{"id":1825,"date":"2011-11-22T21:46:18","date_gmt":"2011-11-22T21:46:18","guid":{"rendered":"http:\/\/icelandgeology.net\/?p=1825"},"modified":"2011-11-22T21:46:18","modified_gmt":"2011-11-22T21:46:18","slug":"update-for-the-eruption-in-el-hierro-volcano","status":"publish","type":"post","link":"https:\/\/icelandgeology.net\/?p=1825","title":{"rendered":"Update for the eruption in El Hierro volcano"},"content":{"rendered":"<p>As the eruption in <a href=\"http:\/\/www.volcano.si.edu\/world\/volcano.cfm?vnum=1803-02-\" target=\"_blank\">El Hierro<\/a> volcano moves closer to the second month. Information on what has been going on has gone bit hard to come by (for me anyway). As people settle with there new reality (erupting volcano). But that does not stop me from reporting on it.<\/p>\n<p>The current status of the eruption is that nothing much has changed since last blog post. But yesterday there where reports of new vents opening up off the south coast of El Hierro volcano. But this is the area where current eruption has been taking place the past month and a half. It remains to be seen if that is going to change or not. But earthquake activity has continued in north part of El Hierro volcano. This earthquake activity seems to be a mixed one. But that means there are both earthquakes due to dike intrusions and local tectonic earthquakes. I now think that this earthquake activity is going to continue all the eruption. I am not sure why a eruption has not started in north part of El Hierro volcano yet. But for the moment it is just earthquakes. The strongest earthquakes in this area can go up to Mb5.0 in size. But I base that on what type of rock makes up the area, along with the thickness of the crust. But that is from 10 km thick.<\/p>\n<p><a href=\"http:\/\/icelandgeology.net\/wp-content\/uploads\/2011\/11\/Eventos_HIERRO_2D.22.november.2011.20.23.utc_.jpg\"><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/icelandgeology.net\/wp-content\/uploads\/2011\/11\/Eventos_HIERRO_2D.22.november.2011.20.23.utc_.jpg\" alt=\"\" title=\"Eventos_HIERRO_2D.22.november.2011.20.23.utc\" width=\"1001\" height=\"1000\" class=\"aligncenter size-full wp-image-1826\" srcset=\"https:\/\/icelandgeology.net\/wp-content\/uploads\/2011\/11\/Eventos_HIERRO_2D.22.november.2011.20.23.utc_.jpg 1001w, https:\/\/icelandgeology.net\/wp-content\/uploads\/2011\/11\/Eventos_HIERRO_2D.22.november.2011.20.23.utc_-150x150.jpg 150w, https:\/\/icelandgeology.net\/wp-content\/uploads\/2011\/11\/Eventos_HIERRO_2D.22.november.2011.20.23.utc_-300x300.jpg 300w\" sizes=\"auto, (max-width: 767px) 89vw, (max-width: 1000px) 54vw, (max-width: 1071px) 543px, 580px\" \/><\/a><br \/>\nThe earthquake activity for the past 48 hours in El Hierro volcano (picture from 22 November, 2011). <em>Copyright of this picture belongs to IGN (Instituto Geogr\u00e1fico Nacional).<\/em><\/p>\n<p><a href=\"http:\/\/icelandgeology.net\/wp-content\/uploads\/2011\/11\/Eventos_HIERRO_10.22.november.2011.20.23.utc_.jpg\"><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/icelandgeology.net\/wp-content\/uploads\/2011\/11\/Eventos_HIERRO_10.22.november.2011.20.23.utc_.jpg\" alt=\"\" title=\"Eventos_HIERRO_10.22.november.2011.20.23.utc\" width=\"1001\" height=\"1000\" class=\"aligncenter size-full wp-image-1827\" srcset=\"https:\/\/icelandgeology.net\/wp-content\/uploads\/2011\/11\/Eventos_HIERRO_10.22.november.2011.20.23.utc_.jpg 1001w, https:\/\/icelandgeology.net\/wp-content\/uploads\/2011\/11\/Eventos_HIERRO_10.22.november.2011.20.23.utc_-150x150.jpg 150w, https:\/\/icelandgeology.net\/wp-content\/uploads\/2011\/11\/Eventos_HIERRO_10.22.november.2011.20.23.utc_-300x300.jpg 300w\" sizes=\"auto, (max-width: 767px) 89vw, (max-width: 1000px) 54vw, (max-width: 1071px) 543px, 580px\" \/><\/a><br \/>\nEarthquake activity in El Hierro volcano for the past 4 days. <em>Copyright of this picture belongs to IGN (Instituto Geogr\u00e1fico Nacional).<\/em><\/p>\n<p><a href=\"http:\/\/icelandgeology.net\/wp-content\/uploads\/2011\/11\/Eventos_HIERRO_2011.22.november.2011.21.00.utc_.jpg\"><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/icelandgeology.net\/wp-content\/uploads\/2011\/11\/Eventos_HIERRO_2011.22.november.2011.21.00.utc_.jpg\" alt=\"\" title=\"Eventos_HIERRO_2011.22.november.2011.21.00.utc\" width=\"1001\" height=\"1000\" class=\"aligncenter size-full wp-image-1828\" srcset=\"https:\/\/icelandgeology.net\/wp-content\/uploads\/2011\/11\/Eventos_HIERRO_2011.22.november.2011.21.00.utc_.jpg 1001w, https:\/\/icelandgeology.net\/wp-content\/uploads\/2011\/11\/Eventos_HIERRO_2011.22.november.2011.21.00.utc_-150x150.jpg 150w, https:\/\/icelandgeology.net\/wp-content\/uploads\/2011\/11\/Eventos_HIERRO_2011.22.november.2011.21.00.utc_-300x300.jpg 300w\" sizes=\"auto, (max-width: 767px) 89vw, (max-width: 1000px) 54vw, (max-width: 1071px) 543px, 580px\" \/><\/a><br \/>\nThe earthquake activity from July 2011. This earthquake activity maps out well where the magma lies in the El Hierro volcano. But as the magma expands in the crust, it creates earthquake activity. <em>Copyright of this picture belongs to IGN (Instituto Geogr\u00e1fico Nacional).