{"id":131182,"date":"2020-11-24T09:56:39","date_gmt":"2020-11-24T19:56:39","guid":{"rendered":"https:\/\/www.hawaii.edu\/news\/?p=131182"},"modified":"2020-11-24T09:56:39","modified_gmt":"2020-11-24T19:56:39","slug":"kilauea-eruption-triggered","status":"publish","type":"post","link":"https:\/\/www.hawaii.edu\/news\/2020\/11\/24\/kilauea-eruption-triggered\/","title":{"rendered":"K\u012blauea eruption triggered by pressure built over a decade"},"content":{"rendered":"Reading time: <\/span> 2<\/span> minutes<\/span><\/span>
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Fissure 8 lava fountain and lava channel during 2018 Kīlauea eruption. (Photo credit: Bruce Houghton)<\/figcaption><\/figure>\n

The 2018 eruption of Kīlauea Volcano was one of the largest volcanic events in Hawaiʻi<\/span> in 200 years. This eruption was triggered by a relatively small and rapid change at the volcano after a decade-long build-up of pressure in the upper parts of the volcano, according to a recent study published in Nature Communications<\/em><\/a> by Earth science researchers from the University of Hawaiʻi<\/span> at Mānoa and U.S. Geological Survey (USGS<\/abbr>).<\/p>\n

Using USGS<\/abbr> Hawaiian Volcanoes Observatory<\/a> (HVO<\/abbr>) data from before and during the 2018 eruptions at the summit and flank, the research team reconstructed the geologic events.<\/p>\n

“The data suggest that a backup in the magma plumbing system at the long-lived Puʻu<\/span> ʻO\u0304ʻo\u0304<\/span> eruption site caused widespread pressurization in the volcano, driving magma into the lower flank,” said Matthew Patrick, research geologist at the USGS<\/abbr> HVO<\/abbr> and lead author of the study.<\/p>\n

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Fissure 8 lava fountain in Leilani Estates during the 2018 Kīlauea eruption. (Photo credit: Bruce Houghton)<\/figcaption><\/figure>\n

The eruption evolved, and its impact expanded, as a sequence of cascading events allowed relatively minor changes at Puʻu<\/span> ʻO\u0304ʻo\u0304<\/span> to cause major destruction and historic changes across the volcano.<\/p>\n

Challenges of forecasting volcanic hazards<\/h2>\n

A cascading series of events of this type was not considered the most likely outcome in the weeks prior to the onset of the eruption.<\/p>\n

“This form of tunnel vision, which gives less attention to the least likely outcomes, is a bias that can be overcome by considering the broader, longer history of the volcano,” said Bruce Houghton<\/strong>, the Hawaiʻi<\/span> state volcanologist, an Earth sciences professor at the 糖心视频<\/abbr> Mānoa School of Ocean and Earth Science and Technology<\/a> (SOEST<\/abbr>) and study co-author. “For Kīlauea, this consists of widening the scope to consider the types of behavior seen in the first half of the 20th century and perhaps earlier.”<\/p>\n

“Our study demonstrates that eruption forecasting can be inherently challenging in scenarios where volcanoes prime slowly and trigger due to a small event, as the processes that build to eruption may be hard to detect and are easy to overlook on the scale of the entire volcano,” said Patrick. “It is also a cautionary tale against over-reliance on recent activity as a guide for future eruptions.”<\/p>\n

For more see SOEST<\/abbr>\u2019s website<\/a>.<\/p>\n

–By Marcie Grabowski<\/em><\/p>\n","protected":false},"excerpt":{"rendered":"

This eruption was triggered by a relatively small and rapid change after a decade-long build up of pressure in the upper parts of the volcano.<\/p>\n","protected":false},"author":16,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[30],"tags":[1187,1363,158,92,9,108],"class_list":["post-131182","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-research","tag-earth-science","tag-manoa-research","tag-publication","tag-school-of-ocean-and-earth-science-and-technology","tag-uh-manoa","tag-volcano","entry","has-media"],"aioseo_notices":[],"aioseo_head":"\n\t\t\n\t\n\t\n\t\n\t\n\t\n\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t