{"id":1308,"date":"2014-08-26T12:32:37","date_gmt":"2014-08-26T11:32:37","guid":{"rendered":"http:\/\/all-geo.org\/volcan01010\/?p=1308"},"modified":"2014-08-26T12:32:37","modified_gmt":"2014-08-26T11:32:37","slug":"bardarbunga-turning-dettifoss-into-niagara-falls","status":"publish","type":"post","link":"https:\/\/all-geo.org\/volcan01010\/2014\/08\/bardarbunga-turning-dettifoss-into-niagara-falls\/","title":{"rendered":"B\u00e1r\u00f0arbunga &#8211; turning Dettifoss into Niagara Falls"},"content":{"rendered":"<blockquote><p>While international concern about an eruption at B\u00e1r\u00f0arbunga is focussed on flight disruption, a <a href=\"https:\/\/en.wikipedia.org\/wiki\/J%C3%B6kulhlaup\" target=\"_blank\">j\u00f6kulhlaup<\/a> (meltwater flood) is the most destructive potential outcome of a subglacial eruption. It would travel north from the glacier along the J\u00f6kuls\u00e1 \u00e1 Fj\u00f6llum river, and for this reason <a href=\"http:\/\/www.mbl.is\/frettir\/innlent\/2014\/08\/20\/a_map_of_seismic_activity_by_severity\/\">roads have been closed<\/a> in the area. Edwin Baynes is a PhD student at Edinburgh University who studies past j\u00f6kulhlaups in this area. In this guest post, he puts such a potential flood in context.<\/p><\/blockquote>\n<hr \/>\n<h3>Turning Dettifoss into Niagara Falls<\/h3>\n<p>An Icelandic geophysicist, Magn\u00fas Tumi Gu\u00f0mundsson, has predicted that if a subglacial eruption were to occur at B\u00e1r\u00f0arbunga, the meltwaters could increase the discharge in the J\u00f6kuls\u00e1 \u00e1 Fj\u00f6llum river by <a href=\"http:\/\/www.mbl.is\/frettir\/innlent\/2014\/08\/20\/it_could_go_either_way\/\" target=\"_blank\">10 or 20 times<\/a> (to 2,000 &#8211; 4,000 m<sup>3<\/sup> s<sup>-1<\/sup>). He describes such a flood as &#8216;<em>not catastrophic<\/em>&#8216; because it is <a href=\"http:\/\/www.almannavarnir.is\/upload\/files\/Volcanic%20hazards%20in%20Iceland.pdf\" target=\"_blank\">smaller than the j\u00f6kulhlaups<\/a> caused by the 1996 Gj\u00e1lp eruption (45,000 m<sup>3<\/sup> s<sup>-1<\/sup>), which washed away the Skei\u00f0ar\u00e1sandur bridge in South Iceland, or the estimated discharge for the <a href=\"http:\/\/all-geo.org\/volcan01010\/2011\/11\/why-people-are-scared-of-katla\/\">Katla 1918 flood<\/a> (300,000 m<sup>3<\/sup> s<sup>-1<\/sup>). It is still very serious, however, and has potential to inundate the landscape and destroy important infrastructure such as bridges and farms. The map below shows the areas most likely to be affected.<\/p>\n<div id=\"attachment_1310\" style=\"width: 380px\" class=\"wp-caption aligncenter\"><a href=\"http:\/\/www.mbl.is\/frettir\/innlent\/2014\/08\/21\/flestir_skjalftanna_um_tvo_stig\/\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1310\" class=\"size-full wp-image-1310\" alt=\"\" src=\"http:\/\/all-geo.org\/volcan01010\/wp-content\/uploads\/2014\/08\/759786.jpg\" width=\"370\" height=\"640\" srcset=\"https:\/\/all-geo.org\/volcan01010\/wp-content\/uploads\/2014\/08\/759786.jpg 370w, https:\/\/all-geo.org\/volcan01010\/wp-content\/uploads\/2014\/08\/759786-173x300.jpg 173w\" sizes=\"auto, (max-width: 370px) 100vw, 370px\" \/><\/a><p id=\"caption-attachment-1310\" class=\"wp-caption-text\">Area most likely to be affected by j\u00f6kulhlaup following subglacial eruption at B\u00e1r\u00f0arbunga. Published by Morgunbla\u00f0i\u00f0 &#8211; click image to see original article.