{"id":9431,"date":"2014-05-01T08:52:05","date_gmt":"2014-05-01T08:52:05","guid":{"rendered":"http:\/\/blogs.agu.org\/landslideblog\/?p=9431"},"modified":"2014-05-01T08:52:05","modified_gmt":"2014-05-01T08:52:05","slug":"annapurna-plateau","status":"publish","type":"post","link":"https:\/\/blogs.agu.org\/landslideblog\/2014\/05\/01\/annapurna-plateau\/","title":{"rendered":"Annapurna plateau: more on the Seti River rock avalanche"},"content":{"rendered":"<h5>Annapurna Plateau<\/h5>\n<p><a href=\"https:\/\/blogs.agu.org\/landslideblog\/2014\/04\/30\/the-seti-river-landslide-2\/\">Following on from my post yesterday<\/a>, I have been asked to explain in more detail why I think that the Google Earth imagery indicates that the rock avalanche reached the gorge system on the edge of the Annapurna Plateau.\u00a0 I realise that I was insufficiently clear.\u00a0 In fact the best way to do this is to zoom in to look at the (actually very good quality) imagery in more detail.\u00a0 This is the December 2011 image of the deposit area of the landslide &#8211; the source is to the right of the image, the gorge system to the left:<\/p>\n<p style=\"text-align: center;\"><a href=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2014\/05\/14_05-Seti-4.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-9433  aligncenter\" alt=\"Annapurna\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2014\/05\/14_05-Seti-4.jpg\" width=\"640\" height=\"400\" srcset=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2014\/05\/14_05-Seti-4.jpg 640w, https:\/\/blogs.agu.org\/landslideblog\/files\/2014\/05\/14_05-Seti-4-300x187.jpg 300w\" sizes=\"auto, (max-width: 640px) 100vw, 640px\" \/><\/a><\/p>\n<p>..<\/p>\n<p>And this is the image of the same area from after the landslide:<\/p>\n<p style=\"text-align: center;\"><a href=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2014\/05\/14_05-Seti-5.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-9434 aligncenter\" alt=\"Annapurna\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2014\/05\/14_05-Seti-5.jpg\" width=\"640\" height=\"400\" srcset=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2014\/05\/14_05-Seti-5.jpg 640w, https:\/\/blogs.agu.org\/landslideblog\/files\/2014\/05\/14_05-Seti-5-300x187.jpg 300w\" sizes=\"auto, (max-width: 640px) 100vw, 640px\" \/><\/a>..<\/p>\n<p style=\"text-align: left;\">I hope that these two image make the changes in the landscape on the plateau rather more clear.\u00a0 In the first, the glaciers and glacial sediments have a very complex topography.\u00a0 In the latter image much of this complexity has been removed as the landslide has eroded away the surface.\u00a0 A zoom in to the area close to the edge of the plateau illustrates this more clearly.\u00a0 This is the &#8220;before&#8221; image:<\/p>\n<p style=\"text-align: center;\"><a href=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2014\/05\/14_05-Seti-6.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-9435 aligncenter\" alt=\"Annapurna\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2014\/05\/14_05-Seti-6.jpg\" width=\"640\" height=\"400\" srcset=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2014\/05\/14_05-Seti-6.jpg 640w, https:\/\/blogs.agu.org\/landslideblog\/files\/2014\/05\/14_05-Seti-6-300x187.jpg 300w\" sizes=\"auto, (max-width: 640px) 100vw, 640px\" \/><\/a><\/p>\n<p style=\"text-align: left;\">..<\/p>\n<p style=\"text-align: left;\">And this is the same area after the landslide:<\/p>\n<p style=\"text-align: center;\"><a href=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2014\/05\/14_05-Seti-7.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-9436 aligncenter\" alt=\"Annapurna\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2014\/05\/14_05-Seti-7.jpg\" width=\"640\" height=\"400\" srcset=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2014\/05\/14_05-Seti-7.jpg 640w, https:\/\/blogs.agu.org\/landslideblog\/files\/2014\/05\/14_05-Seti-7-300x187.jpg 300w\" sizes=\"auto, (max-width: 640px) 100vw, 640px\" \/><\/a><\/p>\n<p style=\"text-align: left;\">..<\/p>\n<p style=\"text-align: left;\">Away from the glaciers, the plateau was clearly covered by a brown layer &#8211; I assume that this is thin, scrubby vegetation (though am happy to be corrected).\u00a0 In the lower image this is still present at the very bottom of the shot, which was not affected by the landslide, but it is not present elsewhere, right up to the head of the gully system on the left side.\u00a0 Indeed this change even extends into the gullies.\u00a0 However, there is not much evidence of a landslide deposit anywhere on the image.\u00a0 So to me it is likely that the landslide ran clean across the Annapurna plateau, eroding and entraining ice and sediment en route, and then entered the gullies.\u00a0 This material then made up the bulk of the devastating debris flow that swept down the Seti River valley.<\/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>I have been asked to provide more detail on why I think the Seti River rock avalanche reached the gully system at the edge of the Annapurna plateau<!-- 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":9436,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[3],"tags":[469,66,306,767,72],"class_list":["post-9431","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-landslide-report","tag-featured","tag-nepal","tag-rock-avalanche","tag-seti","tag-south-asia"],"_links":{"self":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/9431","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=9431"}],"version-history":[{"count":0,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/9431\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media\/9436"}],"wp:attachment":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media?parent=9431"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/categories?post=9431"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/tags?post=9431"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}