{"id":1183,"date":"2026-06-03T12:18:52","date_gmt":"2026-06-03T10:18:52","guid":{"rendered":"https:\/\/lessciensonautes.fr\/?p=1183"},"modified":"2026-06-07T23:56:31","modified_gmt":"2026-06-07T21:56:31","slug":"documentaire-photo-eboulis","status":"publish","type":"post","link":"https:\/\/lessciensonautes.fr\/?p=1183","title":{"rendered":"Documentaire photo \u00e9boulis"},"content":{"rendered":"\n<style>\n\n\/* =========================\n   DOSSIER PHOTO SCIENSONAUTES\n   PARTIE 1\n========================= *\/\n\n@import url('https:\/\/fonts.googleapis.com\/css2?family=Caveat:wght@500;700&family=Special+Elite&display=swap');\n\n.sc-photo{\nmax-width:1100px;\nmargin:auto;\nfont-family:Georgia,serif;\ncolor:#2d2d2d;\nline-height:1.8;\n}\n\n.sc-photo *{\nbox-sizing:border-box;\n}\n\n\/* ---------- EN-T\u00caTE ---------- *\/\n\n.sc-header{\nbackground:#f5f1e7;\nborder:3px solid #c8baa0;\npadding:35px;\nmargin:30px 0;\nposition:relative;\nbox-shadow:0 8px 20px rgba(0,0,0,.08);\n}\n\n.sc-stamp{\nposition:absolute;\nright:20px;\ntop:30px;\nborder:3px solid #b64242;\ncolor:#b64242;\npadding:10px 18px;\nfont-weight:bold;\ntransform:rotate(8deg);\nfont-size:14px;\nletter-spacing:2px;\n}\n\n.sc-kicker{\nfont-family:'Special Elite',monospace;\nletter-spacing:2px;\nfont-size:13px;\ntext-transform:uppercase;\ncolor:#6f6758;\n}\n\n.sc-title{\nfont-size:38px;\nfont-weight:700;\nmargin:15px 0;\nline-height:1.2;\n}\n\n.sc-subtitle{\nfont-family:'Special Elite',monospace;\nfont-size:14px;\ntext-transform:uppercase;\nletter-spacing:2px;\ncolor:#666;\n}\n\n.sc-intro{\nbackground:white;\npadding:30px;\nborder-left:6px solid #8f7856;\nmargin-top:25px;\n}\n\n\/* ---------- SECTION ---------- *\/\n\n.sc-section{\nmargin:80px 0;\nposition:relative;\n}\n\n.sc-doc-label{\ndisplay:inline-block;\nbackground:#263648;\ncolor:white;\npadding:10px 18px;\nfont-family:'Special Elite',monospace;\nletter-spacing:1px;\nfont-size:14px;\nmargin-bottom:20px;\n}\n\n.sc-doc-title{\nfont-size:30px;\nfont-weight:700;\nmargin-bottom:35px;\n}\n\n\/* ---------- POLAROID ---------- *\/\n\n.sc-polaroid{\nbackground:white;\npadding:15px 15px 60px;\nbox-shadow:0 12px 25px rgba(0,0,0,.15);\ntransform:rotate(-2deg);\nmargin-bottom:35px;\nposition:relative;\n}\n\n.sc-polaroid img{\nwidth:100%;\ndisplay:block;\nborder-radius:2px;\n}\n\n.sc-note{\nposition:absolute;\nbottom:18px;\nleft:25px;\nfont-family:'Caveat',cursive;\nfont-size:28px;\ncolor:#444;\n}\n\n.sc-paperclip{\nposition:absolute;\ntop:-12px;\nright:35px;\nfont-size:40px;\ntransform:rotate(20deg);\n}\n\n\/* ---------- CARTES ---------- *\/\n\n.sc-card{\nbackground:#fffdf8;\nborder:1px solid #ddd4bf;\npadding:25px;\nmargin:25px 0;\nbox-shadow:0 5px 15px rgba(0,0,0,.05);\n}\n\n.sc-card h4{\nmargin-top:0;\nfont-size:22px;\n}\n\n.sc-observation{\nborder-left:6px solid #8f7856;\n}\n\n.sc-geologue{\nborder-left:6px solid #396a9e;\nbackground:#f4f8fc;\n}\n\n\/* ---------- BLOC CARNET ---------- *\/\n\n.sc-fieldnote{\nbackground:#fff9ea;\nborder:1px