Volcanic eruptions are triggered in static dilatational strain fields generated by large earthquakes

Abstract Although data catalog analyses have confirmed that volcanic eruptions are triggered by large earthquakes, the triggering mechanism has been under discussion for many decades. In the present study, recent earthquake and volcanic data from the past 35–55 years were analyzed, and it was demons...

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Main Author: Takeshi Nishimura
Format: Article
Language:English
Published: Nature Portfolio 2021-08-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-021-96756-z
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author Takeshi Nishimura
author_facet Takeshi Nishimura
author_sort Takeshi Nishimura
collection DOAJ
description Abstract Although data catalog analyses have confirmed that volcanic eruptions are triggered by large earthquakes, the triggering mechanism has been under discussion for many decades. In the present study, recent earthquake and volcanic data from the past 35–55 years were analyzed, and it was demonstrated for the first time that the likelihood of new eruptions increases two to three times in the 5–10 years following large earthquakes for volcanoes where the generated static dilatational strain exceeds 0.5 µ, which may, for example, activate gas bubble growth and thereby generate a buoyant force in the magma. In contrast, the eruption likelihood does not increase for volcanoes that are subjected to strong ground motion alone, which affect the magma system and volcanic edifice. These results indicate that we can evaluate the likelihood of triggered eruptions and prepare for new eruptions when a large earthquake occurs.
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spelling doaj.art-f61bbf82281e4163befb4050a3ed56912022-12-21T21:47:38ZengNature PortfolioScientific Reports2045-23222021-08-011111910.1038/s41598-021-96756-zVolcanic eruptions are triggered in static dilatational strain fields generated by large earthquakesTakeshi Nishimura0Department of Geophysics, Graduate School of Science, Tohoku UniversityAbstract Although data catalog analyses have confirmed that volcanic eruptions are triggered by large earthquakes, the triggering mechanism has been under discussion for many decades. In the present study, recent earthquake and volcanic data from the past 35–55 years were analyzed, and it was demonstrated for the first time that the likelihood of new eruptions increases two to three times in the 5–10 years following large earthquakes for volcanoes where the generated static dilatational strain exceeds 0.5 µ, which may, for example, activate gas bubble growth and thereby generate a buoyant force in the magma. In contrast, the eruption likelihood does not increase for volcanoes that are subjected to strong ground motion alone, which affect the magma system and volcanic edifice. These results indicate that we can evaluate the likelihood of triggered eruptions and prepare for new eruptions when a large earthquake occurs.https://doi.org/10.1038/s41598-021-96756-z
spellingShingle Takeshi Nishimura
Volcanic eruptions are triggered in static dilatational strain fields generated by large earthquakes
Scientific Reports
title Volcanic eruptions are triggered in static dilatational strain fields generated by large earthquakes
title_full Volcanic eruptions are triggered in static dilatational strain fields generated by large earthquakes
title_fullStr Volcanic eruptions are triggered in static dilatational strain fields generated by large earthquakes
title_full_unstemmed Volcanic eruptions are triggered in static dilatational strain fields generated by large earthquakes
title_short Volcanic eruptions are triggered in static dilatational strain fields generated by large earthquakes
title_sort volcanic eruptions are triggered in static dilatational strain fields generated by large earthquakes
url https://doi.org/10.1038/s41598-021-96756-z
work_keys_str_mv AT takeshinishimura volcaniceruptionsaretriggeredinstaticdilatationalstrainfieldsgeneratedbylargeearthquakes