{"id":4044,"date":"2018-10-08T08:52:24","date_gmt":"2018-10-08T06:52:24","guid":{"rendered":"http:\/\/wp.unil.ch\/risk\/?p=4044"},"modified":"2023-12-06T11:03:09","modified_gmt":"2023-12-06T10:03:09","slug":"inventory-of-shallow-and-spontaneous-landslides-and-improvement-of-the-methodology-to-establish-hazard-and-risk-maps-for-the-canton-of-vaud","status":"publish","type":"post","link":"https:\/\/wp.unil.ch\/risk\/inventory-of-shallow-and-spontaneous-landslides-and-improvement-of-the-methodology-to-establish-hazard-and-risk-maps-for-the-canton-of-vaud\/","title":{"rendered":"Inventory of shallow and spontaneous landslides and improvement of the methodology to establish hazard and risk maps for the Canton of Vaud"},"content":{"rendered":"

On contrary to hazards which have defined return time for establishing natural hazard maps (for example rock falls or floods), there is no similar methodology for shallow and spontaneous landslides. One way to improve the current methodology is proposed by Cedric Meier,  Marc-Henri Derron, Michel Jaboyedoff from RISK-UNIL and Christian Gerber, Veronica Artigue and Melanie Pigeon from the Vaud county administration. It includes the definition of 7 pilots zones based in Jura, Plateau and Alps, on riverbanks or mountain slopes. Based on the new airborne LiDAR acquisition, a former inventory from 1889 to 2013 and basics documents such as geological and topographical maps, air photos, about 110 landslides were registered.<\/span><\/span><\/p>\n

\"\"<\/a>Shallow landslide in the area of Ollon in 2018<\/em><\/p>\n

The parameters of the source zone of the landslide, like length, width, estimated depth, area, slope angle and propagation angle (Farb\u00f6schung) were recorded. For each landslide, 3 different volumes (with half-ellipsoid method, elliptical paraboloid <\/span><\/span>method and Sloping Local Base Level or SLBL method, method developed and applied currently at the Institute of Earth Sciences, ISTE \u2013 UNIL) were calculated. A volume-frequency distribution, approximated by the Power Law site specific, but also depending on the slope type was developed. Figures showing the probability of the estimated depth or the volume depending on the area of the source zone were also prepared. For the propagation, only 4 % of the landslide have a propagation angle greater than 13\u00b0.<\/span><\/p>\n

 \"\"<\/a>
\nProbability of max depth in function of the surface area of the landslide<\/em><\/span><\/span><\/p>\n

REFERENCES<\/span><\/span><\/p>\n

Jaboyedoff M., & Derron M.-H. 2005: A new method to estimate the infilling of alluvial sediment of glacial <\/span><\/span>valleys using a Sloping Local Base Level, Geogr.Fis.Dinam. Quat., 28, 37-46. 
\n<\/span><\/span>VD (2017) : <\/span>https:\/\/www.geo.vd.ch\/theme\/dangers_nat_thm<\/span><\/a><\/p>\n","protected":false},"excerpt":{"rendered":"

On contrary to hazards which have defined return time for establishing natural hazard maps (for example rock falls or floods), there is no similar methodology for shallow and spontaneous landslides. … <\/p>\n","protected":false},"author":1405,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_seopress_robots_primary_cat":"","_seopress_titles_title":"","_seopress_titles_desc":"","_seopress_robots_index":"","ngg_post_thumbnail":0,"footnotes":""},"categories":[1,75192,81],"tags":[75202,75203],"class_list":{"0":"post-4044","1":"post","2":"type-post","3":"status-publish","4":"format-standard","6":"category-blog","7":"category-mhs-corner","8":"category-news","9":"tag-marc-h","10":"tag-news"},"_links":{"self":[{"href":"https:\/\/wp.unil.ch\/risk\/wp-json\/wp\/v2\/posts\/4044","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/wp.unil.ch\/risk\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/wp.unil.ch\/risk\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/wp.unil.ch\/risk\/wp-json\/wp\/v2\/users\/1405"}],"replies":[{"embeddable":true,"href":"https:\/\/wp.unil.ch\/risk\/wp-json\/wp\/v2\/comments?post=4044"}],"version-history":[{"count":1,"href":"https:\/\/wp.unil.ch\/risk\/wp-json\/wp\/v2\/posts\/4044\/revisions"}],"predecessor-version":[{"id":6027,"href":"https:\/\/wp.unil.ch\/risk\/wp-json\/wp\/v2\/posts\/4044\/revisions\/6027"}],"wp:attachment":[{"href":"https:\/\/wp.unil.ch\/risk\/wp-json\/wp\/v2\/media?parent=4044"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/wp.unil.ch\/risk\/wp-json\/wp\/v2\/categories?post=4044"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/wp.unil.ch\/risk\/wp-json\/wp\/v2\/tags?post=4044"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}