{"id":29016,"date":"2018-10-22T06:17:04","date_gmt":"2018-10-22T06:17:04","guid":{"rendered":"https:\/\/blogs.agu.org\/landslideblog\/?p=29016"},"modified":"2018-10-22T06:17:04","modified_gmt":"2018-10-22T06:17:04","slug":"yarlung-tsangpo-1-2","status":"publish","type":"post","link":"https:\/\/blogs.agu.org\/landslideblog\/2018\/10\/22\/yarlung-tsangpo-1-2\/","title":{"rendered":"Yarlung Tsangpo: a large valley blocking landslide in Tibet"},"content":{"rendered":"

Yarlung Tsangpo: a large valley blocking landslide in Tibet<\/h4>\n

Xinhua reports<\/a> that on Wednesday of last week (17th October 2018), a very large landslide occurred in Menling County in Tibet, blocking the Yarlung Tsangpo River.\u00a0 The volume of the barrier lake quickly increased, reaching a reported 300 million m\u00b3, and thus presenting a substantial hazard.\u00a0 Interestingly, this is the second barrier lake to form in Tibet in a short period, as on 11th October 2018 a further large, valley blocking landslide occurred at Bolo township in Jomda County<\/a>, also causing a substantial blockage.\u00a0 To have two large valley-blocking slides in such a short period of time is quite surprising.<\/p>\n

In the case of the Yarlung Tsangpao landslide, SANDRP reports<\/a> that the location is in the vicinity of 94.9375\u00b0 E, 29.7496\u00b0 N, although it recognises that there is some uncertainty in this position.\u00a0 Unfortunately at present there is too much cloud in the area to validate this with satellite imagery.<\/p>\n

Xinhua has this view of the landslide barrier<\/a>:-<\/p>\n

\"Yarlung

The landslide blocking the Yarlung Tsangpo river in Tibet. Image via Xinhua.<\/a><\/p><\/div>\n

.<\/p>\n

Initially the landslide caused a complete blockage of the Yarlung Tsangpo river, but the blockage has now breached.\u00a0 There is some evidence that the overtopping event caused flood damage downstream, but prompt evacuation of the downstream communities appears to have ensured that no lives were lost.\u00a0 This image, also from Xinhua<\/a>, shows the blockage prior to overtopping:-<\/p>\n

\"Yarlung

The valley-blocking landslide on the Yarlung Tsangpo river in Tiber. Image via Xinhua<\/a>,<\/p><\/div>\n

.<\/p>\n

This Xinhua image is particularly interesting<\/a>, showing the very lower reaches of the landslide deposit and the dried out riverbed:-<\/p>\n

\"Yarlung

The toe of the landslide at Yarlung Tsango in Tibet. Image via Xinhua<\/a>.<\/p><\/div>\n

.<\/p>\n

SANDRP quotes a researcher in the area<\/a> as indicating that this landslide might have been a glacial surge:-<\/p>\n

“A researcher who alerted India about the landslides along Yarlung Tsagpo in Dec 2017<\/a> said that the Sendapu glacier surged and wasted between September & 13th October, releasing debris that possibly led to the landslide.”<\/em><\/p>\n

Some sort of glacial event, possibly a rock and ice avalanche that flowed across the glacier surface, akin to the Siachen Glacier event in Pakistan in 2012<\/a>, appears to have been the cause.\u00a0 We will need satellite imagery to know for certain.<\/p>\n","protected":false},"excerpt":{"rendered":"

Last week a very large landslide occurred on the Yarlung Tsangpo river in Tibet, temporarily blocking the river. The dam has now breached.<\/p>\n","protected":false},"author":22,"featured_media":29020,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[3],"tags":[881,469,619,15,18126],"class_list":["post-29016","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-landslide-report","tag-east-asia","tag-featured","tag-glacier","tag-landslide-dam","tag-tiber"],"_links":{"self":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/29016","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=29016"}],"version-history":[{"count":0,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/29016\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media\/29020"}],"wp:attachment":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media?parent=29016"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/categories?post=29016"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/tags?post=29016"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}