{"id":30067,"date":"2019-02-07T08:26:30","date_gmt":"2019-02-07T08:26:30","guid":{"rendered":"https:\/\/blogs.agu.org\/landslideblog\/?p=30067"},"modified":"2019-02-07T08:26:30","modified_gmt":"2019-02-07T08:26:30","slug":"cape-kidnappers-1","status":"publish","type":"post","link":"https:\/\/blogs.agu.org\/landslideblog\/2019\/02\/07\/cape-kidnappers-1\/","title":{"rendered":"Cape Kidnappers: a succession of large rockslope failures in New Zealand"},"content":{"rendered":"

Cape Kidnappers: a succession of large rockslope failures in New Zealand<\/h4>\n

According to Wikipedia<\/a>, the delightfully named Cape Kidnappers is “a headland at the southeastern extremity of Hawke’s Bay on the east coast of New Zealand’s North Island and sits at the end of an 8 km peninsula which protrudes into the Pacific Ocean.”\u00a0 This is a stunning site that is renowned for bird life, especially gannets.\u00a0 On 23rd January 2019 Cape Kinappers site suffered a large rockslope failure, seriously injuring two people.\u00a0\u00a0 Reports suggest that the two victims were swept off the beach and into the sea<\/a> – it must have been a terrifying experience.<\/p>\n

There is some stunning imagery available of this large rockfall.\u00a0 Stuff has a lovely image of the deposit and the scar<\/a> for example:-<\/p>\n

\"Cape

The aftermath of the first large rockslope failure at Cape Kidnappers on 23rd January 2019. Image via Stuff.<\/a><\/p><\/div>\n

.<\/p>\n

There is also some excellent images of the rockslope failure at Cape Kidnappers.\u00a0 Stuff has this online as a video<\/a>, and Anusha Bradley<\/a> tweeted a video of the rockfall happening<\/a>:<\/p>\n

 <\/p>\n

\n

Tourist Denis Birnie captured this video of the slip pic.twitter.com\/1DfTaTsfUC<\/a><\/p>\n

\u2014 Anusha Bradley (@AnushaBradley) January 23, 2019<\/a><\/p><\/blockquote>\n

On 2nd February 2019 a further large collapse event occurred, with another significant chunk of the slope detaching.\u00a0 As with the first collapse, the failure appears to be a on\u00a0 a face-parallel detachment surface.\u00a0 A large block remains on the slope to the left of the original collapse; this must now be vulnerable to a failure event, suggesting that there will be a significant hazard at this site for a while:-<\/p>\n

 <\/p>\n

\"Cape

The aftermath of the second large rockslope failure at Cape Kidnappers on 2nd February 2019. Image via Stuff.<\/a><\/p><\/div>\n

.<\/p>\n

The geology of Cape Kidnappers consists of an alternating sequence of Middle Pleistocene shallow water sediments, primarily conglomerates and lignitic mudstones. These are weak rocks that are susceptible to weathering and undercutting (as can be seen on the right side of the images. Thus, significant rockslope failures are unsurprising.\u00a0 In many ways this event is similar to the chalk rockfalls seen on the southern coast of the UK<\/a>.<\/p>\n

 <\/p>\n","protected":false},"excerpt":{"rendered":"

On 23rd January & 2nd February 2019 Cape Kidnappers in New Zealand suffered large rockslope failures. The first, caught on video, seriously injured 2 people <\/p>\n","protected":false},"author":22,"featured_media":30071,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[3],"tags":[469,7,56,310],"class_list":["post-30067","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-landslide-report","tag-featured","tag-new-zealand","tag-rockfall","tag-rockslope-failure"],"_links":{"self":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/30067","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=30067"}],"version-history":[{"count":0,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/30067\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media\/30071"}],"wp:attachment":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media?parent=30067"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/categories?post=30067"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/tags?post=30067"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}