Seismo-acoustic characterisation of the 2018 Ambae (Manaro Voui) eruption, Vanuatu

A new episode of unrest and phreatic/phreatomagmatic/magmatic eruptions occurred at Ambae volcano, Vanuatu, in 2017–2018. We installed a multi-station seismo-acoustic network consisting of seven 3-component broadband seismic stations and four 3-element (26–62 m maximum inter-element separation) infr...

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Veröffentlicht in:Bulletin of volcanology 2021-09, Vol.83 (9), Article 60
Hauptverfasser: Park, Iseul, Jolly, Arthur, Matoza, Robin S., Kennedy, Ben, Kilgour, Geoff, Johnson, Richard, Garaebiti, Esline, Cevuard, Sandrine
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Sprache:eng
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Zusammenfassung:A new episode of unrest and phreatic/phreatomagmatic/magmatic eruptions occurred at Ambae volcano, Vanuatu, in 2017–2018. We installed a multi-station seismo-acoustic network consisting of seven 3-component broadband seismic stations and four 3-element (26–62 m maximum inter-element separation) infrasound arrays during the last phase of the 2018 eruption episode, capturing at least six reported major explosions towards the end of the eruption episode. The observed volcanic seismic signals are generally in the passband 0.5–10 Hz during the eruptive activity, but the corresponding acoustic signals have relatively low frequencies (
ISSN:0258-8900
1432-0819
DOI:10.1007/s00445-021-01474-z