{"id":850,"date":"2025-11-30T15:53:33","date_gmt":"2025-11-30T14:53:33","guid":{"rendered":"https:\/\/schweiz.blog\/?p=850"},"modified":"2026-03-19T14:23:35","modified_gmt":"2026-03-19T13:23:35","slug":"la-geologie-suisse-expliquee-simplement","status":"publish","type":"post","link":"https:\/\/schweiz.blog\/fr\/geologie-schweiz-einfach-erklaert\/","title":{"rendered":"La g\u00e9ologie de la Suisse expliqu\u00e9e simplement"},"content":{"rendered":"<p class=\"wp-block-paragraph\">Le <strong>G\u00e9ologie de la Suisse<\/strong> Il est unique au monde. Trois grandes unit\u00e9s g\u00e9ologiques se rencontrent sur une superficie tr\u00e8s r\u00e9duite\u00a0: <strong>Alpes<\/strong>, <strong>Plateau central<\/strong> et <strong>Loi<\/strong>. Chaque r\u00e9gion poss\u00e8de sa propre histoire g\u00e9ologique, ses types de roches et ses reliefs caract\u00e9ristiques. Cet article explique la structure g\u00e9ologique de la Suisse de mani\u00e8re simple et compr\u00e9hensible.<\/p>\n\n\n\n<h1 class=\"wp-block-heading\"><strong>1. La Suisse est une mosa\u00efque g\u00e9ologique.<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">La Suisse se situe au milieu de la zone o\u00f9 <strong>plaques tectoniques africaines et eurasiennes<\/strong> Une collision a donn\u00e9 naissance aux Alpes et continue d&#039;influencer le paysage actuel.<\/p>\n\n\n\n<figure class=\"wp-block-image\"><img data-recalc-dims=\"1\" decoding=\"async\" src=\"https:\/\/i0.wp.com\/www.researchgate.net\/publication\/271200275\/figure\/fig1\/AS%3A295018574172161%401447349317740\/The-interaction-between-the-Africa-and-Eurasia-plates-generates-a-diffuse-area-of.png?w=1200&#038;ssl=1\" alt=\"https:\/\/www.researchgate.net\/publication\/271200275\/figure\/fig1\/AS%3A295018574172161%401447349317740\/The-interaction-between-the-Africa-and-Eurasia-plates-generates-a-diffuse-area-of.png\"\/><\/figure>\n\n\n\n<figure class=\"wp-block-image\"><img decoding=\"async\" src=\"https:\/\/www.researchgate.net\/publication\/285851152\/figure\/fig2\/AS%3A1061380111233024%401630064146080\/Tectonic-setting-of-the-Carpathian-Basin-in-the-collision-zone-of-the-Eurasian-and.ppm\" alt=\"https:\/\/www.researchgate.net\/publication\/285851152\/figure\/fig2\/AS%3A1061380111233024%401630064146080\/Tectonic-setting-of-the-Carpathian-Basin-in-the-collision-zone-of-the-Eurasian-and.ppm\"\/><\/figure>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Source:<\/strong> <a href=\"https:\/\/www.britannica.com\/science\/plate-tectonics\" target=\"_blank\" rel=\"noopener\">https:\/\/www.britannica.com\/science\/plate-tectonics<\/a><\/p>\n\n\n\n<p class=\"wp-block-paragraph\">La pression des deux plaques a pouss\u00e9 des masses rocheuses l&#039;une sur l&#039;autre, les a pliss\u00e9es et a entra\u00een\u00e9 de forts soul\u00e8vements.<\/p>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<h1 class=\"wp-block-heading\"><strong>2. Les Alpes \u2013 la plus jeune cha\u00eene de montagnes de Suisse<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">Les Alpes se sont form\u00e9es par les <strong>Collision des plaques africaine et eurasienne<\/strong> \u00e0 propos <strong>30 \u00e0 5 millions d&#039;ann\u00e9es<\/strong>. Au cours de ce processus, des roches plus anciennes provenant de l&#039;ancien oc\u00e9an T\u00e9thys ont \u00e9t\u00e9 pouss\u00e9es vers le haut.