{"id":13744,"date":"2021-07-22T18:17:51","date_gmt":"2021-07-22T16:17:51","guid":{"rendered":"http:\/\/volcanx.cluster031.hosting.ovh.net\/?post_type=glossary&#038;p=13744"},"modified":"2021-07-26T17:24:59","modified_gmt":"2021-07-26T15:24:59","slug":"avalanche-debris-fr","status":"publish","type":"glossary","link":"https:\/\/volcanofoundation.org\/fr\/glossary\/avalanche-debris-fr\/","title":{"rendered":"AVALANCHE DE D\u00c9BRIS"},"content":{"rendered":"<p>Les masses mobiles de roches, de terre et de neige qui se produisent lorsque le flanc d&rsquo;une montagne ou d&rsquo;un volcan s&rsquo;effondre et glisse vers le bas de la pente.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Les masses mobiles de roches, de terre et de neige qui se produisent lorsque le flanc d&rsquo;une montagne ou d&rsquo;un volcan s&rsquo;effondre et glisse vers le bas de la pente.<\/p>\n","protected":false},"author":8,"featured_media":0,"menu_order":0,"template":"","meta":{"footnotes":""},"class_list":["post-13744","glossary","type-glossary","status-publish","hentry"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/volcanofoundation.org\/fr\/wp-json\/wp\/v2\/glossary\/13744","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/volcanofoundation.org\/fr\/wp-json\/wp\/v2\/glossary"}],"about":[{"href":"https:\/\/volcanofoundation.org\/fr\/wp-json\/wp\/v2\/types\/glossary"}],"author":[{"embeddable":true,"href":"https:\/\/volcanofoundation.org\/fr\/wp-json\/wp\/v2\/users\/8"}],"version-history":[{"count":0,"href":"https:\/\/volcanofoundation.org\/fr\/wp-json\/wp\/v2\/glossary\/13744\/revisions"}],"wp:attachment":[{"href":"https:\/\/volcanofoundation.org\/fr\/wp-json\/wp\/v2\/media?parent=13744"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}