{"id":27301,"date":"2018-04-03T02:52:31","date_gmt":"2018-04-03T02:52:31","guid":{"rendered":"https:\/\/blogs.agu.org\/landslideblog\/?p=27301"},"modified":"2018-04-03T02:52:31","modified_gmt":"2018-04-03T02:52:31","slug":"bssa-mw-7-8-kaikoura-earthquake-1","status":"publish","type":"post","link":"https:\/\/blogs.agu.org\/landslideblog\/2018\/04\/03\/bssa-mw-7-8-kaikoura-earthquake-1\/","title":{"rendered":"Landslides triggered by the 14 November 2016 Mw 7.8 Kaikoura Earthquake, New Zealand"},"content":{"rendered":"<h4>Landslides triggered by the 14 November 2016 Mw 7.8 Kaikoura Earthquake, New Zealand<\/h4>\n<div id=\"attachment_27306\" style=\"width: 310px\" class=\"wp-caption alignleft\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-27306\" class=\"wp-image-27306 size-medium\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2018\/04\/IMG_0257-300x200.jpg\" alt=\"Mw 7.8 Kaikoura earthquake\" width=\"300\" height=\"200\" \/><p id=\"caption-attachment-27306\" class=\"wp-caption-text\">Examples of landslides triggered by the Mw 7.8 Kaikoura Earthquake<\/p><\/div>\n<p>The 14 November 2016 <a href=\"https:\/\/blogs.agu.org\/landslideblog\/2016\/11\/20\/geonet-1\/\">Mw 7.8 Kaikoura Earthquake in New Zealand<\/a> was one of the most significant seismic events in terms of landslide triggering in recent years.\u00a0 <a href=\"https:\/\/blogs.agu.org\/landslideblog\/2016\/11\/14\/kaikoura-earthquake-1\/\">I have written about this earthquake<\/a>, <a href=\"https:\/\/blogs.agu.org\/landslideblog\/2017\/09\/14\/seafront-landslide\/\">and its landslides<\/a>, on a <a href=\"https:\/\/blogs.agu.org\/landslideblog\/2017\/09\/21\/valley-blocking-slips\/\">number of occasions<\/a>.\u00a0 In the months since the earthquake a large team has been involved in constructing an inventory of landslides from this event, and in analysing it. A first description of this inventory, and analysis of the landslides associated with the earthquake has now been published (<a href=\"https:\/\/pubs.geoscienceworld.org\/ssa\/bssa\/article\/529881\/landslides-triggered-by-the-14-november-2016-mw-7\">Massey <em>et al.<\/em> 2018<\/a>) in the <a href=\"https:\/\/pubs.geoscienceworld.org\/bssa\"><em>Bulletin of the Seismological Society of America<\/em><\/a>.\u00a0 I have to declare an interest &#8211; I am a co-author on this paper.<\/p>\n<p><a href=\"https:\/\/pubs.geoscienceworld.org\/ssa\/bssa\/article\/529881\/landslides-triggered-by-the-14-november-2016-mw-7\">Massey <em>et al.<\/em> (2018<\/a>) demonstrate that the earthquake generated over 10,000 mappable landslides (the inventory described was under development when we wrote the paper, so this total may well increase) over an area of about 10,000 km\u00b2. Neither the number of landslides nor the area over which they occurred are surprisingly high; indeed if anything the number is low when compared with other events in New Zealand and with global landslide inventories.\u00a0 <a href=\"https:\/\/blogs.agu.org\/landslideblog\/2017\/09\/16\/hapuku-landslide\/\">The largest landslide, on the Hapuku River<\/a>, had a volume of about 20 million m\u00b3 and ran out over a distance of about 2.7 km.<\/p>\n<p>The map below shows the distribution of the landslides triggered by the Mw 7.8 Kaikoura Earthquake, as mapped by <a href=\"https:\/\/pubs.geoscienceworld.org\/ssa\/bssa\/article\/529881\/landslides-triggered-by-the-14-november-2016-mw-7\">Massey <em>et al.<\/em> (2018<\/a>). \u00a0 The fault ruptures that generated the earthquake are also shown; note that this was a highly complex seismic event that involved the near-simultaneous rupture of multiple faults and fault segments.\u00a0 The resultant landslide distribution is also highly complex.<\/p>\n<div id=\"attachment_27305\" style=\"width: 650px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-27305\" class=\"wp-image-27305 size-full\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2018\/04\/18_04-Kaikoura-1-e1522721796836.jpg\" alt=\"Mw 7.8 Kaikoura earthquake\" width=\"640\" height=\"638\" \/><p id=\"caption-attachment-27305\" class=\"wp-caption-text\">The distribution of landslides from the Mw 7.8 Kaikoura Earthquake in 2016. Figure from Massey et al. (2018)<\/p><\/div>\n<p>.