<\/p>\n\n\n\n<figure class=\"wp-block-image\"><img data-recalc-dims=\"1\" decoding=\"async\" src=\"https:\/\/i0.wp.com\/www.researchgate.net\/publication\/284820689\/figure\/fig2\/AS%3A646753867030528%401531209546670\/Cross-section-of-the-western-Alps-on-a-western-Switzerland-transect-and-simplified.png?w=1200&#038;ssl=1\" alt=\"https:\/\/www.researchgate.net\/publication\/284820689\/figure\/fig2\/AS%3A646753867030528%401531209546670\/Cross-section-of-the-western-Alps-on-a-western-Switzerland-transect-and-simplified.png\"\/><\/figure>\n\n\n\n<figure class=\"wp-block-image\"><img data-recalc-dims=\"1\" decoding=\"async\" src=\"https:\/\/i0.wp.com\/www.researchgate.net\/publication\/358138717\/figure\/fig4\/AS%3A1118621979938816%401643711671031\/Composite-geological-cross-sections-across-the-Alps-a-section-traces-and-estimated.png?w=1200&#038;ssl=1\" alt=\"https:\/\/www.researchgate.net\/publication\/358138717\/figure\/fig4\/AS%3A1118621979938816%401643711671031\/Composite-geological-cross-sections-across-the-Alps-a-section-traces-and-estimated.png\"\/><\/figure>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Source:<\/strong> <a href=\"https:\/\/www.britannica.com\/place\/Alps\" target=\"_blank\" rel=\"noopener\">https:\/\/www.britannica.com\/place\/Alps<\/a><\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Roches typiques des Alpes<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Gneis<\/strong><\/li>\n\n\n\n<li><strong>granit<\/strong><\/li>\n\n\n\n<li><strong>ardoise<\/strong><\/li>\n\n\n\n<li><strong>calcaire<\/strong><\/li>\n<\/ul>\n\n\n\n<h2 class=\"wp-block-heading\">Caract\u00e9ristiques<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>plus hauts sommets de Suisse<\/li>\n\n\n\n<li>vall\u00e9es escarp\u00e9es<\/li>\n\n\n\n<li>La formation active de montagnes se poursuit encore aujourd&#039;hui.<\/li>\n\n\n\n<li>de nombreux glaciers (en recul, mais influents)<\/li>\n<\/ul>\n\n\n\n<p class=\"wp-block-paragraph\">Les Alpes sont constitu\u00e9es de plusieurs unit\u00e9s tectoniques telles que les <strong>Massif d&#039;Aar<\/strong>, <strong>Massif du Saint-Gothard<\/strong>, <strong>P\u00e9nin<\/strong>, <strong>Helv\u00e9tique<\/strong> etc.<\/p>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<h1 class=\"wp-block-heading\"><strong>3. Le Plateau suisse \u2013 la d\u00e9pression g\u00e9ologique situ\u00e9e entre les Alpes et le Jura<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">Le <strong>Plateau suisse<\/strong> Il s&#039;agit d&#039;une vaste d\u00e9pression qui s&#039;est remplie de d\u00e9p\u00f4ts lors de la formation des Alpes. Elle a \u00e9t\u00e9 cr\u00e9\u00e9e par le poids et la pression des Alpes lors de leur soul\u00e8vement \u00e0 cette \u00e9poque.