  {"id":138628,"date":"2021-04-07T08:00:51","date_gmt":"2021-04-07T18:00:51","guid":{"rendered":"https:\/\/www.hawaii.edu\/news\/?p=138628"},"modified":"2021-04-07T07:26:00","modified_gmt":"2021-04-07T17:26:00","slug":"measuring-magma-viscosity-early","status":"publish","type":"post","link":"https:\/\/www.hawaii.edu\/news\/2021\/04\/07\/measuring-magma-viscosity-early\/","title":{"rendered":"Measuring magma viscosity early could forecast volcanic eruptions"},"content":{"rendered":"<span class=\"span-reading-time rt-reading-time\" style=\"display: block;\"><span class=\"rt-label rt-prefix\">Reading time: <\/span> <span class=\"rt-time\"> 2<\/span> <span class=\"rt-label rt-postfix\">minutes<\/span><\/span><figure id=\"attachment_138631\" aria-describedby=\"caption-attachment-138631\" style=\"width: 676px\" class=\"wp-caption alignright\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2021\/04\/manoa-soest-kilaeua-eruption-1.jpg\" alt=\"volcano erupting\" width=\"676\" height=\"381\" class=\"size-full wp-image-138631\" srcset=\"https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2021\/04\/manoa-soest-kilaeua-eruption-1.jpg 676w, https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2021\/04\/manoa-soest-kilaeua-eruption-1-300x169.jpg 300w, https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2021\/04\/manoa-soest-kilaeua-eruption-1-130x73.jpg 130w\" sizes=\"auto, (max-width: 676px) 100vw, 676px\" \/><figcaption id=\"caption-attachment-138631\" class=\"wp-caption-text\">K&#299;lauea eruption, 2018. (Photo credit: <abbr>USGS<\/abbr>\/ Brian Shiro)<\/figcaption><\/figure>\n<p>The 2018 K&#299;lauea eruption in <span aria-label=\"Hawaii\">Hawai&#699;i<\/span> provided scientists with an unprecedented opportunity to identify new factors that could help forecast the hazard potential of future eruptions.<\/p>\n<p>A team of researchers, including University of <span aria-label=\"Hawaii\">Hawai&#699;i<\/span> at M&#257;noa <a href=\"https:\/\/www.soest.hawaii.edu\/soestwp\/\">School of Ocean and Earth Science and Technology<\/a> Professor <strong>Bruce Houghton<\/strong>, identified an indicator of magma viscosity that can be measured before an eruption, providing critical information to help understand possible future eruptions. The findings are <a href=\"https:\/\/www.nature.com\/articles\/s41586-021-03400-x\">published in <em>Nature<\/em><\/a>.<\/p>\n<p>&ldquo;The study is very unusual because it falls at the interface between two distinct disciplines in volcanology: seismology and studies of the viscosity (fluidity) of the molten rock,&rdquo; said Houghton.<\/p>\n<h2>Viscous magma linked with powerful explosions<\/h2>\n<figure id=\"attachment_138633\" aria-describedby=\"caption-attachment-138633\" style=\"width: 300px\" class=\"wp-caption alignright\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2021\/04\/manoa-soest-kilauea-eruption-2-300x169.jpg\" alt=\"volcano erupting\" width=\"300\" height=\"169\" class=\"size-medium wp-image-138633\" srcset=\"https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2021\/04\/manoa-soest-kilauea-eruption-2-300x169.jpg 300w, https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2021\/04\/manoa-soest-kilauea-eruption-2-130x73.jpg 130w, https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2021\/04\/manoa-soest-kilauea-eruption-2.jpg 676w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><figcaption id=\"caption-attachment-138633\" class=\"wp-caption-text\">K\u012blauea eruption, 2018. (Photo credit: <abbr>USGS<\/abbr>\/Brian Shiro<\/figcaption><\/figure>\n<p>The properties of the magma inside a volcano affect how an eruption will play out. In particular, the viscosity of this molten rock is a major factor in influencing how hazardous an eruption could be for nearby communities.<\/p>\n<p>Very viscous magmas are linked with more powerful explosions because they can block gas from escaping through vents, allowing pressure to build up inside the volcano\u2019s plumbing system. On the other hand, extrusion of more viscous magma results in slower-moving lava flows.<\/p>\n<p>&ldquo;But magma viscosity is usually only quantified well after an eruption, not in advance,&rdquo; explained Diana Roman, lead author of the study and volcanologist at <a href=\"https:\/\/epl.carnegiescience.edu\/\">Carnegie Institution for Science<\/a>. &ldquo;So, we are always trying to identify early indications of magma viscosity that could help forecast a volcano\u2019s eruption style.