{"id":7196,"date":"2017-11-19T15:22:26","date_gmt":"2017-11-19T15:22:26","guid":{"rendered":"http:\/\/icelandgeology.net\/?p=7196"},"modified":"2017-11-19T15:22:26","modified_gmt":"2017-11-19T15:22:26","slug":"update-on-bardarbunga-volcano-and-high-conductivity-in-jokulsa-a-fjollum-glacier-river","status":"publish","type":"post","link":"https:\/\/icelandgeology.net\/?p=7196","title":{"rendered":"Update on B\u00e1r\u00f0arbunga volcano and high conductivity in J\u00f6kuls\u00e1 \u00e1 Fj\u00f6llum glacier river"},"content":{"rendered":"<p>Conductivity remains rather high in J\u00f6kuls\u00e1 \u00e1 Fj\u00f6llum as it has been doing since before 14th of November. The source remains at <a href=\"https:\/\/volcano.si.edu\/volcano.cfm?vn=373030\" rel=\"noopener\" target=\"_blank\">B\u00e1r\u00f0arbunga<\/a> volcano. The conductivity has slowly been getting lower since it peaked before 14th of November (I&#8217;m not sure when the peak was). Yesterday (18-November) I did notice the news a little discussion about B\u00e1r\u00f0arbunga volcano. It was stated that at least one cauldron in the glacier above B\u00e1r\u00f0arbunga volcano is so hot that is makes a steam trough the glacier. I have also not hear any other details about the reason why conductivity remains rather high in J\u00f6kuls \u00e1 Fj\u00f6llum glacier river from the observations yesterday.<\/p>\n<p>The steaming hydrothermal systems means there is a considerable energy in B\u00e1r\u00f0arbunga volcano system at the moment. This also invites the risk that next eruption cycle in B\u00e1r\u00f0arbunga volcano is going to large. This also increases the risk of small eruptions that are also hard to detect and might not break the glacier surface, unless they happen close to one of the new hydrothermal areas.<\/p>\n<p><a href=\"http:\/\/icelandgeology.net\/wp-content\/uploads\/2017\/11\/171119_1515.png\"><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/icelandgeology.net\/wp-content\/uploads\/2017\/11\/171119_1515.png\" alt=\"\" width=\"540\" height=\"596\" class=\"aligncenter size-full wp-image-7197\" srcset=\"https:\/\/icelandgeology.net\/wp-content\/uploads\/2017\/11\/171119_1515.png 540w, https:\/\/icelandgeology.net\/wp-content\/uploads\/2017\/11\/171119_1515-272x300.png 272w\" sizes=\"auto, (max-width: 540px) 100vw, 540px\" \/><\/a><br \/>\nEarthquake activity in B\u00e1r\u00f0arbunga volcano in the last 48 hours. <em>Copyright of this image belongs to Icelandic Met Office.<\/em><\/p>\n<p>When next eruption cycle starts in B\u00e1r\u00f0arbunga volcano is impossible to know.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Conductivity remains rather high in J\u00f6kuls\u00e1 \u00e1 Fj\u00f6llum as it has been doing since before 14th of November. The source remains at B\u00e1r\u00f0arbunga volcano. The conductivity has slowly been getting lower since it peaked before 14th of November (I&#8217;m not sure when the peak was). Yesterday (18-November) I did notice the news a little discussion &hellip; <\/p>\n<p class=\"link-more\"><a href=\"https:\/\/icelandgeology.net\/?p=7196\" class=\"more-link\">Continue reading<span class=\"screen-reader-text\"> &#8220;Update on B\u00e1r\u00f0arbunga volcano and high conductivity in J\u00f6kuls\u00e1 \u00e1 Fj\u00f6llum glacier river&#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":[7,10,64,40,32],"tags":[],"class_list":["post-7196","post","type-post","status-publish","format-standard","hentry","category-bararbunga","category-earthquakes","category-magma","category-monitoring","category-volcano"],"_links":{"self":[{"href":"https:\/\/icelandgeology.net\/index.php?rest_route=\/wp\/v2\/posts\/7196","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=7196"}],"version-history":[{"count":1,"href":"https:\/\/icelandgeology.net\/index.php?rest_route=\/wp\/v2\/posts\/7196\/revisions"}],"predecessor-version":[{"id":7198,"href":"https:\/\/icelandgeology.net\/index.php?rest_route=\/wp\/v2\/posts\/7196\/revisions\/7198"}],"wp:attachment":[{"href":"https:\/\/icelandgeology.net\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=7196"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/icelandgeology.net\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=7196"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/icelandgeology.net\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=7196"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}