{"id":37373,"date":"2021-04-12T07:56:31","date_gmt":"2021-04-12T07:56:31","guid":{"rendered":"https:\/\/blogs.agu.org\/landslideblog\/?p=37373"},"modified":"2021-04-12T07:56:31","modified_gmt":"2021-04-12T07:56:31","slug":"culluchaca-landslide-2","status":"publish","type":"post","link":"https:\/\/blogs.agu.org\/landslideblog\/2021\/04\/12\/culluchaca-landslide-2\/","title":{"rendered":"The interesting morphology of the Culluchaca landslide in Peru"},"content":{"rendered":"

The interesting morphology of the Culluchaca landslide in Peru<\/h4>\n

After posting yesterday about the Culluchaca landslide in Peru<\/a>, I spent some time looking at the morphology of the site using the Google Earth Imagery.\u00a0 As a reminder, this\u00a0 is what the Google Earth images show.\u00a0 The image was collected in July 2019:-<\/p>\n

\"Google

Google Earth view of the site of the landslide close to Culluchaca in Peru.<\/p><\/div>\n

.<\/p>\n

The interesting features of this landslide lie above the crest of the slide shown above.\u00a0 The image below shows that area, on this occasion looking square onto the landslide:-<\/p>\n

\"Google

Google Earth view of the crest of the landslide close to Culluchaca in Peru.<\/p><\/div>\n

.<\/p>\n

The image appears to show two arrays of tension cracks.\u00a0 The first set, marked with A, are about 50 metres back from the landslide crown.\u00a0 But there is another set, marked with B, that are probably less well developed.\u00a0 These are about 150 metres back from the landslide crown, indicating a very large instability.<\/p>\n

Perhaps even more interesting is the set of features further across the slope.\u00a0 The image below shows the morphology of this area.\u00a0 I’ve left the other markers in place for reference:-<\/p>\n

\"Google

Google Earth view of features at the crest of the landslide close to Culluchaca in Peru.<\/p><\/div>\n

.<\/p>\n

Running across the slope parallel to the crest is an array of linear depressions, some of which are large and extensive.\u00a0 Upslope from here is a ridge with extensive bouldery deposits, which is probably a scarp.<\/p>\n

The most likely explanation for these features at that this is the site of a deep-seated gravitational deformation (DSGD)<\/em>, defined as<\/a> “a gravity-induced process affecting large portions of slopes evolving over very long periods of time. A DGSD may displace rock volumes of up to hundreds of millions of cubic meters, with thicknesses of up to a few hundred meters.”<\/em><\/p>\n

DSDGs are very large, slow creeping failures in rock masses, common in high mountain areas.\u00a0 I wrote about an example in Italy in 2019<\/a>.\u00a0 They typically generate arrays of parallel scarps and troughs high up on the hillside.<\/p>\n

Thus, the failure of the Culluchaca landslide on 7 April 2021 is probably only a small part of the unstable mass on this slope.\u00a0 However, that does not necessarily mean that further collapses are likely in the short term – DSGDs creep for hundreds and even thousands of years.<\/p>\n

I should note that an alternative explanation for these features in this landscape as an active fault.\u00a0 This possibility cannot be precluded without further investigation.<\/p>\n","protected":false},"excerpt":{"rendered":"

The interesting morphology of the Culluchaca landslide in Peru – is this part of a much larger deep-seated gravitational deformation (DSGD)?<\/p>\n","protected":false},"author":22,"featured_media":37378,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[598],"tags":[28139,29767,469,158,122],"class_list":["post-37373","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-landslide-processes","tag-deep-seated-gravitational-slope-deformation","tag-dsgd","tag-featured","tag-peru","tag-south-america"],"_links":{"self":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/37373","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=37373"}],"version-history":[{"count":0,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/37373\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media\/37378"}],"wp:attachment":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media?parent=37373"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/categories?post=37373"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/tags?post=37373"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}