<\/p>\n\n\n\n<figure class=\"wp-block-image\"><img data-recalc-dims=\"1\" decoding=\"async\" src=\"https:\/\/i0.wp.com\/nagra.ch\/wp-content\/uploads\/2025\/06\/Geologie-der-Schweiz_neu_en.webp?w=1200&#038;ssl=1\" alt=\"https:\/\/nagra.ch\/wp-content\/uploads\/2025\/06\/Geologie-der-Schweiz_neu_en.webp\"\/><\/figure>\n\n\n\n<figure class=\"wp-block-image\"><img data-recalc-dims=\"1\" decoding=\"async\" src=\"https:\/\/i0.wp.com\/nagra.ch\/wp-content\/uploads\/2025\/06\/Geologisches-Profil-der-Schweiz_neu_en.webp?w=1200&#038;ssl=1\" alt=\"https:\/\/nagra.ch\/wp-content\/uploads\/2025\/06\/Geologisches-Profil-der-Schweiz_neu_en.webp\"\/><\/figure>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Source:<\/strong> <a><a href=\"https:\/\/www.swisstopo.admin.ch\" rel=\"nofollow\">https:\/\/www.swisstopo.admin.ch<\/a><\/a><\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Roches typiques du plateau suisse<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>M\u00e9lasse<\/strong> (Gr\u00e8s, marne, conglom\u00e9rats)<\/li>\n\n\n\n<li>s\u00e9diments r\u00e9cents provenant des rivi\u00e8res et des lacs<\/li>\n<\/ul>\n\n\n\n<h2 class=\"wp-block-heading\">Caract\u00e9ristiques<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>plaines fertiles<\/li>\n\n\n\n<li>douces collines<\/li>\n\n\n\n<li>dens\u00e9ment peupl\u00e9<\/li>\n\n\n\n<li>La r\u00e9gion agricole et \u00e9conomique la plus importante de Suisse<\/li>\n<\/ul>\n\n\n\n<p class=\"wp-block-paragraph\">La molasse provient des mat\u00e9riaux \u00e9rod\u00e9s des Alpes \u00e9mergentes et s&#039;est d\u00e9pos\u00e9e en vastes champs de d\u00e9bris.<\/p>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<h1 class=\"wp-block-heading\"><strong>4. Les monts Jura \u2013 une ancienne cha\u00eene de montagnes pliss\u00e9es compos\u00e9e de calcaire<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">Le <strong>Loi<\/strong> G\u00e9ologiquement, elle est bien plus ancienne que les Alpes. Elle se compose principalement de <strong>calcaire<\/strong>, Cette couche g\u00e9ologique s&#039;est d\u00e9pos\u00e9e dans la mer il y a plus de 150 millions d&#039;ann\u00e9es. Sous la pression des Alpes, elle a \u00e9t\u00e9 pliss\u00e9e vers le nord.<\/p>\n\n\n\n<figure class=\"wp-block-image\"><img data-recalc-dims=\"1\" decoding=\"async\" src=\"https:\/\/i0.wp.com\/www.researchgate.net\/publication\/316716976\/figure\/fig89\/AS%3A638819250487296%401529317786330\/Geology-of-the-Jura-Mountains-around-the-Mont-Terri-Rock-Laboratory-area-modified-after.png?w=1200&#038;ssl=1\" alt=\"https:\/\/www.researchgate.net\/publication\/316716976\/figure\/fig89\/AS%3A638819250487296%401529317786330\/Geology-of-the-Jura-Mountains-around-the-Mont-Terri-Rock-Laboratory-area-modified-after.png\"\/><\/figure>\n\n\n\n<figure class=\"wp-block-image\"><img data-recalc-dims=\"1\" decoding=\"async\" src=\"https:\/\/i0.wp.com\/nagra.ch\/wp-content\/uploads\/2025\/06\/Geologisches-Profil-der-Schweiz_neu_en.webp?w=1200&#038;ssl=1\" alt=\"https:\/\/nagra.ch\/wp-content\/uploads\/2025\/06\/Geologisches-Profil-der-Schweiz_neu_en.webp\"\/><\/figure>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Source:<\/strong> <a href=\"https:\/\/www.britannica.com\/place\/Jura-Mountains\" target=\"_blank\" rel=\"noopener\">https:\/\/www.britannica.com\/place\/Jura-Mountains<\/a><\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Roches