<\/p>\n<p>I think there are two really interesting aspects of the landslides mapped by\u00a0<a href=\"https:\/\/pubs.geoscienceworld.org\/ssa\/bssa\/article\/529881\/landslides-triggered-by-the-14-november-2016-mw-7\">Massey <em>et al.<\/em> (2018<\/a>). First, the density of landslides triggered by the\u00a0Mw 7.8 Kaikoura Earthquake was highest close to the fault &#8211; indeed our model of the landslide distribution suggests that the distance to the fault rupture was a better predictor of landslides than either the modeled peak ground acceleration or peak ground velocity. It is not clear as to whether this means that the distance function is capturing a key parameter in cosieismic landslide initiation (if so, what is it?) or that the models of peak ground acceleration and peak ground velocity are not capturing reality well. Indeed\u00a0<a href=\"https:\/\/pubs.geoscienceworld.org\/ssa\/bssa\/article\/529881\/landslides-triggered-by-the-14-november-2016-mw-7\">Massey <em>et al.<\/em> (2018<\/a>) found that the landslide density within 200\u00a0m of a mapped surface fault rupture was, on average, three times that of locations at a distance of 2500\u00a0m.<\/p>\n<p>And second, <a href=\"https:\/\/pubs.geoscienceworld.org\/ssa\/bssa\/article\/529881\/landslides-triggered-by-the-14-november-2016-mw-7\">Massey <em>et al.<\/em> (2018<\/a>) found that the point density of landslides for the coastal slopes was much higher than that for inland slopes in similar materials. This may well indicate that more active erosion has meant that the coastal slopes are more out of equilibrium with the environment when compared with the inland slopes.<\/p>\n<h4>Reference<\/h4>\n<p>C. Massey, D. Townsend, E. Rathje, K. E. Allstadt, B. Lukovic, Y. Kaneko, B. Bradley, J. Wartman, R. W. Jibson, D. N. Petley, N. Horspool, I. Hamling, J. Carey, S. Cox, J. Davidson, S. Dellow, J. W. Godt, C. Holden, K. Jones, A. Kaiser, M. Little, B. Lyndsell, S. McColl, R. Morgenstern, F. K. Rengers, D. Rhoades, B. Rosser, D. Strong, C. Singeisen, M. Villeneuve. 2018. <a href=\"https:\/\/pubs.geoscienceworld.org\/ssa\/bssa\/article\/529881\/landslides-triggered-by-the-14-november-2016-mw-7\">Landslides Triggered by the 14 November 2016 <span class=\"inline-formula no-formula-id\"><span id=\"MathJax-Element-2-Frame\" class=\"MathJax\" role=\"presentation\"><span id=\"MathJax-Span-6\" class=\"math\"><span id=\"MathJax-Span-7\" class=\"mrow\"><span id=\"MathJax-Span-8\" class=\"msub\"><span id=\"MathJax-Span-9\" class=\"mi\">M<\/span><span id=\"MathJax-Span-10\" class=\"mi\">w<\/span><\/span><\/span><\/span><\/span><\/span>\u00a07.8 Kaikoura Earthquake, New Zealand<\/a>. <em>Bulletin of the Seismological Society of America<\/em> doi: <a href=\"https:\/\/doi.org\/10.1785\/0120170305\" target=\"_blank\" rel=\"noopener\">https:\/\/doi.org\/10.1785\/0120170305<\/a><\/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>In a new paper, Massey et al (2018) describe initial maps of the landslides triggered by the 2016 Mw 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":27305,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[537,544],"tags":[23,469,1213,7],"class_list":["post-27301","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-earthquake-induced-landslide","category-review-of-a-paper","tag-earthquake","tag-featured","tag-kaikoura","tag-new-zealand"],"_links":{"self":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/27301","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=27301"}],"version-history":[{"count":0,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/27301\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media\/27305"}],"wp:attachment":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media?parent=27301"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/categories?post=27301"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/tags?post=27301"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}