{"id":5237,"date":"2014-11-10T22:52:10","date_gmt":"2014-11-10T21:52:10","guid":{"rendered":"http:\/\/icelandgeology.net\/?p=5237"},"modified":"2014-11-10T22:52:33","modified_gmt":"2014-11-10T21:52:33","slug":"bardarbunga-volcano-update-monday-10-november-2014","status":"publish","type":"post","link":"https:\/\/icelandgeology.net\/?p=5237","title":{"rendered":"B\u00e1r\u00f0arbunga volcano update Monday 10-November-2014"},"content":{"rendered":"<p>No major change took place in the eruption in Holuhraun during the weekend. The lava field is now around 70 square kilometres wide and it keeps growing each day. I don&#8217;t know the total volume so far, since that depends on the thickness of the lava. Last calculations that I know of estimated it to be around 1,0 km\u00b3, it is save to assume that volume is now greater since the last estimate that I know of is at least one month old by now.<\/p>\n<p><a href=\"http:\/\/icelandgeology.net\/wp-content\/uploads\/2014\/11\/141110_2055.jpeg\"><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/icelandgeology.net\/wp-content\/uploads\/2014\/11\/141110_2055.jpeg\" alt=\"141110_2055\" width=\"540\" height=\"596\" class=\"aligncenter size-full wp-image-5238\" srcset=\"https:\/\/icelandgeology.net\/wp-content\/uploads\/2014\/11\/141110_2055.jpeg 540w, https:\/\/icelandgeology.net\/wp-content\/uploads\/2014\/11\/141110_2055-271x300.jpeg 271w\" sizes=\"auto, (max-width: 540px) 100vw, 540px\" \/><\/a><br \/>\nThe earthquake activity in B\u00e1r\u00f0arbunga volcano. <em>Copyright of this image belongs to Icelandic Met Office.<\/em><\/p>\n<p>Largest earthquake this weekend had the magnitude of 5,2. Other earthquakes where smaller, but many magnitude 3,0 and larger earthquakes did happen as usual in B\u00e1r\u00f0arbunga volcano. The crust in B\u00e1r\u00f0arbunga volcano is now heavily fractured, this allows heat from the volcano easier way to the surface. This also means new hot springs are going to open up and older ones are going get more active. There is no major change in <a href=\"http:\/\/www.volcano.si.edu\/volcano.cfm?vn=373030\" target=\"_blank\">B\u00e1r\u00f0arbunga<\/a> volcano eruption at the moment, as has been the case for most part of past two months.<br \/>\n<strong><br \/>\nArticle on what is happening in B\u00e1r\u00f0arbunga volcano<\/strong><\/p>\n<p>I am working on a article (in my head at the moment) on what is happening inside B\u00e1r\u00f0arbunga volcano. It is not ready yet, I do hope to have it ready tomorrow if I can process all the data for the article, in order to properly figure out my self what is going on in B\u00e1r\u00f0arbunga volcano.<\/p>\n<p><strong>My geophone network<\/strong><\/p>\n<p>I run a <a href=\"http:\/\/www.jonfr.com\/webicorders\/tremoren.htm\" target=\"_blank\">geophone network<\/a> of just two geophones in Iceland at the moment. Once I get an apartment the total number of working geophones is going to be three. I have decided that once I move from Iceland to Azores Islands[1] it is not going to be workable to keep the network running due the technical problems doing so. I am not going to stop recording earthquakes, I am just going to do so in Azores Islands. At the moment I also have four year backlog of earthquakes that I have to properly add time and location data to. That is a lot of earthquakes over this period, since large events have happened and B\u00e1r\u00f0arbunga alone added up to 2000 earthquakes to my earthquake database in August and now I add around 10 &#8211; 20 earthquakes from B\u00e1r\u00f0arbunga volcano each day (this is just average). The geophone network as it now stands is going to be running for the next 5 &#8211; 10 years while I live in Iceland, after that I am going to relocate it to <a href=\"http:\/\/en.wikipedia.org\/wiki\/Flores_Island_%28Azores%29\" target=\"_blank\">Flores Island<\/a> when I move there[2]. At the moment I <em>don&#8217;t know<\/em> for sure <em>when<\/em> that is going to happen, all I know now is that it is <em>going<\/em> to happen.<\/p>\n<p>1: I am currently living in Denmark. I move next month to Iceland.<br \/>\n2: I plan up to ten years ahead so that I know what I need to do and know before I do it.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>No major change took place in the eruption in Holuhraun during the weekend. The lava field is now around 70 square kilometres wide and it keeps growing each day. I don&#8217;t know the total volume so far, since that depends on the thickness of the lava. Last calculations that I know of estimated it to &hellip; <\/p>\n<p class=\"link-more\"><a href=\"https:\/\/icelandgeology.net\/?p=5237\" class=\"more-link\">Continue reading<span class=\"screen-reader-text\"> &#8220;B\u00e1r\u00f0arbunga volcano update Monday 10-November-2014&#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":[7,169,168,24,10,34,71,17,89,9,82,64,40,96,171,57,85,32,154],"tags":[],"class_list":["post-5237","post","type-post","status-publish","format-standard","hentry","category-bararbunga","category-caldera","category-collapse","category-dyke-intrusions","category-earthquakes","category-eruptions","category-fissures","category-gps-data","category-gps-monitoring","category-harmonic-tremors","category-lava","category-magma","category-monitoring","category-mountain","category-so2","category-swarm","category-tremor-plots","category-volcano","category-webicorders"],"_links":{"self":[{"href":"https:\/\/icelandgeology.net\/index.php?rest_route=\/wp\/v2\/posts\/5237","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=5237"}],"version-history":[{"count":2,"href":"https:\/\/icelandgeology.net\/index.php?rest_route=\/wp\/v2\/posts\/5237\/revisions"}],"predecessor-version":[{"id":5240,"href":"https:\/\/icelandgeology.net\/index.php?rest_route=\/wp\/v2\/posts\/5237\/revisions\/5240"}],"wp:attachment":[{"href":"https:\/\/icelandgeology.net\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=5237"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/icelandgeology.net\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=5237"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/icelandgeology.net\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=5237"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}