{"id":20553,"date":"2016-11-28T07:38:38","date_gmt":"2016-11-28T07:38:38","guid":{"rendered":"http:\/\/blogs.agu.org\/landslideblog\/?p=20553"},"modified":"2016-11-28T07:38:38","modified_gmt":"2016-11-28T07:38:38","slug":"m7-8-kaikoura-earthquake","status":"publish","type":"post","link":"https:\/\/blogs.agu.org\/landslideblog\/2016\/11\/28\/m7-8-kaikoura-earthquake\/","title":{"rendered":"A revised landslide map for the M=7.8 Kaikoura earthquake"},"content":{"rendered":"<h5>A revised landslide map for the M=7.8 Kaikoura earthquake<\/h5>\n<p>Valkaniotis Sotiris of the Earthquake Geology Research Group and the Aristotle University of Thessaloniki has <a href=\"http:\/\/eqgeogr.weebly.com\/blog\/map-of-co-seismic-landslides-surface-ruptures-for-the-m-78-kaikoura-new-zealand-earthquake-version-2\">posted a revised map of the landslides<\/a> triggered by the M=7.8 Kaikoura Earthquake in New Zealand on his blog.\u00a0 This map is available as a <a href=\"http:\/\/eqgeogr.weebly.com\/uploads\/8\/2\/8\/3\/8283914\/landslide_map_v2.jpg\">high resolution download<\/a>:<\/p>\n<div id=\"attachment_20556\" style=\"width: 650px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-20556\" class=\"size-full wp-image-20556\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2016\/11\/16_11-landslide_map_v2-e1480316182792.jpg\" alt=\"M=7.8 Kaikoura earthquake\" width=\"640\" height=\"798\" \/><p id=\"caption-attachment-20556\" class=\"wp-caption-text\"><a href=\"http:\/\/eqgeogr.weebly.com\/uploads\/8\/2\/8\/3\/8283914\/landslide_map_v2.jpg\">Map of Co-seismic ruptures and landslides<\/a> from the M=7.8 Kaikoura earthquake in New Zealand<\/p><\/div>\n<p>.<\/p>\n<p>To generate this map, which shows 5,875 landslides is a remarkable effort.\u00a0 The maps of the density of landslides is particularly interesting to me:<\/p>\n<div id=\"attachment_20558\" style=\"width: 637px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-20558\" class=\"size-full wp-image-20558\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2016\/11\/16_11-Landslide-density.jpg\" alt=\"M=7.8 Kaikoura Earthquake\" width=\"627\" height=\"769\" srcset=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2016\/11\/16_11-Landslide-density.jpg 627w, https:\/\/blogs.agu.org\/landslideblog\/files\/2016\/11\/16_11-Landslide-density-245x300.jpg 245w\" sizes=\"auto, (max-width: 627px) 100vw, 627px\" \/><p id=\"caption-attachment-20558\" class=\"wp-caption-text\"><a href=\"http:\/\/eqgeogr.weebly.com\/uploads\/8\/2\/8\/3\/8283914\/landslide_map_v2.jpg\">Map of landslide density<\/a> from the M=7.8 Kaikoura earthquake, via Valkaniotis Sotiris<\/p><\/div>\n<p>.<\/p>\n<p>I noted in my earlier post that a reasonable first order estimate of the landslide locations can be obtained from the coincidence of the topography and the aftershock sequence.\u00a0 This is a map of the aftershocks from the earthquake, mapped as a<a href=\"http:\/\/quakesearch.geonet.org.nz\/\"> KML by Geonet<\/a>.<\/p>\n<div id=\"attachment_20559\" style=\"width: 650px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-20559\" class=\"size-full wp-image-20559\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2016\/11\/16_11-aftershock-density-e1480317644908.jpg\" alt=\"M=7.8 Kaikoura earthquake\" width=\"640\" height=\"396\" \/><p id=\"caption-attachment-20559\" class=\"wp-caption-text\"><a href=\"http:\/\/quakesearch.geonet.org.nz\/\">Geonet \/ GNS data<\/a> showing the locations of the aftershock sequence triggered by the M=7.8 Kaikoura earthquake, mapped on Google Earth<\/p><\/div>\n<p>.<\/p>\n<p>The coincidence between the two is not perfect of course (we would not expect it to be)\u00a0 but the aftershocks are a surprisingly good predictor of the landslide distribution.