<\/p><\/div>\n<p>J\u00f6kuls\u00e1 a Fj\u00f6llum contains some pretty impressive waterfalls, the most notable of which is Dettifoss. With a vertical drop of around 50 m and a peak summer discharge of 300-400 m<sup>3<\/sup>s<sup>-1<\/sup>, it is reputed to be \u2018<span style=\"color: #000080\"><span style=\"text-decoration: underline\"><a href=\"http:\/\/www.vatnajokulsthjodgardur.is\/english\/education\/dettifoss\/\">Europe\u2019s most powerful waterfall<\/a><\/span><\/span>\u2019. Sci-fi fans may recognise it from the start of Prometheus, much of which <span style=\"color: #000080\"><span style=\"text-decoration: underline\"><a href=\"http:\/\/all-geo.org\/volcan01010\/2012\/06\/on-the-geology-of-prometheus\/\">was filmed in Iceland<\/a><\/span><\/span>.<\/p>\n<p><iframe loading=\"lazy\" title=\"Dettifoss, North-East Iceland\" width=\"640\" height=\"480\" src=\"https:\/\/www.youtube.com\/embed\/UdGJN96Hty4?feature=oembed\" frameborder=\"0\" allow=\"accelerometer; autoplay; clipboard-write; encrypted-media; gyroscope; picture-in-picture; web-share\" referrerpolicy=\"strict-origin-when-cross-origin\" allowfullscreen><\/iframe><\/p>\n<p>For comparison, the average discharge of the <span style=\"color: #000080\"><span style=\"text-decoration: underline\"><a href=\"https:\/\/www.google.co.uk\/maps\/place\/Niagara+Falls\/@43.082816,-79.074163,2260m\/data=!3m1!1e3!4m2!3m1!1s0x89d34307412d7ae9:0x29be1d1e689ce35b\">Niagara river<\/a><\/span><\/span> is ~2,400 m<sup>3<\/sup>s<sup>-1<\/sup> at <a href=\"https:\/\/en.wikipedia.org\/wiki\/Niagara_Falls\" target=\"_blank\">Niagara Falls<\/a>. Although Niagara Falls and Dettifoss have similar vertical drops (~50 m), Dettifoss is much narrower (~100 m wide vs ~700 m). A 20 times increase in discharge would mean a significant rise in water level within the channel, increased erosion and a possibly even an upstream retreat of Dettifoss waterfall by a short distance.<\/p>\n<div id=\"attachment_1330\" style=\"width: 560px\" class=\"wp-caption aligncenter\"><a href=\"http:\/\/all-geo.org\/volcan01010\/wp-content\/uploads\/2014\/08\/DettifossNiagara1.png\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1330\" class=\"size-full wp-image-1330\" alt=\"    A j\u00f6kulhlaup down the J\u00f6kuls\u00e1 \u00e1 Fj\u00f6llum river following a subglacial eruption at B\u00e1r\u00f0arbunga increase the discharge over Dettifoss to levels similar to Niagara Falls.\" src=\"http:\/\/all-geo.org\/volcan01010\/wp-content\/uploads\/2014\/08\/DettifossNiagara1.png\" width=\"550\" height=\"778\" srcset=\"https:\/\/all-geo.org\/volcan01010\/wp-content\/uploads\/2014\/08\/DettifossNiagara1.png 550w, https:\/\/all-geo.org\/volcan01010\/wp-content\/uploads\/2014\/08\/DettifossNiagara1-212x300.png 212w\" sizes=\"auto, (max-width: 550px) 100vw, 550px\" \/><\/a><p id=\"caption-attachment-1330\" class=\"wp-caption-text\">A j\u00f6kulhlaup down the J\u00f6kuls\u00e1 \u00e1 Fj\u00f6llum river following a subglacial eruption at B\u00e1r\u00f0arbunga could increase the discharge over Dettifoss to levels similar to Niagara Falls.