&rdquo;<\/p>\n<h2>K&#299;lauea eruption provides wealth of data<\/h2>\n<p>The 2018 event included the first eruptive activity in K&#299;lauea\u2019s lower East Rift Zone since 1960. The first of 24 fissures opened in early May, and the eruption continued for three months. This situation provided unprecedented access to information for the team of researchers.<\/p>\n<p>The event provided a wealth of simultaneous data about the behavior of both high- and low-viscosity magma, as well as about the pre-eruption stresses in the solid rock underlying K&#299;lauea.<\/p>\n<figure id=\"attachment_138632\" aria-describedby=\"caption-attachment-138632\" style=\"width: 300px\" class=\"wp-caption alignright\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2021\/04\/manoa-soest-kilauea-eruption-3-300x169.jpg\" alt=\"volcano erupting by houses\" width=\"300\" height=\"169\" class=\"size-medium wp-image-138632\" srcset=\"https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2021\/04\/manoa-soest-kilauea-eruption-3-300x169.jpg 300w, https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2021\/04\/manoa-soest-kilauea-eruption-3-130x73.jpg 130w, https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2021\/04\/manoa-soest-kilauea-eruption-3.jpg 676w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><figcaption id=\"caption-attachment-138632\" class=\"wp-caption-text\">K&#299;lauea eruption, 2018. (Photo credit: <abbr>USGS<\/abbr>\/ Brian Shiro)<\/figcaption><\/figure>\n<p>Tectonic and volcanic activity cause fractures, called faults, to form in the rock that makes up Earth\u2019s crust. When geologic stresses cause these faults to move against each other, geoscientists measure the <abbr title=\"three dimension\">3-D<\/abbr> orientation and movement of the faults using seismic instruments.<\/p>\n<p>By studying what happened in K&#299;lauea\u2019s lower East Rift Zone in 2018, Roman and her colleagues determined that the direction of the fault movements in the lower East Rift Zone before and during the volcanic eruption could be used to estimate the viscosity of rising magma during periods of precursory unrest.<\/p>\n<p>&ldquo;We were able to show that with robust monitoring we can relate pressure and stress in a volcano\u2019s plumbing system to the underground movement of more viscous magma,&rdquo; Roman explained. &ldquo;This will enable monitoring experts to better anticipate the eruption behavior of volcanoes like K&#299;lauea and to tailor response strategies in advance.&rdquo;<\/p>\n<p>This research is an example of <abbr>¶«¾«Ó°Òµ<\/abbr> M&#257;noa\u2019s goal of <a href=\"https:\/\/manoa.hawaii.edu\/wp\/wp-content\/uploads\/2020\/12\/manoa-2025-strategic-plan.pdf#page=25\">Excellence in Research: Advancing the Research and Creative Work Enterprise<\/a> (<span class=\"small-text\"><abbr title=\"Portable Document Format\">PDF<\/abbr><\/span>), one of four goals identified in the <a href=\"https:\/\/manoa.hawaii.edu\/wp\/wp-content\/uploads\/2020\/12\/manoa-2025-strategic-plan.pdf\">2015\u201325 Strategic Plan<\/a> (<span class=\"small-text\"><abbr title=\"Portable Document Format\">PDF<\/abbr><\/span>), updated in December 2020.<\/p>\n<p><em>&#8211;By Marcie Grabowski<\/em><\/p>\n","protected":false},"excerpt":{"rendered":"<p>A team of researchers identified an indicator of magma viscosity that can be measured before an eruption, providing information to help understand future eruptions.<\/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":[1313,1467,1363,92,9,108,176],"class_list":["post-138628","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-research","tag-kilauea-eruption-2018","tag-manoa-excellence-in-research","tag-manoa-research","tag-school-of-ocean-and-earth-science-and-technology","tag-uh-manoa","tag-volcano","tag-volcanology","entry","has-media"],"aioseo_notices":[],"jetpack_featured_media_url":"","_links":{"self":[{"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/posts\/138628","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/users\/16"}],"replies":[{"embeddable":true,"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/comments?post=138628"}],"version-history":[{"count":10,"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/posts\/138628\/revisions"}],"predecessor-version":[{"id":138686,"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/posts\/138628\/revisions\/138686"}],"wp:attachment":[{"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/media?parent=138628"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/categories?post=138628"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/tags?post=138628"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}