Tilt signals at Mount Melbourne, Antarctica: evidence of a shallow volcanic source

Mount Melbourne (74°21′ S, 164°43′ E) is a quiescent volcano located in northern Victoria Land, Antarctica. Tilt signals have been recorded on Mount Melbourne since early 1989 by a permanent shallow borehole tiltmeter network comprising five stations. An overall picture of tilt, air and permafrost t...

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Main Authors: Salvatore Gambino, Marco Aloisi, Giuseppe Falzone, Angelo Ferro
Format: Article
Language:English
Published: Norwegian Polar Institute 2016-06-01
Series:Polar Research
Subjects:
Online Access:http://www.polarresearch.net/index.php/polar/article/view/28269/46926
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author Salvatore Gambino
Marco Aloisi
Giuseppe Falzone
Angelo Ferro
author_facet Salvatore Gambino
Marco Aloisi
Giuseppe Falzone
Angelo Ferro
author_sort Salvatore Gambino
collection DOAJ
description Mount Melbourne (74°21′ S, 164°43′ E) is a quiescent volcano located in northern Victoria Land, Antarctica. Tilt signals have been recorded on Mount Melbourne since early 1989 by a permanent shallow borehole tiltmeter network comprising five stations. An overall picture of tilt, air and permafrost temperatures over 15 years of continuous recording data is reported. We focused our observations on long-term tilt trends that at the end of 1997 showed coherent changes at the three highest altitude stations, suggesting the presence of a ground deformation source whose effects are restricted to the summit area of Mount Melbourne. We inverted these data using a finite spherical body source, thereby obtaining a shallow deflation volume source located under the summit area. The ground deformation observed corroborates the hypothesis that the volcanic edifice of Mount Melbourne is active and should be monitored multidisciplinarily.
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spelling doaj.art-5b23335de6354d2f9ae0bad7d84d21b62022-12-21T22:12:07ZengNorwegian Polar InstitutePolar Research1751-83692016-06-013501910.3402/polar.v35.2826928269Tilt signals at Mount Melbourne, Antarctica: evidence of a shallow volcanic sourceSalvatore Gambino0Marco Aloisi1Giuseppe Falzone2Angelo Ferro3Catania Department, National Institute of Geophysics and Volcanology, Piazza Roma 2, IT-95123 Catania, ItalyCatania Department, National Institute of Geophysics and Volcanology, Piazza Roma 2, IT-95123 Catania, ItalyCatania Department, National Institute of Geophysics and Volcanology, Piazza Roma 2, IT-95123 Catania, ItalyCatania Department, National Institute of Geophysics and Volcanology, Piazza Roma 2, IT-95123 Catania, ItalyMount Melbourne (74°21′ S, 164°43′ E) is a quiescent volcano located in northern Victoria Land, Antarctica. Tilt signals have been recorded on Mount Melbourne since early 1989 by a permanent shallow borehole tiltmeter network comprising five stations. An overall picture of tilt, air and permafrost temperatures over 15 years of continuous recording data is reported. We focused our observations on long-term tilt trends that at the end of 1997 showed coherent changes at the three highest altitude stations, suggesting the presence of a ground deformation source whose effects are restricted to the summit area of Mount Melbourne. We inverted these data using a finite spherical body source, thereby obtaining a shallow deflation volume source located under the summit area. The ground deformation observed corroborates the hypothesis that the volcanic edifice of Mount Melbourne is active and should be monitored multidisciplinarily.http://www.polarresearch.net/index.php/polar/article/view/28269/46926Tilt monitoringvolcanic dynamicsphysics volcanologyground deformationVictoria Land
spellingShingle Salvatore Gambino
Marco Aloisi
Giuseppe Falzone
Angelo Ferro
Tilt signals at Mount Melbourne, Antarctica: evidence of a shallow volcanic source
Polar Research
Tilt monitoring
volcanic dynamics
physics volcanology
ground deformation
Victoria Land
title Tilt signals at Mount Melbourne, Antarctica: evidence of a shallow volcanic source
title_full Tilt signals at Mount Melbourne, Antarctica: evidence of a shallow volcanic source
title_fullStr Tilt signals at Mount Melbourne, Antarctica: evidence of a shallow volcanic source
title_full_unstemmed Tilt signals at Mount Melbourne, Antarctica: evidence of a shallow volcanic source
title_short Tilt signals at Mount Melbourne, Antarctica: evidence of a shallow volcanic source
title_sort tilt signals at mount melbourne antarctica evidence of a shallow volcanic source
topic Tilt monitoring
volcanic dynamics
physics volcanology
ground deformation
Victoria Land
url http://www.polarresearch.net/index.php/polar/article/view/28269/46926
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AT giuseppefalzone tiltsignalsatmountmelbourneantarcticaevidenceofashallowvolcanicsource
AT angeloferro tiltsignalsatmountmelbourneantarcticaevidenceofashallowvolcanicsource