{"id":15844,"date":"2015-08-22T05:30:09","date_gmt":"2015-08-22T05:30:09","guid":{"rendered":"http:\/\/blogs.agu.org\/landslideblog\/?p=15844"},"modified":"2015-08-21T16:42:23","modified_gmt":"2015-08-21T16:42:23","slug":"mount-rainier-2015-1","status":"publish","type":"post","link":"https:\/\/blogs.agu.org\/landslideblog\/2015\/08\/22\/mount-rainier-2015-1\/","title":{"rendered":"Mount Rainier debris flows, 13th August 2015"},"content":{"rendered":"<h5>Mount Rainier debris flows<\/h5>\n<p>The Mount Rainier National Park<a href=\"https:\/\/www.facebook.com\/MountRainierNPS\"> Facebook page<\/a> has a nice report about a series of debris flows that occurred on the flanks of the volcano, in Washington State, USA on 13th August 2015 (and there is a good <a href=\"http:\/\/www.nps.gov\/mora\/learn\/news\/westside-road-outburst-flood.htm\">press release<\/a> too).\u00a0 These debris flows originated from the South Tahoma Glacier and rumbled down Tahoma Creek, as this <a href=\"https:\/\/www.facebook.com\/USGSVolcanoes\/photos\/pcb.1101881416507085\/1101881253173768\/?type=1&amp;theater\">Mount Rainier National Park map<\/a> shows:<\/p>\n<div id=\"attachment_15847\" style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2015\/08\/15_08-Rainer-1-e1440172474701.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-15847\" class=\"size-full wp-image-15847\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2015\/08\/15_08-Rainer-1-e1440172474701.jpg\" alt=\"Mount Rainier\" width=\"640\" height=\"494\" \/><\/a><p id=\"caption-attachment-15847\" class=\"wp-caption-text\">Mount Rainer National Park<\/p><\/div>\n<p>.<\/p>\n<p>The debris flows originated as a series of collapses of ice-rich glacial sediment, triggered by the release of stored water from the glacier.\u00a0 This is a common type of event on the flanks of Mount Rainier &#8211; indeed the <a href=\"http:\/\/volcanoes.usgs.gov\/volcanoes\/mount_rainier\/hazard_lahars.html\">USGS has a webpage describing them<\/a>. \u00a0 A <a href=\"https:\/\/www.flickr.com\/photos\/mountrainiernps\/sets\/72157654923795064\/\">helicopter overflight<\/a> by Scott Beason of the Mount Rainer National Park identified the source of the flows quite beautifully:-<\/p>\n<div id=\"attachment_15854\" style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2015\/08\/15_08-Rainer-4-e1440173105111.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-15854\" class=\"size-full wp-image-15854\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2015\/08\/15_08-Rainer-4-e1440173105111.jpg\" alt=\"Mount Rainier\" width=\"640\" height=\"480\" \/><\/a><p id=\"caption-attachment-15854\" class=\"wp-caption-text\"><a href=\"https:\/\/www.facebook.com\/USGSVolcanoes\/photos\/pcb.1101881416507085\/1101881069840453\/?type=1&amp;theater\">Scott Beason, Mount Rainier National Park<\/a><\/p><\/div>\n<p>.<\/p>\n<div id=\"attachment_15858\" style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2015\/08\/15_08-Rainer-2-e1440173202518.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-15858\" class=\"size-full wp-image-15858\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2015\/08\/15_08-Rainer-2-e1440173202518.jpg\" alt=\"Mount Rainier\" width=\"640\" height=\"480\" \/><\/a><p id=\"caption-attachment-15858\" class=\"wp-caption-text\">Scott Beason, Mount Rainier National Park<\/p><\/div>\n<p>.<\/p>\n<p>There is a stunning album of aerial photographs of this event on the <a href=\"https:\/\/www.flickr.com\/photos\/mountrainiernps\/sets\/72157654923795064\/\">Mount Rainier Flickr Page<\/a>.<\/p>\n<p>Perhaps the most exciting element of these events though was the capture of them on the local seismic monitoring network.\u00a0 As the <a href=\"https:\/\/www.facebook.com\/MountRainierNPS\">Mount Rainier National Park Facebook site<\/a> observes:<\/p>\n<blockquote><p>&#8220;Looking at seismic data from the <a class=\"profileLink\" href=\"https:\/\/www.facebook.com\/thePNSN\">Pacific Northwest Seismic Network<\/a>, the vibrations from the debris flow are recorded on seismograms from Rainier station RER, located at Emerald Ridge overlooking Tahoma Creek. The debris flow signal starts at ~9:50 AM PDT. Signals are emergent, pulsatory, and relatively high-frequency\u2014all characteristics of debris flows. There was a period of time from ~9:50 AM through to ~12:45 PM where signals were occurring relatively continuously, with several tens-of-minutes-long higher-amplitude bursts at 10:15-11:10, 11:25-11:50, and 12:30-12:40 that probably correspond to major debris-flow pulses. No debris-flow-like signals showed up overnight.&#8221;<\/p><\/blockquote>\n<p>This is the seismic record:<\/p>\n<div id=\"attachment_15851\" style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2015\/08\/15_08-Rainer-3-e1440173085410.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-15851\" class=\"wp-image-15851 size-full\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2015\/08\/15_08-Rainer-3-e1440173085410.jpg\" alt=\"Mount Rainier\" width=\"640\" height=\"535\" \/><\/a><p id=\"caption-attachment-15851\" class=\"wp-caption-text\"><a href=\"https:\/\/www.facebook.com\/USGSVolcanoes\/photos\/pcb.1101881416507085\/1101881209840439\/?type=1&amp;theater\">Mount Rainer National Park<\/a><\/p><\/div>\n<p>.<\/p>\n<p><a href=\"http:\/\/www.liveleak.com\/view?i=078_1439881529\">Liveleak has a nice video<\/a> of one of the debris flow pulses passing through:<\/p>\n<p><iframe loading=\"lazy\" src=\"http:\/\/www.liveleak.com\/ll_embed?f=085a3eb52d51\" width=\"640\" height=\"360\" frameborder=\"0\" allowfullscreen=\"allowfullscreen\"><\/iframe><\/p>\n<p>.<\/p>\n<h5>Acknowledgement<\/h5>\n<p>Thanks to <a href=\"https:\/\/profile.usgs.gov\/highland\">Lynn Highland of the USGS<\/a> for bringing this one to my attention.<\/p>\n<p>&nbsp;<\/p>\n<!-- AddThis Advanced Settings generic via filter on the_content --><!-- AddThis Share Buttons generic via filter on the_content -->","protected":false},"excerpt":{"rendered":"<p>On 13th August a series of debris flows occurred on the flanks of Mount Rainier in Washington State, USA. These glacier collapse events were captured on video, photographs &#038; seismic instruments<!-- AddThis Advanced Settings generic via filter on wp_trim_excerpt --><!-- AddThis Share Buttons generic via filter on wp_trim_excerpt --><\/p>\n","protected":false},"author":22,"featured_media":15858,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[3,29],"tags":[57,469,619,925,34,959,468,725,48,107],"class_list":["post-15844","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-landslide-report","category-landslide-video","tag-debris-flow","tag-featured","tag-glacier","tag-glof","tag-lahar","tag-landslide-report","tag-n-america","tag-north-america","tag-usa","tag-volcano"],"_links":{"self":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/15844","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/users\/22"}],"replies":[{"embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/comments?post=15844"}],"version-history":[{"count":0,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/15844\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media\/15858"}],"wp:attachment":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media?parent=15844"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/categories?post=15844"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/tags?post=15844"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}