<\/em><\/p>\n<p>The harmonic tremor tells me what is going on in the eruption, when I lack all other visual data on what exactly is going on. But the harmonic tremor increases or drops depending on the strength of the eruption. But that aspect of the eruption is based on how many and how large fissures are open at the time.<\/p>\n<p><a href=\"http:\/\/icelandgeology.net\/wp-content\/uploads\/2011\/11\/CHIE_2011-11-22.21.11.utc_.jpg\"><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/icelandgeology.net\/wp-content\/uploads\/2011\/11\/CHIE_2011-11-22.21.11.utc_-1024x767.jpg\" alt=\"\" title=\"CHIE_2011-11-22.21.11.utc\" width=\"640\" height=\"479\" class=\"aligncenter size-large wp-image-1829\" srcset=\"https:\/\/icelandgeology.net\/wp-content\/uploads\/2011\/11\/CHIE_2011-11-22.21.11.utc_-1024x767.jpg 1024w, https:\/\/icelandgeology.net\/wp-content\/uploads\/2011\/11\/CHIE_2011-11-22.21.11.utc_-300x224.jpg 300w, https:\/\/icelandgeology.net\/wp-content\/uploads\/2011\/11\/CHIE_2011-11-22.21.11.utc_.jpg 1025w\" sizes=\"auto, (max-width: 640px) 100vw, 640px\" \/><\/a><br \/>\nThe harmonic tremor as it is today (22 November, 2011) at 21:11 UTC. The eruption as can be seen is around the same level as before. But this is not the strongest the harmonic tremor has been. <em>Copyright of this picture belongs to IGN (Instituto Geogr\u00e1fico Nacional).<\/em><\/p>\n<p><a href=\"http:\/\/icelandgeology.net\/wp-content\/uploads\/2011\/11\/CHIE_2011-11-20.svd_.22.november.2011.20.43.utc_.jpg\"><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/icelandgeology.net\/wp-content\/uploads\/2011\/11\/CHIE_2011-11-20.svd_.22.november.2011.20.43.utc_-1024x767.jpg\" alt=\"\" title=\"CHIE_2011-11-20.svd.22.november.2011.20.43.utc\" width=\"640\" height=\"479\" class=\"aligncenter size-large wp-image-1830\" srcset=\"https:\/\/icelandgeology.net\/wp-content\/uploads\/2011\/11\/CHIE_2011-11-20.svd_.22.november.2011.20.43.utc_-1024x767.jpg 1024w, https:\/\/icelandgeology.net\/wp-content\/uploads\/2011\/11\/CHIE_2011-11-20.svd_.22.november.2011.20.43.utc_-300x224.jpg 300w, https:\/\/icelandgeology.net\/wp-content\/uploads\/2011\/11\/CHIE_2011-11-20.svd_.22.november.2011.20.43.utc_.jpg 1025w\" sizes=\"auto, (max-width: 640px) 100vw, 640px\" \/><\/a><br \/>\nThe harmonic tremor when the eruption was more active then today. This can clearly be seen by how the harmonic tremor is stronger then the scale of the harmonic tremor plot. This happens when a new fissure opens up and its eruption is at the strongest. <em>Copyright of this picture belongs to IGN (Instituto Geogr\u00e1fico Nacional).<\/em><\/p>\n<p>The IGN web site on El Hierro volcano eruption can be found <a href=\"http:\/\/www.01.ign.es\/ign\/resources\/volcanologia\/HIERRO.html\" target=\"_blank\">here<\/a>. But it is in Spanish.<\/p>\n<p>I am continuing to monitor this eruption. Even if it is a long term eruption, but that are eruptions that are longer then 1 month. As the for the eruption as a whole, little change has taken place in terms of strenght and location of the eruption. But that might change without warning as before.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>As the eruption in El Hierro volcano moves closer to the second month. Information on what has been going on has gone bit hard to come by (for me anyway). As people settle with there new reality (erupting volcano). But that does not stop me from reporting on it. The current status of the eruption &hellip; <\/p>\n<p class=\"link-more\"><a href=\"https:\/\/icelandgeology.net\/?p=1825\" class=\"more-link\">Continue reading<span class=\"screen-reader-text\"> &#8220;Update for the eruption in El Hierro 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":[93,24,10,91,34,71,82,64,40,92,57,85,32],"tags":[],"class_list":["post-1825","post","type-post","status-publish","format-standard","hentry","category-canary-islands","category-dyke-intrusions","category-earthquakes","category-el-hierro","category-eruptions","category-fissures","category-lava","category-magma","category-monitoring","category-spain","category-swarm","category-tremor-plots","category-volcano"],"_links":{"self":[{"href":"https:\/\/icelandgeology.net\/index.php?rest_route=\/wp\/v2\/posts\/1825","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=1825"}],"version-history":[{"count":1,"href":"https:\/\/icelandgeology.net\/index.php?rest_route=\/wp\/v2\/posts\/1825\/revisions"}],"predecessor-version":[{"id":1831,"href":"https:\/\/icelandgeology.net\/index.php?rest_route=\/wp\/v2\/posts\/1825\/revisions\/1831"}],"wp:attachment":[{"href":"https:\/\/icelandgeology.net\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=1825"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/icelandgeology.net\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=1825"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/icelandgeology.net\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=1825"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}