{"id":36950,"date":"2021-03-09T08:38:23","date_gmt":"2021-03-09T08:38:23","guid":{"rendered":"https:\/\/blogs.agu.org\/landslideblog\/?p=36950"},"modified":"2021-03-09T08:38:23","modified_gmt":"2021-03-09T08:38:23","slug":"ebisu-circuit","status":"publish","type":"post","link":"https:\/\/blogs.agu.org\/landslideblog\/2021\/03\/09\/ebisu-circuit\/","title":{"rendered":"Ebisu Circuit: an intriguing landslide caused by the 2021 Fukushima Earthquake"},"content":{"rendered":"

Ebisu Circuit: an intriguing landslide caused by the 2021 Fukushima Earthquake<\/h4>\n

On 13 February 2021 the M=7.3 2021 Fukushima Earthquake<\/a> (also known as the Fukushima-ken Oki (Fukushima Prefecture Offshore) earthquake) struck eastern Japan<\/a>.\u00a0 This earthquake killed one person and injured around 185 people, and caused some structural damage and landslides.<\/p>\n

The most interesting landslide occurred at Ebisu Circuit<\/a>, a motor racing track located in the hills near to Nihonmatsu in Fukushima Prefecture.\u00a0 This landslide did not cause any loss of life but it has inflicted considerable damage to the track.\u00a0 The best overview image that I can find is this one, from Reuters:-<\/p>\n

\"The

An aerial view of the landslide caused by a strong earthquake at the Ebisu Circuit in Nihonmatsu, Fukushima Prefecture, Japan on February 14, 2021 in this photo taken by Kyodo. Image:Kyodo\/via REUTERS and The Japan Times<\/a>.<\/p><\/div>\n

.<\/p>\n

Meanwhile, Sankei.com has an alternative view looking up the length of the length of the landslide<\/a>:<\/p>\n

\"The

The track of the Ebisu Circuit landslide. Image from Sankei.com<\/a><\/p><\/div>\n

.<\/p>\n

On first inspection I assumed that this would be a fill slope failure associated with material emplaced to create the small circuit at the top of the slope.\u00a0 However, This image of the top of the slope, tweeted by @tarokote<\/a>, suggests that this is not the case:<\/p>\n

\"The

The crown of the slope failure at Ebisu Circuit. Image tweeted by @tarokote<\/a>.<\/p><\/div>\n

.<\/p>\n

There is no evidence of a fill slope, and indeed the failure is shallow and slope parallel along its length – almost the epitome of an infinite slope failure.\u00a0 It is slightly deeper on the right side than on the left, which is an interesting feature.<\/p>\n

There is a short article, in Japanese, about the geology of this failure, posted by the Geological Society of Japan<\/a>.\u00a0 Google Translate<\/a> suggests that it says (I have modified the language a little, and abridged it):-<\/p>\n

Regarding the geology near this place, there is a wind formation layer of about 10 m containing many tephras originating from Adatara volcano that covers the surface layer. Below that are the early Pleistocene debris avalanche deposits (Fd) with a thickness of several meters to 10 meters, and below that are the rhyolite pyroclastic rocks and lava (M2r) of the Middle Miocene Iwakura Formation.\u00a0<\/em><\/p>\n

It is certain that at least the surface wind layer slipped down at the collapse of this point. It is necessary to wait for a field survey to find out where the slip surface is between the Iwakura Formation and the Fushiogami debris avalanche deposit, or in the pumice layer of the Fuse Formation, which contains many tephras.<\/em><\/p>\n

It is known that similar surface collapses of the wind formation including the tephra layer occurred at three sites in Shirakawa City, Fukushima Prefecture during the 2011 Tohoku Taihei-oki Earthquake, resulting in 14 deaths and missing persons.<\/em><\/p>\n

So, it appears that the landslide at Ebisu Circuit is a failure in a volcanic soil formed from tephra (volcanic materials such as ash).\u00a0 These materials appear to have formed a flow that has had a high level of mobility.<\/p>\n","protected":false},"excerpt":{"rendered":"

Ebisu Circuit: an intriguing, high mobility landslide in volcanic materials caused by the 2021 Fukushima Earthquake in Japan<\/p>\n","protected":false},"author":22,"featured_media":36955,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[537],"tags":[16802,23,469,30624,30623],"class_list":["post-36950","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-earthquake-induced-landslide","tag-coseismic-landslide","tag-earthquake","tag-featured","tag-tephra","tag-volcanic"],"_links":{"self":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/36950","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=36950"}],"version-history":[{"count":0,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/36950\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media\/36955"}],"wp:attachment":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media?parent=36950"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/categories?post=36950"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/tags?post=36950"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}