Advances in Understanding Intrusive, Explosive and Effusive Processes as Revealed by the Borehole Dilatometer Network on Mt. Etna Volcano

For detecting below surface sources of deformation, strain measurements offer a very large advantage (orders of magnitude) in sensitivity over displacement measurements. On active volcanoes an intriguing open challenge is to measure the strain variations caused by the different types of eruptive act...

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Main Authors: Alessandro Bonaccorso, Gilda Currenti, Alan Linde, Selwyn Sacks, Antonino Sicali
Format: Article
Language:English
Published: Frontiers Media S.A. 2020-01-01
Series:Frontiers in Earth Science
Subjects:
Online Access:https://www.frontiersin.org/article/10.3389/feart.2019.00357/full
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spelling doaj-8820935f44794b0e9dc39faed92152552020-11-25T02:06:38ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632020-01-01710.3389/feart.2019.00357486761Advances in Understanding Intrusive, Explosive and Effusive Processes as Revealed by the Borehole Dilatometer Network on Mt. Etna VolcanoAlessandro Bonaccorso0Gilda Currenti1Alan Linde2Selwyn Sacks3Antonino Sicali4Osservatorio Etneo – Istituto Nazionale di Geofisica e Vulcanologia, Catania, ItalyOsservatorio Etneo – Istituto Nazionale di Geofisica e Vulcanologia, Catania, ItalyDepartment of Terrestrial Magnetism, Carnegie Institution, Washington, DC, United StatesDepartment of Terrestrial Magnetism, Carnegie Institution, Washington, DC, United StatesOsservatorio Etneo – Istituto Nazionale di Geofisica e Vulcanologia, Catania, ItalyFor detecting below surface sources of deformation, strain measurements offer a very large advantage (orders of magnitude) in sensitivity over displacement measurements. On active volcanoes an intriguing open challenge is to measure the strain variations caused by the different types of eruptive activity with the highest possible precision in order to obtain advantages on the clear detecting of phenomena, their modeling and understanding. We present the updated main results obtained from the high precision strain recorded by the borehole dilatometer network on Mt. Etna volcano. The instruments, installed from the end of 2011, detected significant changes during different types of eruptive activity: several lava fountains during 2011–2014; two explosive sequences in 2015 and 2016; moderate effusive activity in 2017 and a dike intrusion in 2018. The strain changes provided powerful diagnostic information on the different ongoing processes, and allowed us to add key information on the different eruptive styles and sources. We also highlight how the recorded signals, with the associated modeling and interpretation, provide a powerful contribution to surveillance requirements on an active volcano. This report demonstrates that the borehole dilatometer network represents a useful tool both for the understanding of the volcano processes and for surveillance needs.https://www.frontiersin.org/article/10.3389/feart.2019.00357/fullEtna volcanovolcano monitoringborehole strainmetersvolcano processes detectioneruption modeling
collection DOAJ
language English
format Article
sources DOAJ
author Alessandro Bonaccorso
Gilda Currenti
Alan Linde
Selwyn Sacks
Antonino Sicali
spellingShingle Alessandro Bonaccorso
Gilda Currenti
Alan Linde
Selwyn Sacks
Antonino Sicali
Advances in Understanding Intrusive, Explosive and Effusive Processes as Revealed by the Borehole Dilatometer Network on Mt. Etna Volcano
Frontiers in Earth Science
Etna volcano
volcano monitoring
borehole strainmeters
volcano processes detection
eruption modeling
author_facet Alessandro Bonaccorso
Gilda Currenti
Alan Linde
Selwyn Sacks
Antonino Sicali
author_sort Alessandro Bonaccorso
title Advances in Understanding Intrusive, Explosive and Effusive Processes as Revealed by the Borehole Dilatometer Network on Mt. Etna Volcano
title_short Advances in Understanding Intrusive, Explosive and Effusive Processes as Revealed by the Borehole Dilatometer Network on Mt. Etna Volcano
title_full Advances in Understanding Intrusive, Explosive and Effusive Processes as Revealed by the Borehole Dilatometer Network on Mt. Etna Volcano
title_fullStr Advances in Understanding Intrusive, Explosive and Effusive Processes as Revealed by the Borehole Dilatometer Network on Mt. Etna Volcano
title_full_unstemmed Advances in Understanding Intrusive, Explosive and Effusive Processes as Revealed by the Borehole Dilatometer Network on Mt. Etna Volcano
title_sort advances in understanding intrusive, explosive and effusive processes as revealed by the borehole dilatometer network on mt. etna volcano
publisher Frontiers Media S.A.
series Frontiers in Earth Science
issn 2296-6463
publishDate 2020-01-01
description For detecting below surface sources of deformation, strain measurements offer a very large advantage (orders of magnitude) in sensitivity over displacement measurements. On active volcanoes an intriguing open challenge is to measure the strain variations caused by the different types of eruptive activity with the highest possible precision in order to obtain advantages on the clear detecting of phenomena, their modeling and understanding. We present the updated main results obtained from the high precision strain recorded by the borehole dilatometer network on Mt. Etna volcano. The instruments, installed from the end of 2011, detected significant changes during different types of eruptive activity: several lava fountains during 2011–2014; two explosive sequences in 2015 and 2016; moderate effusive activity in 2017 and a dike intrusion in 2018. The strain changes provided powerful diagnostic information on the different ongoing processes, and allowed us to add key information on the different eruptive styles and sources. We also highlight how the recorded signals, with the associated modeling and interpretation, provide a powerful contribution to surveillance requirements on an active volcano. This report demonstrates that the borehole dilatometer network represents a useful tool both for the understanding of the volcano processes and for surveillance needs.
topic Etna volcano
volcano monitoring
borehole strainmeters
volcano processes detection
eruption modeling
url https://www.frontiersin.org/article/10.3389/feart.2019.00357/full
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