{"id":3479,"date":"2011-08-05T21:14:04","date_gmt":"2011-08-05T21:14:04","guid":{"rendered":"http:\/\/blogs.agu.org\/landslideblog\/?p=3479"},"modified":"2011-08-06T23:31:08","modified_gmt":"2011-08-06T23:31:08","slug":"landslides-from-the-christchurch-earthquakes-part-4-large-scale-cliff-collapses","status":"publish","type":"post","link":"https:\/\/blogs.agu.org\/landslideblog\/2011\/08\/05\/landslides-from-the-christchurch-earthquakes-part-4-large-scale-cliff-collapses\/","title":{"rendered":"Landslides from the Christchurch earthquakes part 4: large-scale cliff collapses"},"content":{"rendered":"

The other parts of this series may be found here:<\/p>\n

Part one: boulder damage to a house<\/a><\/p>\n

Part two: evil dancing rocks<\/a><\/p>\n

Part three: topographic amplification at the cliff tops<\/a><\/p>\n

Part four: large-scale cliff collapses<\/a><\/p>\n

Part five: landslides that involve sliding<\/a><\/p>\n

In the Christchurch earthquakes there were a number of large-scale rock collapses in the areas to the south-east of the city.\u00a0 These events caused a small number of fatalities and considerable damage.\u00a0 At the lower end of the scale were some isolated rock detachments, albeit involving large blocks:<\/p>\n

\"\"<\/a><\/p>\n

However, the real story is with some very large cliff collapses that have driven retreat of the clifftop by ten metres or more.\u00a0 These two image show two of these very large collapse sites.\u00a0 Note the inundation of the land at the toe of the slopes and the proximity of some buildings to the debris:<\/p>\n

\"\"<\/a>\"\"<\/a><\/p>\n

The impacts on properties at the top of the cliff has been severe.\u00a0 In some cases, houses have already been partially or completely destroyed as a result of the rockfalls:<\/p>\n

\"\"<\/a><\/p>\n

In others, blocks that have partially detached, but not yet failed, have opened huge cracks that have profoundly damaged properties.\u00a0 In some cases these blocks extend tens of metres back from the clifftop, leaving a long-term legacy of severe hazard.\u00a0 This house for example has one of these cracks extending through the living room:<\/p>\n

\"\"<\/a><\/p>\n

This house is also on one such block.\u00a0 The lower part of the house is being pulled apart as it moves:<\/p>\n

\"\"<\/a><\/p>\n

Meanwhile, this house is entirely on such a block, such that the deformation is occurring in the patio on the road side of the building as the structure is being pulled forwards:<\/p>\n

\"\"<\/a><\/p>\n

Finally, these cracks of course mean that there is a huge volume if potentially unstable material that threatens roads and buildings at the toe of the slope.\u00a0 As an emergency measure, shipping containers are being used to provide protection:<\/p>\n

\"\"<\/a><\/p>\n

<\/a>\"\"<\/a><\/p>\n

The next part of this series should follow tomorrow.\u00a0 It will look at conventional landslides triggered by the earthquake.\u00a0 On Monday I will post some images of the ruined city centre.<\/p>\n

The other posts in this series are as follows:<\/p>\n

Part one: boulder damage to a house<\/a><\/p>\n

Part two: evil dancing rocks<\/a><\/p>\n

Part three: topographic amplification at the cliff tops<\/a><\/p>\n

Part four: large-scale cliff collapses<\/a><\/p>\n

Part five: landslides that involve sliding<\/a><\/p>\n

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

Part four in the series posts examining landslides from the Christchurch earthquakes. This edition looks at large-scale cliff collapses.<\/p>\n","protected":false},"author":22,"featured_media":3482,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[537],"tags":[23,469,21,7,56],"class_list":["post-3479","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-earthquake-induced-landslide","tag-earthquake","tag-featured","tag-images","tag-new-zealand","tag-rockfall"],"_links":{"self":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/3479","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=3479"}],"version-history":[{"count":0,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/3479\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media\/3482"}],"wp:attachment":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media?parent=3479"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/categories?post=3479"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/tags?post=3479"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}