<\/p><\/div>\n<h3>Evidence for past j\u00f6kulhlaups<\/h3>\n<p>Although rare on a human timescale, the J\u00f6kuls\u00e1 \u00e1 Fj\u00f6llum is no stranger to j\u00f6kulhlaups. There are historic reports of powerful floods in the 17<sup>th<\/sup> and 18<sup>th<\/sup> centuries that destroyed farmland further downstream from Dettifoss.\u00a0 There have also been numerous prehistoric j\u00f6kulhlaups of varying magnitude over the last 10,000 years, since most of the ice retreated from Iceland. \u00a0<a href=\"http:\/\/www.sciencedirect.com\/science\/article\/pii\/S0277379105001599\">Alho <i>et al.<\/i> (2005)<\/a> used computer models to estimate the discharge that would be necessary to produce the water levels indicated by the highest boulder deposits and the highest fluvially-washed surfaces along the channel. Their result was 900,000 m<sup>3<\/sup>s<sup>-1<\/sup>. This is more than triple the flow of the Amazon and close to rivalling some of the biggest \u2018megafloods\u2019 that have ever occurred on Earth.<\/p>\n<p>As expected, such large discharges had a significant impact on the landscape.\u00a0 The evidence for this erosion by the J\u00f6kuls\u00e1 \u00e1 Fj\u00f6llum river is preserved in the rocks of the J\u00f6kuls\u00e1rglj\u00fafur and \u00c1sbyrgi canyons.<\/p>\n<div id=\"attachment_1313\" style=\"width: 570px\" class=\"wp-caption aligncenter\"><a href=\"http:\/\/all-geo.org\/volcan01010\/wp-content\/uploads\/2014\/08\/downstream.png\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1313\" class=\" wp-image-1313 \" alt=\"Looking downstream from Dettifoss into the ~500 m wide, 100m deep, J\u00f6kuls\u00e1rglj\u00fafur canyon, carved out by j\u00f6kulhlaups since the last Ice Age. Photo: E. Baynes, June 2012\" src=\"http:\/\/all-geo.org\/volcan01010\/wp-content\/uploads\/2014\/08\/downstream.png\" width=\"560\" height=\"421\" srcset=\"https:\/\/all-geo.org\/volcan01010\/wp-content\/uploads\/2014\/08\/downstream.png 700w, https:\/\/all-geo.org\/volcan01010\/wp-content\/uploads\/2014\/08\/downstream-300x225.png 300w\" sizes=\"auto, (max-width: 560px) 100vw, 560px\" \/><\/a><p id=\"caption-attachment-1313\" class=\"wp-caption-text\">Looking downstream from Dettifoss into the ~500 m wide, 100m deep, J\u00f6kuls\u00e1rglj\u00fafur canyon, carved out by j\u00f6kulhlaups since the last Ice Age. Photo: E. Baynes, June 2012<\/p><\/div>\n<p>The canyon is significantly wider than the modern river channel (~100 m wide), indicating that the flow was much greater when the canyon was formed. Within the canyon are strath terraces (white dashed lines) that indicate historical positions of the river bed. The upper terrace is at the same elevation as Dettifoss and has been abandoned due to the retreat of Dettifoss during the largest j\u00f6kulhlaups. Also shown in the photo is a volcanic fissure that erupted 8500 years ago. The canyon has eroded through one of the volcanic craters, exposing the conduit that brings lava to the surface in the canyon walls. The canyon is therefore younger than the fissure (i.e. &lt;8,500 years).<\/p>\n<h3>The product of a catastrophic j\u00f6kulhlaup<\/h3>\n<div id=\"attachment_1315\" style=\"width: 586px\" class=\"wp-caption aligncenter\"><a href=\"http:\/\/all-geo.org\/volcan01010\/wp-content\/uploads\/2014\/08\/AsbyrgiView.