{"id":32914,"date":"2020-01-29T07:26:04","date_gmt":"2020-01-29T07:26:04","guid":{"rendered":"https:\/\/blogs.agu.org\/landslideblog\/?p=32914"},"modified":"2020-01-29T07:26:04","modified_gmt":"2020-01-29T07:26:04","slug":"pumice-layers-in-the-2018-hokkaido-earthquake","status":"publish","type":"post","link":"https:\/\/blogs.agu.org\/landslideblog\/2020\/01\/29\/pumice-layers-in-the-2018-hokkaido-earthquake\/","title":{"rendered":"The role of weak pumice layers in landslides triggered by the M=6.7 6 September 2018 Hokkaido Iburi-Tobu Earthquake"},"content":{"rendered":"

The role of weak pumice layers in landslides triggered by the M=6.7 6 September 2018 Hokkaido Iburi-Tobu Earthquake<\/h4>\n

On 6 September 2018 the M=6.7\u00a0Hokkaido Iburi-Tobu earthquake triggered large numbers of landslides<\/a> in Japan.\u00a0 A subsequent analysis<\/a> (Yamagishi and Yamazaki 2018<\/a>) suggested indicated that over 6,000 landslides were triggered, resulting in 36 fatalities.\u00a0 They suggested that the exceptionally high landslide initiation rate probably resulted from high susceptibility of the local geology to earthquake shaking.<\/p>\n

\"06\/09\/2018

The area of intense landslides from the 06\/09\/2018 Hokkaido Iburi-Tobu earthquake. Image via Tokyo Keizai.<\/a><\/p><\/div>\n

In a new study, Li et al.<\/em> (2020<\/a>) have examined the role of weak pumice layers in the triggering of these landslides.\u00a0 The landslides occurred in an area of pyroclastic deposits from the various volcanoes located in the vicinity.\u00a0 Field mapping suggests that there is a particularly weak pumice layer, the so-called Ta-d strata, which dates from an eruption of Tarumae volcano about 8,700 to 10,000 years ago.\u00a0 The image below, from Li et al.<\/em> (2020<\/a>), shows the complex layering in these landslides, including the Ta-d pumice low down in the section.<\/p>\n

\"Landslides

A vertical section through one of the landslide scarps from the M=6.7 6 September 2018 Hokkaido Iburi-Tobu Earthquake. Image from Li et al.<\/em> (2020)<\/a>.<\/p><\/div>\n

.<\/p>\n

Li et al.<\/em> (2020<\/a>) consistently found that the Ta-d pumice layer acting at the sliding layer in the landslides triggered by this earthquake.\u00a0 They have undertaken a series of laboratory analyses of this material, finding that it is extremely susceptible to liquefaction<\/a>.\u00a0 They have concluded that a lower permeability palaeosol under the pumice layer enabled seepage parallel to the slope, which may have weakened this layer over time.\u00a0 When subjected to ground accelerations in excess of about 5 m\/s2<\/sup> the pumice layer underwent liquefaction, reducing shear strength to close to zero, allowing the slopes to fail.<\/p>\n

This paper provides an elegant explanation for the extensive landsliding that occurred in the M=6.7 Hokkaido Iburi-Tobu earthquake. As we found in our work in New Zealand (Massey et al.<\/em> 2013<\/a>), thin layers of weak volcanic materials can often control the susceptibility of slopes to failure.\u00a0 This is probably the most extreme version of this effect that I have seen to date.<\/p>\n

References<\/h4>\n

Li, R., Wang, F. & Zhang, S. 2020. Controlling role of Ta-d pumice on the coseismic landslides triggered by 2018 Hokkaido Eastern Iburi Earthquake<\/a>. Landslides<\/em> https:\/\/doi.org\/10.1007\/s10346-020-01349-y<\/a><\/p>\n

Massey, C.I., Petley, David and McSaveney, M.J. (2013) Patterns of movement in reactivated landslides<\/a>. Engineering Geology<\/em>, 159,<\/strong> 1-19.<\/span><\/p>\n

Yamagishi, H. & Yamazaki, F. 2018.\u00a0 Landslides by the 2018 Hokkaido Iburi-Tobu Earthquake on September 6<\/a>. Landslides<\/em><\/a>. https:\/\/doi.org\/10.1007\/s10346-018-1092-z<\/a>.<\/p>\n","protected":false},"excerpt":{"rendered":"

A new study (Li et al. 2020) has found that a specific weak pumice layer controlled landslides triggered by the M=6.7 September 2018 Hokkaido Iburi-Tobu earthquake <\/p>\n","protected":false},"author":22,"featured_media":32917,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1],"tags":[16802,23,881,469,361,17],"class_list":["post-32914","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-uncategorized","tag-coseismic-landslide","tag-earthquake","tag-east-asia","tag-featured","tag-japan","tag-research"],"_links":{"self":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/32914","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=32914"}],"version-history":[{"count":0,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/32914\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media\/32917"}],"wp:attachment":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media?parent=32914"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/categories?post=32914"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/tags?post=32914"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}