\u00a0 It would be interesting to know whether the aftershocks are a better predictor than the ShakeMap peak ground acceleration data.\u00a0 The map produced by Valkaniotis Sotiris hints that this might be the case.<\/p>\n<h5>Other posts that might be of interest:<\/h5>\n<ul>\n<li class=\"posttitle srch\"><a title=\"Permanent Link to Geonet commentary on landslides triggered by the Kaikoura Earthquake\" href=\"https:\/\/blogs.agu.org\/landslideblog\/2016\/11\/20\/geonet-1\/\" rel=\"bookmark\">Geonet commentary on landslides triggered by the Kaikoura Earthquake<\/a><\/li>\n<li class=\"posttitle srch\"><a title=\"Permanent Link to Kaikoura earthquake landslides: the picture slowly emerges\" href=\"https:\/\/blogs.agu.org\/landslideblog\/2016\/11\/15\/kaikoura-earthquake-landslides\/\" rel=\"bookmark\">Kaikoura earthquake landslides: the picture slowly emerges<\/a><\/li>\n<li class=\"posttitle srch\"><a title=\"Permanent Link to First news of landslides from the Kaikoura Earthquake sequence in New Zealand yesterday\" href=\"https:\/\/blogs.agu.org\/landslideblog\/2016\/11\/14\/kaikoura-earthquake-1\/\" rel=\"bookmark\">First news of landslides from the Kaikoura Earthquake sequence in New Zealand yesterday<\/a><\/li>\n<li class=\"posttitle srch\"><a title=\"Permanent Link to Hapuku River: a major landslide dam after the earthquake in New Zealand\" href=\"https:\/\/blogs.agu.org\/landslideblog\/2016\/11\/17\/hapuku-river-1\/\" rel=\"bookmark\">Hapuku River: a major landslide dam after the earthquake in New Zealand<\/a><\/li>\n<li class=\"posttitle srch\"><a title=\"Permanent Link to Comparing initial landslide reports: Tumbi Quarry, Papua New Guinea and Kaikora, New Zealand\" href=\"https:\/\/blogs.agu.org\/landslideblog\/2012\/02\/09\/comparing-initial-landslide-reports-tumbi-quarry-papua-new-guinea-and-kaikora-new-zealand\/\" rel=\"bookmark\">Comparing initial landslide reports: Tumbi Quarry, Papua New Guinea and Kaikora, New Zealand<\/a><\/li>\n<li class=\"posttitle srch\"><a title=\"Permanent Link to Landslides from the 2015 Wilberforce earthquake in New Zealand\" href=\"https:\/\/blogs.agu.org\/landslideblog\/2015\/02\/18\/wilberforce-earthquake-1\/\" rel=\"bookmark\">Landslides from the 2015 Wilberforce earthquake in New Zealand<\/a><\/li>\n<li class=\"posttitle srch\"><a title=\"Permanent Link to UBC distinguished lecture powerpoint file: Earthquake-induced landslides \u2013 lessons from Taiwan, Pakistan, China and New Zealand\" href=\"https:\/\/blogs.agu.org\/landslideblog\/2014\/03\/10\/ubc-lecture\/\" rel=\"bookmark\">UBC distinguished lecture powerpoint file: Earthquake-induced landslides \u2013 lessons from Taiwan, Pakistan, China and New Zealand<\/a><\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/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>Valkaniotis Sotiris of the University of Thessaloniki has posted a revised map of landslides triggered by the M=7.8 Kaikoura earthquake in New Zealand<!-- 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":20558,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[537],"tags":[23,469,1213,7],"class_list":["post-20553","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-earthquake-induced-landslide","tag-earthquake","tag-featured","tag-kaikoura","tag-new-zealand"],"_links":{"self":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/20553","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=20553"}],"version-history":[{"count":0,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/20553\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media\/20558"}],"wp:attachment":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media?parent=20553"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/categories?post=20553"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/tags?post=20553"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}