dashed #bba87f;\npadding:18px;\nmargin-top:20px;\nfont-family:'Caveat',cursive;\nfont-size:28px;\n}\n\n\/* ---------- S\u00c9PARATEUR ---------- *\/\n\n.sc-sep{\ntext-align:center;\nfont-size:26px;\ncolor:#8a8a8a;\nmargin:60px 0;\n}\n\n<\/style>\n\n<div class=\"sc-photo\">\n\n<div class=\"sc-header\">\n\n<div class=\"sc-stamp\">\nARCHIVE VALID\u00c9E\n<\/div>\n\n<div class=\"sc-kicker\">\nDOSSIER PHOTOGRAPHIQUE DE TERRAIN\n<\/div>\n\n<h1 class=\"sc-title\">\n\u00c9BOULIS OBSERV\u00c9S EN MONTAGNE\n<\/h1>\n\n<div class=\"sc-subtitle\">\nARCHIVE SCIENSONAUTES \u2014 DOCUMENT COMPL\u00c9MENTAIRE\n<\/div>\n\n<div class=\"sc-intro\">\n\n<p>\nLorsqu&#8217;on observe une montagne de loin, elle semble immobile et \u00e9ternelle.\nPourtant, les g\u00e9ologues savent que les reliefs sont en transformation permanente.\n<\/p>\n\n<p>\nLes photographies qui suivent montrent de v\u00e9ritables \u00e9boulis observ\u00e9s dans diff\u00e9rentes r\u00e9gions montagneuses du monde.\nChaque image r\u00e9v\u00e8le les traces d&#8217;un travail lent mais incessant : la fragmentation progressive de la roche sous l&#8217;action du gel, de l&#8217;eau, de la gravit\u00e9 et du temps.\n<\/p>\n\n<\/div>\n\n<\/div>\n\n\n<!-- DOCUMENT 1 -->\n\n<section class=\"sc-section\">\n\n<div class=\"sc-doc-label\">\nDOCUMENT PHOTO N\u00b01\n<\/div>\n\n<h2 class=\"sc-doc-title\">\n\u00c9boulis au pied d&#8217;une falaise alpine\n<\/h2>\n\n<div class=\"sc-polaroid\">\n\n<div class=\"sc-paperclip\">\ud83d\udcce<\/div>\n\n<img decoding=\"async\" src=\"https:\/\/monde.ccdmd.qc.ca\/media\/image1024\/47732.jpg\">\n\n<div class=\"sc-note\">\nRelev\u00e9 de terrain n\u00b0184\n<\/div>\n\n<\/div>\n\n<div class=\"sc-card sc-observation\">\n\n<h4>\ud83d\udd0d Observation<\/h4>\n\n<p>\nDes milliers de blocs rocheux recouvrent le pied de la falaise.\nLa plupart de ces roches se sont d\u00e9tach\u00e9es progressivement au cours des hivers successifs.\n<\/p>\n\n<p>\nL&#8217;eau s&#8217;est infiltr\u00e9e dans les fissures, a gel\u00e9 puis a agrandi ces fractures jusqu&#8217;\u00e0 provoquer la rupture des blocs.\n<\/p>\n\n<\/div>\n\n<div class=\"sc-card sc-geologue\">\n\n<h4>\ud83e\uddd1\u200d\ud83d\udd2c Ce que remarquent les g\u00e9ologues<\/h4>\n\n<p>\nLa taille tr\u00e8s vari\u00e9e des roches indique que la falaise continue encore aujourd&#8217;hui \u00e0 produire de nouveaux fragments.\n<\/p>\n\n<\/div>\n\n<div class=\"sc-fieldnote\">\n\ud83d\udccd Processus dominant : g\u00e9lifraction + gravit\u00e9\n<\/div>\n\n<\/section>\n\n\n<!-- DOCUMENT 2 -->\n\n<section class=\"sc-section\">\n\n<div class=\"sc-doc-label\">\nDOCUMENT PHOTO N\u00b02\n<\/div>\n\n<h2 class=\"sc-doc-title\">\nFissures dans une paroi rocheuse de haute montagne\n<\/h2>\n\n<div class=\"sc-polaroid\" style=\"transform:rotate(2deg);\">\n\n<div class=\"sc-paperclip\">\ud83d\udcce<\/div>\n\n<img decoding=\"async\" src=\"https:\/\/images.openai.com\/static-rsc-4\/BuGNXJFJCYE1GvadRCtAJWM3uWprsYX8yq2IRmRNOS8qafGVuPiLCfIhBt8I9T0KmyDwDYqv9InpmTe1Xm7eZh0ZK3GRUCZLPSbABI5TfcgCqZXrdgQsFYISvmpqFYtcbPL3VdUU8pQ7HaYmlkQHl8nMvjlQfoNB-RY70Okq91FtjZQNUmpfX1G7qO3MvS0L?purpose=fullsize\">\n\n<div class=\"sc-note\">\nParoi inspect\u00e9e au lever du jour\n<\/div>\n\n<\/div>\n\n<div class=\"sc-card sc-observation\">\n\n<h4>\ud83d\udd0d Observation<\/h4>\n\n<p>\n\u00c0 premi\u00e8re vue, la paroi semble solide.