typiques du Jurassique<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>calcaire<\/li>\n\n\n\n<li>marne<\/li>\n\n\n\n<li>argile<\/li>\n<\/ul>\n\n\n\n<h2 class=\"wp-block-heading\">Caract\u00e9ristiques<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>plis doux et allong\u00e9s (g\u00e9n\u00e9ralement en forme d&#039;antenne dans les montagnes du Jura)<\/li>\n\n\n\n<li>de nombreuses grottes (paysages karstiques)<\/li>\n\n\n\n<li>vastes for\u00eats<\/li>\n\n\n\n<li>Plateaux et vall\u00e9es<\/li>\n<\/ul>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<h1 class=\"wp-block-heading\"><strong>5. Trois unit\u00e9s g\u00e9ologiques en comparaison directe<\/strong><\/h1>\n\n\n\n<figure class=\"wp-block-table\"><table class=\"has-fixed-layout\"><thead><tr><th>r\u00e9gion<\/th><th>Origine<\/th><th>rochers<\/th><th>Hauteur<\/th><th>Paysage<\/th><\/tr><\/thead><tbody><tr><td><strong>Alpes<\/strong><\/td><td>Il y a 30 \u00e0 5 millions d&#039;ann\u00e9es, collision de plaques<\/td><td>Granite, gneiss, calcaire<\/td><td>1 500\u20134 600 m<\/td><td>sommets escarp\u00e9s et \u00e9lev\u00e9s<\/td><\/tr><tr><td><strong>Plateau central<\/strong><\/td><td>S\u00e9diments issus de la formation alpine<\/td><td>M\u00e9lasse<\/td><td>300\u2013800 m<\/td><td>plaines douces<\/td><\/tr><tr><td><strong>Loi<\/strong><\/td><td>Il y a 150 \u00e0 10 millions d&#039;ann\u00e9es, des rides se sont form\u00e9es.<\/td><td>calcaire<\/td><td>800\u20131\u00a0600 m<\/td><td>longues rides, karst<\/td><\/tr><\/tbody><\/table><\/figure>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<h1 class=\"wp-block-heading\"><strong>6. Les glaciers ont fa\u00e7onn\u00e9 de vastes portions du paysage suisse.<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">Lors des derni\u00e8res p\u00e9riodes glaciaires, de vastes r\u00e9gions de Suisse \u00e9taient recouvertes de glace. Les glaciers\u00a0:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>vall\u00e9es mod\u00e9lis\u00e9es (par exemple, les vall\u00e9es de la Limmat, du Rh\u00f4ne et de la Reuss)<\/li>\n\n\n\n<li>lacs laiss\u00e9s derri\u00e8re (par exemple le lac de Zurich, le lac de Lucerne, le lac de Constance)<\/li>\n\n\n\n<li>transport\u00e9 d&#039;\u00e9normes quantit\u00e9s de roches<\/li>\n<\/ul>\n\n\n\n<figure class=\"wp-block-image\"><img data-recalc-dims=\"1\" decoding=\"async\" src=\"https:\/\/i0.wp.com\/www.nccs.admin.ch\/nccs\/en\/home\/sectors\/water-management\/auswirkungen-auf-den-wasserhaushalt\/snow-and-glaciers\/_jcr_content\/par\/image_2036487948\/image.imagespooler.png\/1620813138521\/DE_Abb_6_23_Sedimenttransport_V04.png?w=1200&#038;ssl=1\" alt=\"https:\/\/www.nccs.admin.ch\/nccs\/en\/home\/sectors\/water-management\/auswirkungen-auf-den-wasserhaushalt\/snow-and-glaciers\/_jcr_content\/par\/image_2036487948\/image.imagespooler.png\/1620813138521\/DE_Abb_6_23_Sedimenttransport_V04.png\"\/><\/figure>\n\n\n\n<figure class=\"wp-block-image\"><img