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1315\" class=\" wp-image-1315\" alt=\"AsbyrgiView\" src=\"http:\/\/all-geo.org\/volcan01010\/wp-content\/uploads\/2014\/08\/AsbyrgiView-1024x768.jpg\" width=\"576\" height=\"432\" srcset=\"https:\/\/all-geo.org\/volcan01010\/wp-content\/uploads\/2014\/08\/AsbyrgiView-1024x768.jpg 1024w, https:\/\/all-geo.org\/volcan01010\/wp-content\/uploads\/2014\/08\/AsbyrgiView-300x225.jpg 300w, https:\/\/all-geo.org\/volcan01010\/wp-content\/uploads\/2014\/08\/AsbyrgiView.jpg 1297w\" sizes=\"auto, (max-width: 576px) 100vw, 576px\" \/><\/a><p id=\"caption-attachment-1315\" class=\"wp-caption-text\">Caption: Looking North into \u00c1sbyrgi canyon. Horseshoe shaped, 3 km long, 1 km wide, up to 100 m deep was carved out during a j\u00f6kulhlaup that flowed away from where the photo is taken from. The floor of \u00c1sbyrgi is littered with large boulders (some greater than 3 m in diameter) which shows that once there was a high magnitude flow within \u00c1sbyrgi capable of transporting such large blocks. Photo: M. Attal, August 2012<\/p><\/div>\n<p>Twenty-five kilometres north of Dettifoss is <span style=\"color: #000080\"><span style=\"text-decoration: underline\"><a href=\"http:\/\/www.vatnajokulsthjodgardur.is\/english\/education\/asbyrgi\/\">\u00c1sbyrgi<\/a><\/span><\/span>, a vast horseshoe-shaped canyon 3 km long, 1 km wide and up to 100 m deep. According to Norse mythology, \u00c1sbyrgi was formed when Odin\u2019s 8-legged horse, Sleipnir, stumbled and put a hoof down on Earth. However, evidence in the landscape suggests that a more likely hypothesis is that \u00c1sbyrgi was carved during a j\u00f6kulhlaup along the course of the J\u00f6kuls\u00e1 \u00e1 Fj\u00f6llum.<\/p>\n<div id=\"attachment_1314\" style=\"width: 594px\" class=\"wp-caption aligncenter\"><a href=\"http:\/\/all-geo.org\/volcan01010\/wp-content\/uploads\/2014\/08\/AsbyrgiRim.png\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1314\" class=\" wp-image-1314 \" alt=\"AsbyrgiRim\" src=\"http:\/\/all-geo.org\/volcan01010\/wp-content\/uploads\/2014\/08\/AsbyrgiRim.png\" width=\"584\" height=\"438\" srcset=\"https:\/\/all-geo.org\/volcan01010\/wp-content\/uploads\/2014\/08\/AsbyrgiRim.png 730w, https:\/\/all-geo.org\/volcan01010\/wp-content\/uploads\/2014\/08\/AsbyrgiRim-300x224.png 300w\" sizes=\"auto, (max-width: 584px) 100vw, 584px\" \/><\/a><p id=\"caption-attachment-1314\" class=\"wp-caption-text\">The large plunge pool at the base of the headwall at \u00c1sbyrgi. Upstream, the landscape has been heavily scoured and sculpted by the action of water. Photo: M. Attal, August 2012<\/p><\/div>\n<p>Large plunge pools are present at the base of the canyon headwall, there is a water-sculpted surface immediately upstream of the canyon and the amphitheatre-shaped canyon head is very similar to features elsewhere such as <span style=\"color: #000080\"><span style=\"text-decoration: underline\"><a href=\"https:\/\/www.google.co.uk\/maps\/place\/Box+Canyon+State+Park\/@42.7079859,-114.8117695,2261m\/data=!3m1!1e3!4m2!3m1!1s0x54ac8dd8110b781f:0x76069a60b50fa9b8\">Box Canyon<\/a><\/span><\/span> in Idaho and <span style=\"color: #000080\"><span style=\"text-decoration: underline\"><a