{"id":10037,"date":"2014-06-19T07:59:29","date_gmt":"2014-06-19T07:59:29","guid":{"rendered":"http:\/\/blogs.agu.org\/landslideblog\/?p=10037"},"modified":"2014-06-19T07:59:29","modified_gmt":"2014-06-19T07:59:29","slug":"devdoraki-1","status":"publish","type":"post","link":"https:\/\/blogs.agu.org\/landslideblog\/2014\/06\/19\/devdoraki-1\/","title":{"rendered":"The Devdoraki landslide: a new set of high quality images"},"content":{"rendered":"
The Devdoraki Landslide<\/b><\/h5>\n

The Devdoraki landslide was a large event in the Dariali Valley in Georgia<\/a> that blocked the main road between Russia and Georgia a month ago.\u00a0 I featured some images of the landslide at the time<\/a>, but (via Jorg Hanisch), I have been provided with a new set of very high quality photographs of the landslide.\u00a0 These images were collected by Georgy Gotsiridze of the Consulting Center “GeoGraphic”, Tbilisi, Georgia, who has made them available for free use.\u00a0 They are remarkable.<\/p>\n

This is the source zone of the Devdoraki landslide:<\/p>\n

\"Devdoraki\"<\/a>

Image copyright of Georgy Gotsiridze, used with permission<\/p><\/div>\n

..<\/p>\n

Note the failure appears to have started as a rock mass failure on a very steep, ice-covered slope.\u00a0 This then appears to have entrained a very large volume of material as it loved down the steep slope.\u00a0 The dynamics are complex though – on the left side of the flow as seen from the camera the slide has spilled over a rock spur to create a second slide.\u00a0 Down-slope this merges again with the main slide, as shown in this image:<\/p>\n

\"Devdoraki\"<\/a>

Image copyright of Georgy Gotsiridze, used with permission<\/p><\/div>\n

..<\/p>\n

The most dramatic aspect of this image through is the extraordinary super-elevation of the slide when it reached the foot of the steepest slope and then needed to turn 90 degrees to follow the valley.\u00a0 Super-elevation is the term used when the slide travels up a slope, typically because of a sharp turn.\u00a0 On the right side of the image this super-elevation is very clear.\u00a0 This indicates that the landslide was travelling very fast at this point.\u00a0 The super-elevation is better illustrated in this image, showing the entire upper portion of the landslide:<\/p>\n

\"Devdoraki\"<\/a>

Image copyright of Georgy Gotsiridze, used with permission<\/p><\/div>\n

..<\/p>\n

Interestingly, from this point onwards the character of the slide appears to have changed markedly, I assume from a rock avalanche to a rapid debris flow.\u00a0 This is an image of the track of the landslide in the lower reaches:<\/p>\n

\"Devdoraki\"<\/a>

Image copyright of Georgy Gotsiridze, used with permission<\/p><\/div>\n

..<\/p>\n

There is some evidence of super-elevation on the outside of the bend, but to nothing like the extent upslope.\u00a0 The flow appears to have been strongly channelized in this portion.\u00a0 This is supported by this image of the slide, taken from a lower angle:<\/p>\n

\"Devdoraki\"<\/a>

Image copyright of Georgy Gotsiridze, used with permission<\/p><\/div>\n

..<\/p>\n

Finally, this is the landslide deposit at the point that it entered the main channel and stopped:<\/p>\n

\"Devdoraki\"<\/a>

Image copyright of Georgy Gotsiridze, used with permission<\/p><\/div>\n

..<\/p>\n

The diversion channel, which flowed into a tunnel, is clearly evident.\u00a0 The landslide does not seem to have traveled far, or to have spread dramatically, once it entered the main channel.\u00a0 There is little evidence of super-elevation as well.\u00a0 This supports the hypothesis that the movement rate was notably lower than for the initial stages.<\/p>\n

This is a very unusual and interesting landslide – I hope that it will be analyzed and written up in detail.<\/p>\n","protected":false},"excerpt":{"rendered":"

Amazing new images have been made available of the Devdoraki landslide, which affected the Dariali Valley in Georgia a month ago<\/p>\n","protected":false},"author":22,"featured_media":10040,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[69,1],"tags":[469,563,983,959,306,546],"class_list":["post-10037","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-landslide-images","category-uncategorized","tag-featured","tag-georgia","tag-landslide-images","tag-landslide-report","tag-rock-avalanche","tag-russia"],"_links":{"self":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/10037","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=10037"}],"version-history":[{"count":0,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/10037\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media\/10040"}],"wp:attachment":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media?parent=10037"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/categories?post=10037"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/tags?post=10037"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}