{"id":9043,"date":"2021-03-08T21:21:35","date_gmt":"2021-03-08T21:21:35","guid":{"rendered":"https:\/\/icelandgeology.net\/?p=9043"},"modified":"2021-03-08T21:50:00","modified_gmt":"2021-03-08T21:50:00","slug":"new-information-about-the-situation-in-fagradalsfjall-volcano","status":"publish","type":"post","link":"https:\/\/icelandgeology.net\/?p=9043","title":{"rendered":"New information about the situation in Fagradalsfjall volcano"},"content":{"rendered":"<p>This is a short article about the new information published today (8-March-2021) by <a href=\"https:\/\/en.vedur.is\" rel=\"noopener\" target=\"_blank\">Icelandic Met Office<\/a> and Department of <a href=\"https:\/\/www.almannavarnir.is\/english\/\" rel=\"noopener\" target=\"_blank\">Civil Protection and Emergency Management<\/a>.<\/p>\n<p>New measurements of the situation in <a href=\"https:\/\/volcano.si.edu\/volcano.cfm?vn=371800\" rel=\"noopener\" target=\"_blank\">Fagradalsfjall<\/a> volcano show that the dyke intrusion continues to grow and as at its shallowest point at 1 km depth. Possible eruption is expected at the south end of the dyke intrusion (closest to Fagradalsfjall mountain). Earthquakes are going to happen at the south-west end of the dyke and north-east of the dyke because of the inflation the magma is creating in the area.<\/p>\n<figure id=\"attachment_9044\" aria-describedby=\"caption-attachment-9044\" style=\"width: 525px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/icelandgeology.net\/wp-content\/uploads\/2021\/03\/earthquake-zones-Fagradalsfjall-volcano.jpg\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/icelandgeology.net\/wp-content\/uploads\/2021\/03\/earthquake-zones-Fagradalsfjall-volcano-1024x576.jpg\" alt=\"The dyke shown with dotted line and circle shows the most effective area. Gray areas at both ends shows earthquake effected area\" width=\"525\" height=\"295\" class=\"size-large wp-image-9044\" srcset=\"https:\/\/icelandgeology.net\/wp-content\/uploads\/2021\/03\/earthquake-zones-Fagradalsfjall-volcano-1024x576.jpg 1024w, https:\/\/icelandgeology.net\/wp-content\/uploads\/2021\/03\/earthquake-zones-Fagradalsfjall-volcano-300x169.jpg 300w, https:\/\/icelandgeology.net\/wp-content\/uploads\/2021\/03\/earthquake-zones-Fagradalsfjall-volcano-768x432.jpg 768w, https:\/\/icelandgeology.net\/wp-content\/uploads\/2021\/03\/earthquake-zones-Fagradalsfjall-volcano-1536x864.jpg 1536w, https:\/\/icelandgeology.net\/wp-content\/uploads\/2021\/03\/earthquake-zones-Fagradalsfjall-volcano.jpg 1640w\" sizes=\"auto, (max-width: 525px) 100vw, 525px\" \/><\/a><figcaption id=\"caption-attachment-9044\" class=\"wp-caption-text\">The earthquake areas at the ends of the dyke intrusion, shown in gray areas on this map. The dyke is shown within the line with dot lines. Copyright of this image belongs to Icelandic Met Office.<\/figcaption><\/figure>\n<p>There are going to be quiet times between high period of activity according to the news about this activity. There is also ongoing risk of a earthquake with magnitude of Mw6,5 in Brennisteinsfj\u00f6ll volcano and according to Icelandic Met Office that risk has not been reduced in recent days. Outside of the Fagradalsfjall volcano magma dyke, no magma movement has been detected in Reykjanes (Svartsengi?) volcano and in Kr\u00fdsuv\u00edk volcano.<\/p>\n<p><strong>Sources (Icelandic)<\/strong><\/p>\n<p><a href=\"https:\/\/www.almannavarnir.is\/frettir\/afram-ma-buast-vid-ad-virknin-a-reykjanesskaga-verdi-kaflaskipt\/\" rel=\"noopener\" target=\"_blank\">\u00c1fram m\u00e1 b\u00faast vi\u00f0 a\u00f0 virknin \u00e1 Reykjanesskaga ver\u00f0i kaflaskipt<\/a> (Iceland, English, Polish, Almannavarnir.is)<br \/>\n<a href=\"https:\/\/www.ruv.is\/frett\/2021\/03\/08\/kvikan-er-a-kilometra-dypi\" rel=\"noopener\" target=\"_blank\">Kvikan er \u00e1 k\u00edl\u00f3metra d\u00fdpi<\/a> (R\u00fav.is, Icelandic)<\/p>\n","protected":false},"excerpt":{"rendered":"<p>This is a short article about the new information published today (8-March-2021) by Icelandic Met Office and Department of Civil Protection and Emergency Management. New measurements of the situation in Fagradalsfjall volcano show that the dyke intrusion continues to grow and as at its shallowest point at 1 km depth. Possible eruption is expected at &hellip; <\/p>\n<p class=\"link-more\"><a href=\"https:\/\/icelandgeology.net\/?p=9043\" class=\"more-link\">Continue reading<span class=\"screen-reader-text\"> &#8220;New information about the situation in Fagradalsfjall volcano&#8221;<\/span><\/a><\/p>\n","protected":false},"author":2,"featured_media":0,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[149,24,10,204,71,17,89,9,19,64,40,42,207,57,32],"tags":[],"class_list":["post-9043","post","type-post","status-publish","format-standard","hentry","category-breinnisteinsfjoll","category-dyke-intrusions","category-earthquakes","category-fagradalsfjall","category-fissures","category-gps-data","category-gps-monitoring","category-harmonic-tremors","category-inflation","category-magma","category-monitoring","category-reykjanes","category-reykjanes-peninsula","category-swarm","category-volcano"],"_links":{"self":[{"href":"https:\/\/icelandgeology.net\/index.php?rest_route=\/wp\/v2\/posts\/9043","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/icelandgeology.net\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/icelandgeology.net\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/icelandgeology.net\/index.php?rest_route=\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/icelandgeology.net\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=9043"}],"version-history":[{"count":3,"href":"https:\/\/icelandgeology.net\/index.php?rest_route=\/wp\/v2\/posts\/9043\/revisions"}],"predecessor-version":[{"id":9047,"href":"https:\/\/icelandgeology.net\/index.php?rest_route=\/wp\/v2\/posts\/9043\/revisions\/9047"}],"wp:attachment":[{"href":"https:\/\/icelandgeology.net\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=9043"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/icelandgeology.net\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=9043"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/icelandgeology.net\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=9043"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}