\nPourtant, plusieurs fissures traversent la roche.\n<\/p>\n\n<p>\nCertaines ne mesurent que quelques millim\u00e8tres de large mais peuvent s&#8217;\u00e9tendre sur plusieurs m\u00e8tres.\n<\/p>\n\n<\/div>\n\n<div class=\"sc-card sc-geologue\">\n\n<h4>\ud83e\uddd1\u200d\ud83d\udd2c Ce que remarquent les g\u00e9ologues<\/h4>\n\n<p>\nCes fissures constituent les points faibles de la montagne.\nLorsque l&#8217;eau y p\u00e9n\u00e8tre puis g\u00e8le, elles s&#8217;\u00e9largissent lentement.\n<\/p>\n\n<\/div>\n\n<div class=\"sc-fieldnote\">\n\u270f\ufe0f Chaque fissure repr\u00e9sente une future ligne de rupture potentielle.\n<\/div>\n\n<\/section>\n\n\n<!-- DOCUMENT 3 -->\n\n<section class=\"sc-section\">\n\n<div class=\"sc-doc-label\">\nDOCUMENT PHOTO N\u00b03\n<\/div>\n\n<h2 class=\"sc-doc-title\">\nChamp d&#8217;\u00e9boulis sous un sommet escarp\u00e9\n<\/h2>\n\n<div class=\"sc-polaroid\">\n\n<div class=\"sc-paperclip\">\ud83d\udcce<\/div>\n\n<img decoding=\"async\" src=\"https:\/\/images.openai.com\/static-rsc-4\/D9eh5roNubGf_RkKl99lKWWF-QevWwDVwJhzGNVgIoAUmyPXO5M4SDtSmbAqvwpRihZyfpjvDCde4jLkn9fdmKsUW24y5EV2WqU543Aqe-0HKrGWBqyRzaVg7ngDS-MXVhRIcjI5bZOHjBlzvmn1eKnE5C30Sqz7i1l0lX6Vd3GSg5HNtVNlxLJmS1asRlEy?purpose=fullsize\">\n\n<div class=\"sc-note\">\nAccumulation observ\u00e9e sur versant nord\n<\/div>\n\n<\/div>\n\n<div class=\"sc-card sc-observation\">\n\n<h4>\ud83d\udd0d Observation<\/h4>\n\n<p>\nLa pente est recouverte d&#8217;une immense accumulation de blocs.\nCe type de paysage est appel\u00e9 un champ d&#8217;\u00e9boulis.\n<\/p>\n\n<p>\nChaque pierre visible provient autrefois de la montagne situ\u00e9e au-dessus.\n<\/p>\n\n<\/div>\n\n<div class=\"sc-card sc-geologue\">\n\n<h4>\ud83e\uddd1\u200d\ud83d\udd2c Ce que remarquent les g\u00e9ologues<\/h4>\n\n<p>\nL&#8217;\u00e9tude de ces d\u00e9p\u00f4ts permet parfois de reconstituer l&#8217;histoire de l&#8217;\u00e9rosion d&#8217;un versant pendant plusieurs milliers d&#8217;ann\u00e9es.\n<\/p>\n\n<\/div>\n\n<div class=\"sc-fieldnote\">\n\ud83e\udea8 Chaque bloc constitue un fragment de l&#8217;histoire de la montagne.\n<\/div>\n\n<\/section>\n\n<\/div>\n\n<!-- DOCUMENT 4 -->\n\n<section class=\"sc-section\">\n\n<div class=\"sc-doc-label\">\nDOCUMENT PHOTO N\u00b04\n<\/div>\n\n<h2 class=\"sc-doc-title\">\nBloc r\u00e9cemment d\u00e9tach\u00e9\n<\/h2>\n\n<div class=\"sc-polaroid\" style=\"transform:rotate(-3deg);\">\n\n<div class=\"sc-paperclip\">\ud83d\udcce<\/div>\n\n<img decoding=\"async\" src=\"https:\/\/ichef.bbci.co.uk\/images\/ic\/1920xn\/p0fb8h8g.jpg.webp\">\n\n<div class=\"sc-note\">\nCassure fra\u00eeche observ\u00e9e sur le terrain\n<\/div>\n\n<\/div>\n\n<div class=\"sc-card sc-observation\">\n\n<h4>\ud83d\udd0d Observation<\/h4>\n\n<p>\nLa surface claire du bloc indique une cassure relativement r\u00e9cente.