href=\"https:\/\/www.google.co.uk\/maps\/place\/Dry+Falls+Lake,+Washington+99115,+USA\/@47.602888,-119.3508897,4130m\/data=!3m1!1e3!4m2!3m1!1s0x549c07beb2202045:0x9849862f34c01c7f\">Dry Falls Lake<\/a><\/span><\/span> in Washington. Both of these formed during floods following catastrophic drainage of ice-dammed lakes <span style=\"color: #000080\"><span style=\"text-decoration: underline\"><a href=\"http:\/\/en.wikipedia.org\/wiki\/Lake_Bonneville\">Bonneville<\/a><\/span><\/span> and <span style=\"color: #000080\"><span style=\"text-decoration: underline\"><a href=\"http:\/\/en.wikipedia.org\/wiki\/Missoula_Floods\">Missoula<\/a><\/span><\/span>, respectively.\u00a0 Each of these features indicate a j\u00f6kulhlaup origin for \u00c1sbyrgi and show the potential for catastrophic erosion during j\u00f6kulhlaups along the J\u00f6kuls\u00e1 \u00e1 Fj\u00f6llum following volcanic eruptions beneath the Vatnaj\u00f6kull ice cap.<\/p>\n<hr \/>\n<blockquote><p>Edwin&#8217;s PhD project is titled: <i>Constraining bedrock erosion during <\/i><i>extreme flood events in Iceland<\/i>. He researches j\u00f6kulhlaups in the J\u00f6kuls\u00e1rglj\u00fafur and \u00c1sbyrgi canyons using topographic analysis and surface exposure dating with cosmogenic nuclides. You can find more information on his website at <a href=\"http:\/\/www.geos.ed.ac.uk\/homes\/s1141604\/\">http:\/\/www.geos.ed.ac.uk\/homes\/s1141604\/<\/a>. You can also follow Edwin on Twitter: <a href=\"https:\/\/twitter.com\/EdwinBaynes\">@EdwinBaynes<\/a>.<\/p><\/blockquote>\n","protected":false},"excerpt":{"rendered":"<p>While international concern about an eruption at B\u00e1r\u00f0arbunga is focussed on flight disruption, a j\u00f6kulhlaup (meltwater flood) is the most destructive potential outcome of a subglacial eruption. It would travel north from the glacier along the J\u00f6kuls\u00e1 \u00e1 Fj\u00f6llum river, &hellip; <a href=\"https:\/\/all-geo.org\/volcan01010\/2014\/08\/bardarbunga-turning-dettifoss-into-niagara-falls\/\">Continue reading <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":3,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1],"tags":[],"class_list":["post-1308","post","type-post","status-publish","format-standard","hentry","category-uncategorized"],"_links":{"self":[{"href":"https:\/\/all-geo.org\/volcan01010\/wp-json\/wp\/v2\/posts\/1308","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/all-geo.org\/volcan01010\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/all-geo.org\/volcan01010\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/all-geo.org\/volcan01010\/wp-json\/wp\/v2\/users\/3"}],"replies":[{"embeddable":true,"href":"https:\/\/all-geo.org\/volcan01010\/wp-json\/wp\/v2\/comments?post=1308"}],"version-history":[{"count":23,"href":"https:\/\/all-geo.org\/volcan01010\/wp-json\/wp\/v2\/posts\/1308\/revisions"}],"predecessor-version":[{"id":1337,"href":"https:\/\/all-geo.org\/volcan01010\/wp-json\/wp\/v2\/posts\/1308\/revisions\/1337"}],"wp:attachment":[{"href":"https:\/\/all-geo.org\/volcan01010\/wp-json\/wp\/v2\/media?parent=1308"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/all-geo.org\/volcan01010\/wp-json\/wp\/v2\/categories?post=1308"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/all-geo.org\/volcan01010\/wp-json\/wp\/v2\/tags?post=1308"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}