data-recalc-dims=\"1\" loading=\"lazy\" decoding=\"async\" width=\"782\" height=\"510\" data-attachment-id=\"853\" data-permalink=\"https:\/\/schweiz.blog\/fr\/geologie-schweiz-einfach-erklaert\/jt4fjttk21ptb7p0f0vlaw_b\/\" data-orig-file=\"https:\/\/i0.wp.com\/schweiz.blog\/wp-content\/uploads\/2025\/11\/jT4fJTtK21PtB7P0F0Vlaw_b.png?fit=782%2C510&amp;ssl=1\" data-orig-size=\"782,510\" data-comments-opened=\"1\" data-image-meta=\"{&quot;aperture&quot;:&quot;0&quot;,&quot;credit&quot;:&quot;&quot;,&quot;camera&quot;:&quot;&quot;,&quot;caption&quot;:&quot;&quot;,&quot;created_timestamp&quot;:&quot;0&quot;,&quot;copyright&quot;:&quot;&quot;,&quot;focal_length&quot;:&quot;0&quot;,&quot;iso&quot;:&quot;0&quot;,&quot;shutter_speed&quot;:&quot;0&quot;,&quot;title&quot;:&quot;&quot;,&quot;orientation&quot;:&quot;0&quot;}\" data-image-title=\"jT4fJTtK21PtB7P0F0Vlaw_b\" data-image-description=\"\" data-image-caption=\"\" data-large-file=\"https:\/\/i0.wp.com\/schweiz.blog\/wp-content\/uploads\/2025\/11\/jT4fJTtK21PtB7P0F0Vlaw_b.png?fit=782%2C510&amp;ssl=1\" src=\"https:\/\/i0.wp.com\/schweiz.blog\/wp-content\/uploads\/2025\/11\/jT4fJTtK21PtB7P0F0Vlaw_b.png?resize=782%2C510&#038;ssl=1\" alt=\"https:\/\/o.quizlet.com\/jT4fJTtK21PtB7P0F0Vlaw_b.png\" class=\"wp-image-853\" srcset=\"https:\/\/i0.wp.com\/schweiz.blog\/wp-content\/uploads\/2025\/11\/jT4fJTtK21PtB7P0F0Vlaw_b.png?w=782&amp;ssl=1 782w, https:\/\/i0.wp.com\/schweiz.blog\/wp-content\/uploads\/2025\/11\/jT4fJTtK21PtB7P0F0Vlaw_b.png?resize=300%2C196&amp;ssl=1 300w, https:\/\/i0.wp.com\/schweiz.blog\/wp-content\/uploads\/2025\/11\/jT4fJTtK21PtB7P0F0Vlaw_b.png?resize=768%2C501&amp;ssl=1 768w, https:\/\/i0.wp.com\/schweiz.blog\/wp-content\/uploads\/2025\/11\/jT4fJTtK21PtB7P0F0Vlaw_b.png?resize=542%2C353&amp;ssl=1 542w\" sizes=\"auto, (max-width: 782px) 100vw, 782px\" \/><\/figure>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Source:<\/strong> <a href=\"https:\/\/www.swisseduc.ch\/glaciers\" target=\"_blank\" rel=\"noopener\">https:\/\/www.swisseduc.ch\/glaciers<\/a><\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Aujourd&#039;hui encore, les glaciers fa\u00e7onnent les Alpes, m\u00eame s&#039;ils reculent consid\u00e9rablement.<\/p>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<h1 class=\"wp-block-heading\"><strong>7. Pourquoi la diversit\u00e9 g\u00e9ologique de la Suisse est unique<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">La Suisse est g\u00e9ologiquement unique car :<\/p>\n\n\n\n<ol class=\"wp-block-list\">\n<li><strong>Trois grandes cha\u00eenes de montagnes dans une petite zone<\/strong> rencontrer.<\/li>\n\n\n\n<li><strong>Des dizaines de types de roches<\/strong> se superposer verticalement.<\/li>\n\n\n\n<li>Ils font partie des <strong>les r\u00e9gions les plus \u00e9tudi\u00e9es au monde<\/strong> est.<\/li>\n\n\n\n<li>Les paysages sont extr\u00eamement vari\u00e9s \u2013 des hautes Alpes aux replis calcaires.<\/li>\n\n\n\n<li>Des r\u00e9gions comme l&#039;Engadine, le Valais ou le Jura <strong>histoires g\u00e9ologiques ind\u00e9pendantes<\/strong> avoir.