/file/microseismic-activity-within-a-serac-zone-in-an-alpine-glacier-glacier-dargentiere-mont-blanc-france.pdf doi:10.3189/002214308784409053 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 0022-1430 EISSN: 1727-5652 Journal of Glaciology https://insu.hal.science/insu-00343887 Journal of Glaciology, 2008, 54 (184), pp.157 -168. ⟨10.3189/002214308784409053⟩ ICEQUAKES CALIFORNIA EARTHQUAKES ICE ARRAY GEOMETRY BENEATH MOTION [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology [SDE.ES]Environmental Sciences/Environment and Society info:eu-repo/semantics/article Journal articles 2008 ftunigrenoble https://doi.org/10.3189/002214308784409053 2024-04-18T03:12:00Z International audience A passive seismic study was carried out underneath Glacier d'Argentiere, Mont Blanc, France, where an array of seismometers was installed in a subglacial access tunnel. The data show a very high emissivity from the glacier. Fracturing can be discriminated from serac falls using the signal characteristics. We apply seismic array methods to locate the sources of these signals, using a two-step grid search in the parameter space. Four clusters of activity are found close to the network, showing that this fracturing does not take place uniformly over the glacier, but rather in isolated small zones. We compute a local magnitude using regional earthquakes for calibration. The magnitudes follow a classical Gutenberg-Richter law in the range M-L = -3 to 0.15, showing that no characteristic size events dominate the process. We suggest that those spatial clusters of icequakes could reveal the heterogeneous nature of the friction at the base of the glacier, with patches of high frictional stresses locally generating intense fracturing within the ice mass. Article in Journal/Newspaper Journal of Glaciology Université Grenoble Alpes: HAL Journal of Glaciology 54 184 157 168
institution Open Polar
collection Université Grenoble Alpes: HAL
op_collection_id ftunigrenoble
language English
topic ICEQUAKES
CALIFORNIA
EARTHQUAKES
ICE
ARRAY
GEOMETRY
BENEATH
MOTION
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
[SDE.ES]Environmental Sciences/Environment and Society
spellingShingle ICEQUAKES
CALIFORNIA
EARTHQUAKES
ICE
ARRAY
GEOMETRY
BENEATH
MOTION
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
[SDE.ES]Environmental Sciences/Environment and Society
Roux, P.
Marsan, David
Metaxian, J. P.
O'Brien, G.
Moreau, Luc
Microseismic activity within a serac zone in an alpine glacier (Glacier d'Argentieire, Mont Blanc, France)
topic_facet ICEQUAKES
CALIFORNIA
EARTHQUAKES
ICE
ARRAY
GEOMETRY
BENEATH
MOTION
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
[SDE.ES]Environmental Sciences/Environment and Society
description International audience A passive seismic study was carried out underneath Glacier d'Argentiere, Mont Blanc, France, where an array of seismometers was installed in a subglacial access tunnel. The data show a very high emissivity from the glacier. Fracturing can be discriminated from serac falls using the signal characteristics. We apply seismic array methods to locate the sources of these signals, using a two-step grid search in the parameter space. Four clusters of activity are found close to the network, showing that this fracturing does not take place uniformly over the glacier, but rather in isolated small zones. We compute a local magnitude using regional earthquakes for calibration. The magnitudes follow a classical Gutenberg-Richter law in the range M-L = -3 to 0.15, showing that no characteristic size events dominate the process. We suggest that those spatial clusters of icequakes could reveal the heterogeneous nature of the friction at the base of the glacier, with patches of high frictional stresses locally generating intense fracturing within the ice mass.
author2 Laboratoire de Géophysique Interne et Tectonophysique (LGIT)
Observatoire des Sciences de l'Univers de Grenoble (OSUG)
Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Laboratoire Central des Ponts et Chaussées (LCPC)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)
University College Dublin Dublin (UCD)
Environnements, Dynamiques et Territoires de Montagne (EDYTEM)
Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)
format Article in Journal/Newspaper
author Roux, P.
Marsan, David
Metaxian, J. P.
O'Brien, G.
Moreau, Luc
author_facet Roux, P.
Marsan, David
Metaxian, J. P.
O'Brien, G.
Moreau, Luc
author_sort Roux, P.
title Microseismic activity within a serac zone in an alpine glacier (Glacier d'Argentieire, Mont Blanc, France)
title_short Microseismic activity within a serac zone in an alpine glacier (Glacier d'Argentieire, Mont Blanc, France)
title_full Microseismic activity within a serac zone in an alpine glacier (Glacier d'Argentieire, Mont Blanc, France)
title_fullStr Microseismic activity within a serac zone in an alpine glacier (Glacier d'Argentieire, Mont Blanc, France)
title_full_unstemmed Microseismic activity within a serac zone in an alpine glacier (Glacier d'Argentieire, Mont Blanc, France)
title_sort microseismic activity within a serac zone in an alpine glacier (glacier d'argentieire, mont blanc, france)
publisher HAL CCSD
publishDate 2008
url https://insu.hal.science/insu-00343887
https://insu.hal.science/insu-00343887/document
https://insu.hal.science/insu-00343887/file/microseismic-activity-within-a-serac-zone-in-an-alpine-glacier-glacier-dargentiere-mont-blanc-france.pdf
https://doi.org/10.3189/002214308784409053
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source ISSN: 0022-1430
EISSN: 1727-5652
Journal of Glaciology
https://insu.hal.science/insu-00343887
Journal of Glaciology, 2008, 54 (184), pp.157 -168. ⟨10.3189/002214308784409053⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.3189/002214308784409053
insu-00343887
https://insu.hal.science/insu-00343887
https://insu.hal.science/insu-00343887/document
https://insu.hal.science/insu-00343887/file/microseismic-activity-within-a-serac-zone-in-an-alpine-glacier-glacier-dargentiere-mont-blanc-france.pdf
doi:10.3189/002214308784409053
op_rights http://creativecommons.org/licenses/by/
info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.3189/002214308784409053
container_title Journal of Glaciology
container_volume 54
container_issue 184
container_start_page 157
op_container_end_page 168
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