\nLes roches expos\u00e9es depuis longtemps prennent souvent une couleur plus sombre sous l&#8217;effet du climat.\n<\/p>\n\n<\/div>\n\n<div class=\"sc-card sc-geologue\">\n\n<h4>\ud83e\uddd1\u200d\ud83d\udd2c Ce que remarquent les g\u00e9ologues<\/h4>\n\n<p>\nLes diff\u00e9rences de couleur permettent parfois d&#8217;estimer quels \u00e9boulements sont r\u00e9cents et lesquels sont beaucoup plus anciens.\n<\/p>\n\n<\/div>\n\n<div class=\"sc-fieldnote\">\n\ud83d\udccc La teinte claire sugg\u00e8re une rupture r\u00e9cente de la paroi.\n<\/div>\n\n<\/section>\n\n<div class=\"sc-sep\"> <\/div>\n\n<!-- DOCUMENT 5 -->\n\n<section class=\"sc-section\">\n\n<div class=\"sc-doc-label\">\nDOCUMENT PHOTO N\u00b05\n<\/div>\n\n<h2 class=\"sc-doc-title\">\n\u00c9boulis observ\u00e9 dans une vall\u00e9e glaciaire\n<\/h2>\n\n<div class=\"sc-polaroid\" style=\"transform:rotate(2deg);\">\n\n<div class=\"sc-paperclip\">\ud83d\udcce<\/div>\n\n<img decoding=\"async\" src=\"https:\/\/images.openai.com\/static-rsc-4\/mVI-9URRCDtp0IVL9ac-Nlym3-x5T9o8CDKGfEm_GaDtIegI4yTgT1ZCjztPk1d4ead1Onldl5h1qil--sdiHnwhc5IXc2_BBDCsKkHuQ7YpcRz5fov9j7vubDneTGJgIv1L8XUXzll83gi5Au3PlWuc4v8vn_5GMN--ycwANGEJDn6gG3mxkvTyBQU6ON0_?purpose=fullsize\">\n\n<div class=\"sc-note\">\nAncienne vall\u00e9e fa\u00e7onn\u00e9e par les glaciers\n<\/div>\n\n<\/div>\n\n<div class=\"sc-card sc-observation\">\n\n<h4>\ud83d\udd0d Observation<\/h4>\n\n<p>\nLes anciens glaciers ont laiss\u00e9 derri\u00e8re eux des parois abruptes particuli\u00e8rement sensibles \u00e0 la g\u00e9lifraction.\nM\u00eame apr\u00e8s la disparition de la glace, les falaises continuent \u00e0 se fragmenter.\n<\/p>\n\n<\/div>\n\n<div class=\"sc-card sc-geologue\">\n\n<h4>\ud83e\uddd1\u200d\ud83d\udd2c Ce que remarquent les g\u00e9ologues<\/h4>\n\n<p>\nCertaines vall\u00e9es connaissent encore aujourd&#8217;hui des chutes de pierres r\u00e9guli\u00e8res li\u00e9es aux cycles gel-d\u00e9gel.\n<\/p>\n\n<\/div>\n\n<div class=\"sc-fieldnote\">\n\u2744\ufe0f H\u00e9ritage glaciaire encore visible plusieurs milliers d&#8217;ann\u00e9es apr\u00e8s le retrait des glaces.\n<\/div>\n\n<\/section>\n\n\n<!-- ANALYSE DE TERRAIN -->\n\n<section class=\"sc-section\">\n\n<div class=\"sc-doc-label\">\nANALYSE DE TERRAIN\n<\/div>\n\n<div class=\"sc-card\" style=\"background:#f7f4eb;\">\n\n<h3 style=\"margin-top:0;font-size:28px;\">\n\ud83e\uddd1\u200d\ud83d\udd2c Synth\u00e8se des observations\n<\/h3>\n\n<p>\nLes photographies pr\u00e9c\u00e9dentes montrent que les \u00e9boulis ne sont pas les cons\u00e9quences d&#8217;un unique \u00e9v\u00e9nement spectaculaire.\n<\/p>\n\n<p>\nDans la majorit\u00e9 des cas, ils r\u00e9sultent d&#8217;une accumulation de petits changements r\u00e9p\u00e9t\u00e9s pendant des centaines, parfois des milliers d&#8217;ann\u00e9es.