<\/li>\n<\/ol>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<h1 class=\"wp-block-heading\"><strong>8. Conclusion<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">Le <strong>G\u00e9ologie de la Suisse<\/strong> Ceci explique la grande diversit\u00e9 du pays\u00a0: les hautes Alpes, les douces collines, le vaste plateau suisse et le massif pliss\u00e9 du Jura. Sa formation r\u00e9sulte d\u2019une combinaison de collisions de plaques tectoniques, de d\u00e9p\u00f4ts s\u00e9dimentaires, de soul\u00e8vement et d\u2019\u00e9rosion \u2013 une histoire g\u00e9ologique encore visible aujourd\u2019hui.<\/p>","protected":false},"excerpt":{"rendered":"Die Geologie der Schweiz ist weltweit einzigartig. Auf kleinstem Raum treffen drei grosse geologische Einheiten zusammen: Alpen, Mittelland&hellip;","protected":false},"author":274216737,"featured_media":852,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_crdt_document":"","_jetpack_newsletter_access":"","_jetpack_dont_email_post_to_subs":true,"_jetpack_newsletter_tier_id":0,"_jetpack_memberships_contains_paywalled_content":false,"csco_display_header_overlay":false,"csco_singular_sidebar":"","csco_page_header_type":"","csco_page_load_nextpost":"","csco_page_reading_time":"","csco_page_toc_navigation":"","csco_post_video_location":[],"csco_post_video_location_hash":"","csco_post_video_url":"","csco_post_video_bg_start_time":0,"csco_post_video_bg_end_time":0,"csco_post_video_bg_volume":false,"_jetpack_memberships_contains_paid_content":false,"footnotes":"","jetpack_post_was_ever_published":false},"categories":[2723],"tags":[2969,2968,2971,2970],"class_list":{"0":"post-850","1":"post","2":"type-post","3":"status-publish","4":"format-standard","5":"has-post-thumbnail","7":"category-schweiz","8":"tag-alpine-geologie-schweiz","9":"tag-geologie-schweiz","10":"tag-jura-geologie","11":"tag-schweiz-geologie-erklaerung","12":"cs-entry","13":"cs-video-wrap"},"jetpack_featured_media_url":"https:\/\/i0.wp.com\/schweiz.blog\/wp-content\/uploads\/2025\/11\/20251130_1551_Schweizer-Geologie-Illustration_simple_compose_01kbakwqsafp8reakka1r6pdny.png?fit=1536%2C1024&ssl=1","jetpack_sharing_enabled":true,"jetpack_shortlink":"https:\/\/wp.me\/pgWLwP-dI","_links":{"self":[{"href":"https:\/\/schweiz.blog\/fr\/wp-json\/wp\/v2\/posts\/850","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/schweiz.blog\/fr\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/schweiz.blog\/fr\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/schweiz.blog\/fr\/wp-json\/wp\/v2\/users\/274216737"}],"replies":[{"embeddable":true,"href":"https:\/\/schweiz.blog\/fr\/wp-json\/wp\/v2\/comments?post=850"}],"version-history":[{"count":2,"href":"https:\/\/schweiz.blog\/fr\/wp-json\/wp\/v2\/posts\/850\/revisions"}],"predecessor-version":[{"id":854,"href":"https:\/\/schweiz.blog\/fr\/wp-json\/wp\/v2\/posts\/850\/revisions\/854"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/schweiz.blog\/fr\/wp-json\/wp\/v2\/media\/852"}],"wp:attachment":[{"href":"https:\/\/schweiz.blog\/fr\/wp-json\/wp\/v2\/media?parent=850"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/schweiz.blog\/fr\/wp-json\/wp\/v2\/categories?post=850"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/schweiz.blog\/fr\/wp-json\/wp\/v2\/tags?post=850"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}