{"id":7272,"date":"2026-07-17T18:16:33","date_gmt":"2026-07-17T09:16:33","guid":{"rendered":"https:\/\/www.eri.u-tokyo.ac.jp\/en\/?p=7272"},"modified":"2026-08-17T22:10:36","modified_gmt":"2026-08-17T13:10:36","slug":"friday-seminar-28-august-2026-kyle-anderson-u-s-geologocal-survey","status":"publish","type":"post","link":"https:\/\/www.eri.u-tokyo.ac.jp\/en\/seminars\/7272\/","title":{"rendered":"Friday Seminar (28 August 2026) Kyle Anderson (U.S. Geologocal Survey)"},"content":{"rendered":"<p>Title:<\/p>\n<p>The 2018 eruption and caldera collapse at Kilauea volcano<\/p>\n<p>&nbsp;<\/p>\n<p>Abstract:<\/p>\n<p>The 2018 eruption of Kilauea volcano (Hawai\u2018i) was its most impactful in centuries, involving an outpouring of more than one cubic kilometer of basalt, a magnitude 7 flank earthquake, and the volcano\u2019s largest summit collapse since at least the nineteenth century. Observations have yielded unprecedented insights into basaltic caldera collapses, the dynamics of large caldera-rift eruptions, the geometry of a shallow magma storage-transport system and its interaction with rift zone tectonics, mechanisms of basaltic tephra-producing explosions, and the dynamics of fissure eruptions and high-volume lava flows. I will summarize eruptive activity and describe how magma flow to a low-elevation vent triggered quasi-periodic step-like collapse of the summit caldera, which pressurized the magma system and sustained the eruption. I will also show evidence that Kilauea\u2019s magmatic-tectonic system is tightly interconnected over tens of kilometers, and that magma is stored in diverse locations, volumes, and compositions beneath the volcano&#8217;s summit and East Rift Zone. I will also discuss parallels with other basaltic caldera-forming eruptions, including at Miyakejima. Finally I will highlight some outstanding questions which may motivate new studies into this remarkable eruption.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Title: The 2018 eruption and caldera collapse at Kilauea volcano &nbsp; Abstract: The 2018 eruption of Kilauea &hellip; <a href=\"https:\/\/www.eri.u-tokyo.ac.jp\/en\/seminars\/7272\/\" class=\"more-link\">Continue reading<span class=\"screen-reader-text\"> &#8220;Friday Seminar (28 August 2026) Kyle Anderson (U.S. Geologocal Survey)&#8221;<\/span><\/a><\/p>\n","protected":false},"author":8,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[36],"tags":[],"class_list":["post-7272","post","type-post","status-publish","format-standard","hentry","category-seminars"],"_links":{"self":[{"href":"https:\/\/www.eri.u-tokyo.ac.jp\/en\/wp-json\/wp\/v2\/posts\/7272"}],"collection":[{"href":"https:\/\/www.eri.u-tokyo.ac.jp\/en\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.eri.u-tokyo.ac.jp\/en\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.eri.u-tokyo.ac.jp\/en\/wp-json\/wp\/v2\/users\/8"}],"replies":[{"embeddable":true,"href":"https:\/\/www.eri.u-tokyo.ac.jp\/en\/wp-json\/wp\/v2\/comments?post=7272"}],"version-history":[{"count":2,"href":"https:\/\/www.eri.u-tokyo.ac.jp\/en\/wp-json\/wp\/v2\/posts\/7272\/revisions"}],"predecessor-version":[{"id":7302,"href":"https:\/\/www.eri.u-tokyo.ac.jp\/en\/wp-json\/wp\/v2\/posts\/7272\/revisions\/7302"}],"wp:attachment":[{"href":"https:\/\/www.eri.u-tokyo.ac.jp\/en\/wp-json\/wp\/v2\/media?parent=7272"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.eri.u-tokyo.ac.jp\/en\/wp-json\/wp\/v2\/categories?post=7272"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.eri.u-tokyo.ac.jp\/en\/wp-json\/wp\/v2\/tags?post=7272"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}