\n<\/p>\n\n<p>\nChaque hiver ajoute de nouvelles fissures.\nChaque cycle gel-d\u00e9gel fragilise un peu plus la roche.\nChaque chute de bloc modifie lentement le paysage.\n<\/p>\n\n<\/div>\n\n<div style=\"\nbackground:white;\npadding:35px;\nborder:2px dashed #b9b09d;\nmargin-top:35px;\ntext-align:center;\nfont-size:24px;\nline-height:2.2;\n\">\n\n<img decoding=\"async\" src=\"https:\/\/lessciensonautes.fr\/wp-content\/uploads\/2026\/06\/24394CE9-ADB2-4D06-8107-DD9F8B6DDB0A.png\">\n\n<\/div>\n\n<div class=\"sc-fieldnote\" style=\"margin-top:25px;\">\nObservation g\u00e9n\u00e9rale : la montagne semble immobile \u00e0 l&#8217;\u00e9chelle humaine mais \u00e9volue continuellement \u00e0 l&#8217;\u00e9chelle g\u00e9ologique.\n<\/div>\n\n<\/section>\n\n<div class=\"sc-sep\">. <\/div>\n\n<!-- CONCLUSION -->\n\n<section class=\"sc-section\">\n\n<div class=\"sc-doc-label\">\nCONCLUSION SCIENTIFIQUE\n<\/div>\n\n<div class=\"sc-card\">\n\n<p>\nUne montagne ne s&#8217;effondre pas d&#8217;un seul coup.\nLa plupart du temps, sa transformation est progressive.\n<\/p>\n\n<p>\nLes \u00e9boulis observ\u00e9s aujourd&#8217;hui sont les t\u00e9moins visibles d&#8217;un processus g\u00e9ologique discret mais extr\u00eamement puissant.\n<\/p>\n\n<p>\nIls rappellent que m\u00eame les reliefs les plus imposants sont continuellement fa\u00e7onn\u00e9s par l&#8217;eau, la temp\u00e9rature, la gravit\u00e9 et le temps.\n<\/p>\n\n<\/div>\n\n<\/section>\n\n\n<!-- CLASSEMENT -->\n\n<section class=\"sc-section\">\n\n<div style=\"\nbackground:#f1ece0;\nborder:3px solid #cbbfa6;\npadding:30px;\nposition:relative;\n\">\n\n<div style=\"\nposition:absolute;\ntop:20px;\nright:20px;\nborder:3px solid #b64242;\npadding:10px 18px;\ncolor:#b64242;\nfont-weight:bold;\ntransform:rotate(8deg);\n\">\nCLASS\u00c9\n<\/div>\n\n<h2 style=\"\nmargin-top:0;\nfont-family:'Special Elite',monospace;\nletter-spacing:2px;\n\">\nCLASSEMENT DE L&#8217;ARCHIVE\n<\/h2>\n\n<table style=\"\nwidth:100%;\nborder-collapse:collapse;\nmargin-top:20px;\n\">\n\n<tbody><tr>\n<td style=\"padding:12px;border-bottom:1px solid #d7cfbe;\"><strong>Dossier<\/strong><\/td>\n<td style=\"padding:12px;border-bottom:1px solid #d7cfbe;\">\u00c9boulis de montagne<\/td>\n<\/tr>\n\n<tr>\n<td style=\"padding:12px;border-bottom:1px solid #d7cfbe;\"><strong>Statut<\/strong><\/td>\n<td style=\"padding:12px;border-bottom:1px solid #d7cfbe;\">V\u00e9rifi\u00e9 par observations de terrain<\/td>\n<\/tr>\n\n<tr>\n<td style=\"padding:12px;border-bottom:1px solid #d7cfbe;\"><strong>Classification<\/strong><\/td>\n<td style=\"padding:12px;border-bottom:1px solid #d7cfbe;\">Alt\u00e9ration des reliefs<\/td>\n<\/tr>\n\n<tr>\n<td style=\"padding:12px;\"><strong>R\u00e9f\u00e9rence<\/strong><\/td>\n<td style=\"padding:12px;\">ARCH-SCI-GEO-EB-001<\/td>\n<\/tr>\n\n<\/tbody><\/table>\n\n<\/div>\n\n<div class=\"sc-fieldnote\" style=\"margin-top:30px;\">\n\ud83d\udcc1 Fin du dossier \u2014 Archive conserv\u00e9e dans les collections Sciensonautes.