{"id":594,"date":"2022-07-01T12:46:32","date_gmt":"2022-07-01T11:46:32","guid":{"rendered":"https:\/\/monito.irpi.cnr.it\/caso-di-studio-mont-de-la-saxe\/"},"modified":"2023-03-13T18:22:00","modified_gmt":"2023-03-13T17:22:00","slug":"caso-di-studio-mont-de-la-saxe","status":"publish","type":"post","link":"https:\/\/monito.irpi.cnr.it\/fr\/caso-di-studio-mont-de-la-saxe\/","title":{"rendered":"Glissement de terrain du Mont de la Saxe"},"content":{"rendered":"\n<p>Le glissement de terrain du Mont de la Saxe (<a rel=\"noreferrer noopener\" href=\"https:\/\/monito.irpi.cnr.it\/wp-content\/uploads\/2022\/07\/FR-Scheda_Mont_de_la_Saxe_ED.pdf\" target=\"_blank\">download la fiche<\/a>) concerne un vaste secteur situ\u00e9 en amont imm\u00e9diat du village d\u2019Entr\u00e8ves, commune de Courmayeur (Aoste).<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><img decoding=\"async\" loading=\"lazy\" width=\"1024\" height=\"453\" src=\"https:\/\/monito.irpi.cnr.it\/wp-content\/uploads\/2022\/07\/Saxe-scheda-1024x453.jpg\" alt=\"\" class=\"wp-image-652\" srcset=\"https:\/\/monito.irpi.cnr.it\/wp-content\/uploads\/2022\/07\/Saxe-scheda-1024x453.jpg 1024w, https:\/\/monito.irpi.cnr.it\/wp-content\/uploads\/2022\/07\/Saxe-scheda-300x133.jpg 300w, https:\/\/monito.irpi.cnr.it\/wp-content\/uploads\/2022\/07\/Saxe-scheda-768x340.jpg 768w, https:\/\/monito.irpi.cnr.it\/wp-content\/uploads\/2022\/07\/Saxe-scheda.jpg 1223w\" sizes=\"(max-width: 1024px) 100vw, 1024px\" \/><\/figure>\n\n\n\n<p>Ce glissement est un des mouvements de terrain les plus importants de toutes les Alpes italiennes et implique des volumes rocheux tr\u00e8s \u00e9lev\u00e9s atteignant 8 millions de m\u00e8tres cubes. Sa r\u00e9activation constitue une menace pour les villages d\u2019Entr\u00e8ves et La Palud, c\u00e9l\u00e8bres localit\u00e9s<br>touristiques de montagne, ainsi que pour l\u2019acc\u00e8s au<br>tunnel transfrontalier du Mont Blanc.<\/p>\n\n\n\n<figure class=\"wp-block-image aligncenter size-large\"><img decoding=\"async\" loading=\"lazy\" width=\"1024\" height=\"687\" src=\"https:\/\/monito.irpi.cnr.it\/wp-content\/uploads\/2022\/07\/Saxe-1024x687.jpg\" alt=\"\" class=\"wp-image-571\" srcset=\"https:\/\/monito.irpi.cnr.it\/wp-content\/uploads\/2022\/07\/Saxe-1024x687.jpg 1024w, https:\/\/monito.irpi.cnr.it\/wp-content\/uploads\/2022\/07\/Saxe-300x201.jpg 300w, https:\/\/monito.irpi.cnr.it\/wp-content\/uploads\/2022\/07\/Saxe-768x515.jpg 768w, https:\/\/monito.irpi.cnr.it\/wp-content\/uploads\/2022\/07\/Saxe.jpg 1316w\" sizes=\"(max-width: 1024px) 100vw, 1024px\" \/><figcaption>Vue du front du glissement de terrain de Mont de la Saxe et d\u00e9limitation des zones \u00e0 dynamique \u00e9volutive diverse identifi\u00e9es (Photo Giordan D., CNR-IRPI si\u00e8ge de Turin)<\/figcaption><\/figure>\n\n\n\n<p>Actuellement, ce glissement de terrain est un des mouvements de terrain les plus surveill\u00e9s en Italie. En particulier, ce ph\u00e9nom\u00e8ne est observ\u00e9 \u00e0 l&rsquo;aide d\u2019un syst\u00e8me de surveillance int\u00e9gr\u00e9 constitu\u00e9 de plusieurs r\u00e9seaux d\u2019instruments destin\u00e9s \u00e0 mesurer les d\u00e9formations superficielles et profondes et \u00e0 transmettre les donn\u00e9es relev\u00e9es en continu afin de d\u00e9clencher en temps utile les syst\u00e8mes d\u2019alerte et d\u2019\u00e9mettre des bulletins p\u00e9riodiques aux fins des activit\u00e9s de protection civile.