{"id":20460,"date":"2016-11-15T08:11:23","date_gmt":"2016-11-15T08:11:23","guid":{"rendered":"http:\/\/blogs.agu.org\/landslideblog\/?p=20460"},"modified":"2016-11-15T08:11:23","modified_gmt":"2016-11-15T08:11:23","slug":"kaikoura-earthquake-landslides","status":"publish","type":"post","link":"https:\/\/blogs.agu.org\/landslideblog\/2016\/11\/15\/kaikoura-earthquake-landslides\/","title":{"rendered":"Kaikoura earthquake landslides: the picture slowly emerges"},"content":{"rendered":"<h5>Kaikoura earthquake landslides: the picture slowly emerges<\/h5>\n<p>As parts of New Zealand continue to reel under the combined effect of the ongoing aftershocks and the effects of very heavy rainfall, the effects and extent of the <a href=\"https:\/\/blogs.agu.org\/landslideblog\/2016\/11\/14\/kaikoura-earthquake-1\/\">Kaikoura earthquake landslides<\/a> are slowly emerging.\u00a0 Much of the focus has been on the coast, and in particular the major landslides that have blocked SH1 and left Kaikoura itself isolated.\u00a0 New images have appeared online of these landslides, which are undoubtedly dramatic.\u00a0 This image was collected by <span class=\"ra-enlarge\"><span class=\"ra-credit\">Sargeant Sam Shepherd of the Royal New Zealand Defence Force:<\/span><\/span><\/p>\n<div id=\"attachment_20463\" style=\"width: 650px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-20463\" class=\"size-full wp-image-20463\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2016\/11\/16_11-Kaikoura-1-e1479195527512.jpg\" alt=\"Kaikoura earthquake landslides\" width=\"640\" height=\"426\" \/><p id=\"caption-attachment-20463\" class=\"wp-caption-text\">One of the Kaikoura earthquake landslides by Sgt Sam Shepherd of the Royal New Zealand Defence Force<\/p><\/div>\n<p>.<\/p>\n<p>Meanwhile some of the most impressive landsliding may well be inland in the Kaikoura Range of hills.\u00a0 The landslide on the Dart Stream that temporarily blocked the valley drew some attention, and this is the first image that I have seen that gives a wider perspective.\u00a0 It suggests extensive landsliding in the range:<\/p>\n<div id=\"attachment_20464\" style=\"width: 634px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-20464\" class=\"size-full wp-image-20464\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2016\/11\/16_11-Clarence-1.jpg\" alt=\"Kaikoura earthquake landslide\" width=\"624\" height=\"415\" srcset=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2016\/11\/16_11-Clarence-1.jpg 624w, https:\/\/blogs.agu.org\/landslideblog\/files\/2016\/11\/16_11-Clarence-1-300x200.jpg 300w\" sizes=\"auto, (max-width: 624px) 100vw, 624px\" \/><p id=\"caption-attachment-20464\" class=\"wp-caption-text\">A first image of Kaikoura earthquake landslides in the Kaikoura range<\/p><\/div>\n<p>.<\/p>\n<p>I suspect that this is the location on Google Earth:<\/p>\n<div id=\"attachment_20466\" style=\"width: 650px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-20466\" class=\"size-full wp-image-20466\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2016\/11\/16_11-Kaikoura-4-e1479196526483.jpg\" alt=\"Kaikoura earthquake landslides\" width=\"640\" height=\"409\" \/><p id=\"caption-attachment-20466\" class=\"wp-caption-text\">Google Earth image of one of the largest of the Kaikoura Earthquake landslides<\/p><\/div>\n<p>.<\/p>\n<p>There will now be a great deal of interest in the extent of the landslides triggered by this earthquake.\u00a0 You can get a reasonable first order estimate of this by comparing the location of the aftershocks to the topography.\u00a0 As a very approximate estimate, the area with steep topography within the area defined by the main aftershocks will have been at a high risk of significant landslides.\u00a0 This is <a href=\"http:\/\/quakesearch.geonet.org.nz\/\">GNS \/ Geonet aftershock data<\/a> plotted on Google Earth, with the location of the valley-blocking landslide above shown:<\/p>\n<div id=\"attachment_20468\" style=\"width: 650px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-20468\" class=\"size-full wp-image-20468\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2016\/11\/16_11-Kaikoura-3b-e1479196890208.jpg\" alt=\"Kaikoura earthquake landslides\" width=\"640\" height=\"396\" \/><p id=\"caption-attachment-20468\" class=\"wp-caption-text\">The location of Kaikoura earthquake aftershocks plotted on Google Earth<\/p><\/div>\n<p>.<\/p>\n<p>The map suggests that a substantial upland area may have been affected by landslides.\u00a0 Of course this sort of approach is extremely rough and ready, and needs to be replaced quickly with proper field data, but it does give an indication of the magnitude of the problem facing New Zealand.<\/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>Over the last 24 hours further information has started to emerge about Kaikoura earthquake landslides on the coast and inland.<!-- 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":20463,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[537],"tags":[1209,23,469,1213,7],"class_list":["post-20460","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-earthquake-induced-landslide","tag-aftershock","tag-earthquake","tag-featured","tag-kaikoura","tag-new-zealand"],"_links":{"self":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/20460","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=20460"}],"version-history":[{"count":0,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/20460\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media\/20463"}],"wp:attachment":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media?parent=20460"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/categories?post=20460"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/tags?post=20460"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}