\n<\/div>\n\n<\/section>\n\n\n\n<style data-wp-block-html=\"css\">\n.scn-end-btn{\nmargin-top:80px;\ntext-align:center;\n}\n\n.scn-end-link{\ndisplay:inline-block;\npadding:14px 28px;\nborder-radius:999px;\nborder:2px solid #0f172a;\nbackground:white;\ncolor:#0f172a !important;\nfont-weight:800;\ntext-decoration:none !important;\nletter-spacing:.5px;\ntransition:.3s;\n}\n\n.scn-end-link:hover{\ntransform:translateY(-3px);\nbackground:#0f172a;\ncolor:white !important;\n}\n<\/style>\n\n<div class=\"scn-end-btn\">\n  <a href=\"https:\/\/lessciensonautes.fr\/?p=1122\" class=\"scn-end-link\">\n    \u2190 Retour \u00e0 l&#8217;exp\u00e9rience\n  <\/a>\n<\/div>\n","protected":false},"excerpt":{"rendered":"<p>ARCHIVE VALID\u00c9E DOSSIER PHOTOGRAPHIQUE DE TERRAIN \u00c9BOULIS OBSERV\u00c9S EN MONTAGNE ARCHIVE SCIENSONAUTES \u2014 DOCUMENT COMPL\u00c9MENTAIRE Lorsqu&#8217;on observe une montagne de loin, elle semble immobile et \u00e9ternelle. Pourtant, les g\u00e9ologues savent que les reliefs sont en transformation permanente. Les photographies qui suivent montrent de v\u00e9ritables \u00e9boulis observ\u00e9s dans diff\u00e9rentes r\u00e9gions montagneuses du monde. Chaque image r\u00e9v\u00e8le&#8230;<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_kad_post_transparent":"","_kad_post_title":"hide","_kad_post_layout":"fullwidth","_kad_post_sidebar_id":"","_kad_post_content_style":"","_kad_post_vertical_padding":"","_kad_post_feature":"","_kad_post_feature_position":"","_kad_post_header":false,"_kad_post_footer":false,"_kad_post_classname":"","footnotes":""},"categories":[1],"tags":[],"class_list":["post-1183","post","type-post","status-publish","format-standard","hentry","category-uncategorized"],"_links":{"self":[{"href":"https:\/\/lessciensonautes.fr\/index.php?rest_route=\/wp\/v2\/posts\/1183","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/lessciensonautes.fr\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/lessciensonautes.fr\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/lessciensonautes.fr\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/lessciensonautes.fr\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=1183"}],"version-history":[{"count":10,"href":"https:\/\/lessciensonautes.fr\/index.php?rest_route=\/wp\/v2\/posts\/1183\/revisions"}],"predecessor-version":[{"id":1312,"href":"https:\/\/lessciensonautes.fr\/index.php?rest_route=\/wp\/v2\/posts\/1183\/revisions\/1312"}],"wp:attachment":[{"href":"https:\/\/lessciensonautes.fr\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=1183"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/lessciensonautes.fr\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=1183"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/lessciensonautes.fr\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=1183"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}