{"id":5718,"date":"2015-06-29T23:27:07","date_gmt":"2015-06-29T23:27:07","guid":{"rendered":"http:\/\/icelandgeology.net\/?p=5718"},"modified":"2015-06-30T00:04:53","modified_gmt":"2015-06-30T00:04:53","slug":"deep-earthquakes-in-bardarbunga-and-tungafellsjokull-volcanoes","status":"publish","type":"post","link":"https:\/\/icelandgeology.net\/?p=5718","title":{"rendered":"Deep earthquakes in B\u00e1r\u00f0arbunga and Tungnafellsj\u00f6kull volcanoes"},"content":{"rendered":"<p>Even if the eruption in Holuhraun and B\u00e1r\u00f0arbunga volcano is over, there is no shortage of activity in <a href=\"http:\/\/volcano.si.edu\/volcano.cfm?vn=373030\" target=\"_blank\">B\u00e1r\u00f0arbunga<\/a> volcano. With deepest earthquake in past 48 hours having the depth of 28,6 km and earthquakes don&#8217;t get a lot deeper than this in B\u00e1r\u00f0arbunga volcano. At this depth earthquake activity happens due to magma movements rather than tectonic stresses.<\/p>\n<p><a href=\"http:\/\/icelandgeology.net\/wp-content\/uploads\/2015\/06\/150629_1615.png\"><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/icelandgeology.net\/wp-content\/uploads\/2015\/06\/150629_1615.png\" alt=\"150629_1615\" width=\"540\" height=\"596\" class=\"aligncenter size-full wp-image-5719\" srcset=\"https:\/\/icelandgeology.net\/wp-content\/uploads\/2015\/06\/150629_1615.png 540w, https:\/\/icelandgeology.net\/wp-content\/uploads\/2015\/06\/150629_1615-272x300.png 272w\" sizes=\"auto, (max-width: 540px) 100vw, 540px\" \/><\/a><br \/>\nEarthquake activity in B\u00e1r\u00f0arbunga volcano (red dots). <em>Copyright of this image belongs to Iceland Meteorological Office.<\/em><br \/>\n<strong><br \/>\nEarthquake activity in Tungnafellsj\u00f6kull volcano<\/strong><\/p>\n<p>Since the end of the eruption and any major activity in B\u00e1r\u00f0arbunga volcano. Earthquake activity in <a href=\"http:\/\/www.volcano.si.edu\/volcano.cfm?vn=373040\" target=\"_blank\">Tungafellsj\u00f6kull<\/a> volcano has not stopped as expected. The earthquake activity continues at low levels and at great depth. With deepest earthquake in last 48 hours at 26,2 km.<\/p>\n<p><a href=\"http:\/\/icelandgeology.net\/wp-content\/uploads\/2015\/06\/150628_1925.png\"><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/icelandgeology.net\/wp-content\/uploads\/2015\/06\/150628_1925.png\" alt=\"150628_1925\" width=\"540\" height=\"596\" class=\"aligncenter size-full wp-image-5720\" srcset=\"https:\/\/icelandgeology.net\/wp-content\/uploads\/2015\/06\/150628_1925.png 540w, https:\/\/icelandgeology.net\/wp-content\/uploads\/2015\/06\/150628_1925-272x300.png 272w\" sizes=\"auto, (max-width: 540px) 100vw, 540px\" \/><\/a><br \/>\nEarthquake activity in Tungnafellsj\u00f6kull volcano (yellow \/ orange dots). <em>Copyright of this image belongs to Iceland Meteorological Office.<\/em><\/p>\n<p>It is unclear what is going on in Tungnafellsj\u00f6kull volcano, it is clear that dyke intrusion is taking place at depth, if and when that might result in a eruption is not clear at this moment. This might lead to an eruption or it might not. It is impossible to know at this moment since Tungnafellsj\u00f6kull volcano has no recorded or documented history of volcano eruptions in historical times.<\/p>\n<p><strong>Donations:<\/strong> Please remember to support my work with donations or by using Amazon. Thanks for the support. \ud83d\ude42<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Even if the eruption in Holuhraun and B\u00e1r\u00f0arbunga volcano is over, there is no shortage of activity in B\u00e1r\u00f0arbunga volcano. With deepest earthquake in past 48 hours having the depth of 28,6 km and earthquakes don&#8217;t get a lot deeper than this in B\u00e1r\u00f0arbunga volcano. At this depth earthquake activity happens due to magma movements &hellip; <\/p>\n<p class=\"link-more\"><a href=\"https:\/\/icelandgeology.net\/?p=5718\" class=\"more-link\">Continue reading<span class=\"screen-reader-text\"> &#8220;Deep earthquakes in B\u00e1r\u00f0arbunga and Tungnafellsj\u00f6kull volcanoes&#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":[7,24,10,64,40,140,32],"tags":[],"class_list":["post-5718","post","type-post","status-publish","format-standard","hentry","category-bararbunga","category-dyke-intrusions","category-earthquakes","category-magma","category-monitoring","category-tungnafellsjokull","category-volcano"],"_links":{"self":[{"href":"https:\/\/icelandgeology.net\/index.php?rest_route=\/wp\/v2\/posts\/5718","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=5718"}],"version-history":[{"count":3,"href":"https:\/\/icelandgeology.net\/index.php?rest_route=\/wp\/v2\/posts\/5718\/revisions"}],"predecessor-version":[{"id":5723,"href":"https:\/\/icelandgeology.net\/index.php?rest_route=\/wp\/v2\/posts\/5718\/revisions\/5723"}],"wp:attachment":[{"href":"https:\/\/icelandgeology.net\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=5718"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/icelandgeology.net\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=5718"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/icelandgeology.net\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=5718"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}