Editorial: Seismicity in Volcanic Areas

Keir, Derek, De Siena, Luca, Doubre, Cécile, Johnson, Jessica H. ORCID: https://orcid.org/0000-0003-3628-6402, Maccaferri, Francesco and Passarelli, Luigi (2021) Editorial: Seismicity in Volcanic Areas. Frontiers in Earth Science, 9. ISSN 2296-6463

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Seismic activity (e.g., earthquakes, tremors) beneath volcanic areas is primarily caused by the dynamic interaction of molten rock and hydrothermal fluids with the solid host rock, by fracturing and fragmentation of the magma itself, and by tectonic processes interacting with the volcano. In addition, near-surface phenomena such as explosions and rockfalls at a volcanic edifice also produce seismic events. At volcano observatories globally, the real-time monitoring of the spatial and temporal patterns of seismic events is an essential geophysical tool to quantify the state of unrest, and forecast eruptions successfully. Seismic waveforms, earthquake catalogues and earthquake ray-path properties commonly supplement this tool to model the complex processes responsible for the earthquakes quantitatively, and to image subsurface magmatic and tectonic structures. Independent constraints provided by other disciplines such as geodesy and structural geology also significantly help scientists to understand the volcanic processes. Recent advances in earthquake recording technology, computing power and algorithms in artificial intelligence, allow processing and interpretation of large and complex multi-parametric datasets and scenarios.

Item Type: Article
Faculty \ School: Faculty of Science > School of Environmental Sciences
UEA Research Groups: Faculty of Science > Research Groups > Geosciences
Depositing User: LivePure Connector
Date Deposited: 12 Dec 2023 01:21
Last Modified: 12 Dec 2023 01:21
URI: https://ueaeprints.uea.ac.uk/id/eprint/93965
DOI: 10.3389/feart.2021.829460

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