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"USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "Article", "additionalType": "Journal Article", "name": "Seismic and geodetic progression of the 2018 summit caldera collapse of K\u012blauea Volcano", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70209463", "url": "https://pubs.usgs.gov/publication/70209463" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70209463 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.1016/j.epsl.2020.116250", "url": "https://doi.org/10.1016/j.epsl.2020.116250" } ], "journal": { "@type": "Periodical", "name": "Earth and Planetary Science Letters", "volumeNumber": "540", "issueNumber": null }, "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Earth and Planetary Science Letters" } ], "datePublished": "2020", "dateModified": "2020-04-09", "abstract": "The 2018 eruption of K\u012blauea volcano, Hawai\u02bbi, resulted in a major collapse of the summit caldera along with an effusive eruption in the lower East Rift Zone. The caldera collapse comprised 62 highly similar collapse cycles of strong ground deformation and earthquake swarms that ended with a magnitude 5 collapse event and one partial cycle that did not end with a collapse event. We analyzed geodetic and seismic data to better understand how the caldera collapse progressed over 3 months of activity, focusing on the cyclical activity. We identified 3 main phases of collapse: initial ring-fault activation and small explosions (Phase 1), an eastward shift in activity and freeing of the central piston (Phase 2), and a recoupling of the piston to the reservoir followed by relatively steady behavior until the eruption\u2019s end (Phase 3). Additionally, we observed geodetic evidence of tangential motion from the localization of the main ring fault (Phase 2) and the formation of a major peripheral ring fault on the eastern side of the collapse caldera during Phase 3. Both geodetic and seismic parameters suggest that the collapse may have had an eastward-component of motion after the ring fault system had formed. The cyclical seismic and geodetic parameters show no obvious signs that the collapse was coming to an end, with the only notable change being a significant increase in the ratio of cyclical displacement to co-collapse displacement observed during the last complete cycle on GNSS stations outside the caldera region.", "description": "116250", "publisher": { "@type": "Organization", "name": "Elsevier" }, "author": [ { "@type": "Person", "name": "Tepp, Gabrielle", "givenName": "Gabrielle", "familyName": "Tepp", "identifier": { "@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0001-5388-5138", "url": "https://orcid.org/0000-0001-5388-5138" }, "affiliation": [ { "@type": "Organization", "name": "Volcano Science Center", "url": "https://www.usgs.gov/centers/volcano-science-center" } ] }, { "@type": "Person", "name": "Hotovec-Ellis, Alicia J.", "givenName": "Alicia J.", "familyName": "Hotovec-Ellis", "identifier": { "@type": "PropertyValue", "propertyID": "ORCID", "value": 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