<\/p>\n\n\n\n<figure class=\"wp-block-image aligncenter size-large\"><img decoding=\"async\" loading=\"lazy\" width=\"1024\" height=\"971\" src=\"https:\/\/monito.irpi.cnr.it\/wp-content\/uploads\/2022\/07\/Saxe_spostamenti-1024x971.jpg\" alt=\"\" class=\"wp-image-573\" srcset=\"https:\/\/monito.irpi.cnr.it\/wp-content\/uploads\/2022\/07\/Saxe_spostamenti-1024x971.jpg 1024w, https:\/\/monito.irpi.cnr.it\/wp-content\/uploads\/2022\/07\/Saxe_spostamenti-300x284.jpg 300w, https:\/\/monito.irpi.cnr.it\/wp-content\/uploads\/2022\/07\/Saxe_spostamenti-768x728.jpg 768w, https:\/\/monito.irpi.cnr.it\/wp-content\/uploads\/2022\/07\/Saxe_spostamenti.jpg 1367w\" sizes=\"(max-width: 1024px) 100vw, 1024px\" \/><figcaption>Mouvements le long de la LOS reconstruits gr\u00e2ce \u00e0 l&rsquo;analyse des donn\u00e9es obtenues gr\u00e2ce \u00e0 l&rsquo;instrumentation de surveillance<\/figcaption><\/figure>\n","protected":false},"excerpt":{"rendered":"<p>Le glissement de terrain du Mont de la Saxe (download la fiche) concerne un vaste secteur situ\u00e9 en amont imm\u00e9diat du village d\u2019Entr\u00e8ves, commune de Courmayeur (Aoste). Ce glissement est un des mouvements de terrain les plus importants de toutes les Alpes italiennes et implique des volumes rocheux tr\u00e8s \u00e9lev\u00e9s atteignant 8 millions de m\u00e8tres cubes. Sa r\u00e9activation constitue une menace pour les villages d\u2019Entr\u00e8ves et La Palud, c\u00e9l\u00e8bres localit\u00e9stouristiques de montagne, ainsi que pour l\u2019acc\u00e8s autunnel transfrontalier du Mont Blanc. Actuellement, ce glissement de terrain est un des mouvements de terrain les plus surveill\u00e9s en Italie. En particulier, ce\u2026<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":[],"categories":[18],"tags":[],"blocksy_meta":{"styles_descriptor":{"styles":{"desktop":"","tablet":"","mobile":""},"google_fonts":[],"version":5}},"_links":{"self":[{"href":"https:\/\/monito.irpi.cnr.it\/fr\/wp-json\/wp\/v2\/posts\/594"}],"collection":[{"href":"https:\/\/monito.irpi.cnr.it\/fr\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/monito.irpi.cnr.it\/fr\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/monito.irpi.cnr.it\/fr\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/monito.irpi.cnr.it\/fr\/wp-json\/wp\/v2\/comments?post=594"}],"version-history":[{"count":3,"href":"https:\/\/monito.irpi.cnr.it\/fr\/wp-json\/wp\/v2\/posts\/594\/revisions"}],"predecessor-version":[{"id":674,"href":"https:\/\/monito.irpi.cnr.it\/fr\/wp-json\/wp\/v2\/posts\/594\/revisions\/674"}],"wp:attachment":[{"href":"https:\/\/monito.irpi.cnr.it\/fr\/wp-json\/wp\/v2\/media?parent=594"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/monito.irpi.cnr.it\/fr\/wp-json\/wp\/v2\/categories?post=594"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/monito.irpi.cnr.it\/fr\/wp-json\/wp\/v2\/tags?post=594"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}