{"id":35760,"date":"2020-12-14T08:12:45","date_gmt":"2020-12-14T08:12:45","guid":{"rendered":"https:\/\/blogs.agu.org\/landslideblog\/?p=35760"},"modified":"2020-12-14T08:12:45","modified_gmt":"2020-12-14T08:12:45","slug":"the-eureka-valley-landslide","status":"publish","type":"post","link":"https:\/\/blogs.agu.org\/landslideblog\/2020\/12\/14\/the-eureka-valley-landslide\/","title":{"rendered":"The Eureka Valley Landslide in Death Valley National Park"},"content":{"rendered":"

The Eureka Valley Landslide in Death Valley National Park<\/h4>\n

Way back in the mists of time, when this blog was fresh-faced, I wrote a brief piece about a very intriguing landslide in Death Valley National Park<\/a>.\u00a0 This feature, known as the Eureka Valley Landslide, is the beautifully-preserved preserved remains of an ancient long runout failure.\u00a0 It is very clear on Google Earth:-<\/p>\n

\"Eureka

Google Earth image of the Eureka Valley landslide in Death Valley National Park, California<\/p><\/div>\n

.<\/p>\n

I have placed the marker at the toe of the main lobe of the landslide, which is located at 37.076, -117.652.\u00a0 Note however that there is another lobe downslope of this point with a slightly different orientation – this is interpreted as being an outwash lobe.\u00a0 The runout distance for the main lobe is about 3.5 km.<\/p>\n

This landslide has just been described in a new paper published in the journal Lithosphere (Shaller et al.<\/em> 2020<\/a>).\u00a0 Many thanks to the authors for highlighting it to me.\u00a0 The authors have found that the landslide started with 5 million cubic metre detachment up in the steep terrain.\u00a0 The authors tentatively suggest that the landslide occurred about 100,000 years ago.<\/p>\n

The most interesting aspect of this study is the detailed sedimentology undertaken by the authors, which has allowed them to construct an interpretation of the likely movement mechanisms.\u00a0 In the early part of its movement, through the canyon system in the mountains, they suggest a “cataclasis mechanism” involving rock fragmentation and energy recycling.\u00a0 However, once out of the rugged terrain they suggest that the mechanism transitioned to a sliding mechanism enabled by liquefaction of the alluvium over which the landslide was moving. The image below provides a full overview of the landslide:-<\/p>\n

\"Eureka

An interpretation of the Eureka Valley landslide. Figure from Shaller et al.<\/em> (2020)<\/a>.<\/p><\/div>\n

.<\/p>\n

In broad terms this feels a bit like the change in mechanism that is seem in the Mount Dixon rock avalanche video<\/a>, where the landslide transitioned from an avalanche phase into sliding, in that case over ice.<\/p>\n

There is a huge amount of rich detail in the paper – it is worth a read.<\/p>\n

Reference<\/h4>\n

Shaller, P.J., Doroudian, M. and Hart, M.W. 2020. The Eureka Valley Landslide: Evidence of a Dual Failure Mechanism for a Long-Runout Landslide<\/a>. Lithosphere<\/em> 2020<\/strong> (1), 1\u201326. doi: https:\/\/doi.org\/10.2113\/2020\/8860819<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"

The Eureka Valley Landslide in Death Valley National Park: a new paper (Shaller et al. 2020) on a beautifully-preserved, ancient, long runout failure.<\/p>\n","protected":false},"author":22,"featured_media":35763,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[544],"tags":[137,469,725,192,306,30603,48],"class_list":["post-35760","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-review-of-a-paper","tag-california","tag-featured","tag-north-america","tag-paper","tag-rock-avalanche","tag-sedimentaology","tag-usa"],"_links":{"self":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/35760","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=35760"}],"version-history":[{"count":0,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/35760\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media\/35763"}],"wp:attachment":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media?parent=35760"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/categories?post=35760"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/tags?post=35760"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}