{"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":"geologi-schweiz-enkelt-foerklarat","status":"publish","type":"post","link":"https:\/\/schweiz.blog\/sv\/geologie-schweiz-einfach-erklaert\/","title":{"rendered":"Schweiz geologi f\u00f6rklarad enkelt"},"content":{"rendered":"<p class=\"wp-block-paragraph\">De <strong>Schweiz geologi<\/strong> Det \u00e4r unikt i v\u00e4rlden. Tre stora geologiska enheter m\u00f6ts p\u00e5 ett mycket litet omr\u00e5de: <strong>Alperna<\/strong>, <strong>Centrala plat\u00e5n<\/strong> och <strong>Lag<\/strong>. Varje region har sin egen geologiska historia, sina egna bergarter och typiska landformer. Den h\u00e4r artikeln f\u00f6rklarar Schweiz geologiska struktur p\u00e5 ett enkelt och begripligt s\u00e4tt.<\/p>\n\n\n\n<h1 class=\"wp-block-heading\"><strong>1. Schweiz \u00e4r en geologisk mosaik.<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">Schweiz ligger mitt i den zon d\u00e4r <strong>Afrikanska och eurasiska tektoniska plattor<\/strong> kolliderade. Denna kollision bildade Alperna och p\u00e5verkar fortfarande landskapet \u00e4n idag.<\/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>K\u00e4lla:<\/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\">Trycket fr\u00e5n de tv\u00e5 plattorna tryckte massor av bergarter \u00f6ver varandra, veckade dem och ledde till starka lyftningar.<\/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. Alperna \u2013 den yngsta bergskedjan i Schweiz<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">Alperna bildades av <strong>Kollision mellan de afrikanska och eurasiska plattorna<\/strong> om <strong>30\u20135 miljoner \u00e5r<\/strong>. I denna process trycktes \u00e4ldre stenar fr\u00e5n det tidigare Tethyshavet upp\u00e5t.<\/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>K\u00e4lla:<\/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\">Typiska klippor i Alperna<\/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>skiffer<\/strong><\/li>\n\n\n\n<li><strong>kalksten<\/strong><\/li>\n<\/ul>\n\n\n\n<h2 class=\"wp-block-heading\">Drag<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>h\u00f6gsta toppar i Schweiz<\/li>\n\n\n\n<li>branta dalar<\/li>\n\n\n\n<li>Aktiv bergsbildning forts\u00e4tter \u00e4n idag<\/li>\n\n\n\n<li>m\u00e5nga glaci\u00e4rer (drar sig tillbaka, men \u00e4r inflytelserika)<\/li>\n<\/ul>\n\n\n\n<p class=\"wp-block-paragraph\">Alperna best\u00e5r av flera tektoniska enheter, s\u00e5som <strong>Aar-massivet<\/strong>, <strong>Gotthardmassivet<\/strong>, <strong>Penninic<\/strong>, <strong>Helveticum<\/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. Den schweiziska plat\u00e5n \u2013 den geologiska f\u00f6rdjupningen mellan Alperna och Jurabergen<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">De <strong>Schweiziska plat\u00e5n<\/strong> Det \u00e4r en bred f\u00f6rdjupning som fylldes med avlagringar under Alpernas bildande. Den skapades av Alpernas vikt och tryck n\u00e4r de h\u00f6jdes vid den tiden.<\/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>K\u00e4lla:<\/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\">Typiska stenar p\u00e5 den schweiziska plat\u00e5n<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Melass<\/strong> (Sandsten, m\u00e4rgel, konglomerat)<\/li>\n\n\n\n<li>unga sediment fr\u00e5n floder och sj\u00f6ar<\/li>\n<\/ul>\n\n\n\n<h2 class=\"wp-block-heading\">Drag<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>b\u00f6rdiga sl\u00e4tter<\/li>\n\n\n\n<li>mjuka kullar<\/li>\n\n\n\n<li>t\u00e4tbefolkad<\/li>\n\n\n\n<li>Schweiz viktigaste jordbruks- och ekonomiska region<\/li>\n<\/ul>\n\n\n\n<p class=\"wp-block-paragraph\">Melassen h\u00e4rstammar fr\u00e5n eroderat material fr\u00e5n de framv\u00e4xande Alperna och avsattes i stora skr\u00e4pf\u00e4lt.<\/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. Jurabergen \u2013 en gammal vikbergskedja gjord av kalksten<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">De <strong>Lag<\/strong> Den \u00e4r geologiskt sett mycket \u00e4ldre \u00e4n Alperna. Den best\u00e5r huvudsakligen av <strong>kalksten<\/strong>, som avsattes i havet f\u00f6r \u00f6ver 150 miljoner \u00e5r sedan. P\u00e5 grund av trycket fr\u00e5n Alperna veckades den norrut.<\/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>K\u00e4lla:<\/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\">Typiska bergarter fr\u00e5n juraperioden<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>kalksten<\/li>\n\n\n\n<li>m\u00e4rgel<\/li>\n\n\n\n<li>lera<\/li>\n<\/ul>\n\n\n\n<h2 class=\"wp-block-heading\">Drag<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>mjuka, avl\u00e5nga veck (vanligtvis antennformade i Jurabergen)<\/li>\n\n\n\n<li>m\u00e5nga grottor (karstlandskap)<\/li>\n\n\n\n<li>vidstr\u00e4ckta skogar<\/li>\n\n\n\n<li>Plat\u00e5er och dalar<\/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. Tre geologiska enheter i direkt j\u00e4mf\u00f6relse<\/strong><\/h1>\n\n\n\n<figure class=\"wp-block-table\"><table class=\"has-fixed-layout\"><thead><tr><th>omr\u00e5de<\/th><th>Ursprung<\/th><th>stenar<\/th><th>H\u00f6jd<\/th><th>Landskap<\/th><\/tr><\/thead><tbody><tr><td><strong>Alperna<\/strong><\/td><td>F\u00f6r 30\u20135 miljoner \u00e5r sedan, plattkollision<\/td><td>Granit, gnejs, kalksten<\/td><td>1 500\u20134 600 m<\/td><td>karga, h\u00f6ga toppar<\/td><\/tr><tr><td><strong>Centrala plat\u00e5n<\/strong><\/td><td>Sediment fr\u00e5n alpin formation<\/td><td>Melass<\/td><td>300\u2013800 m<\/td><td>mjuka sl\u00e4tter<\/td><\/tr><tr><td><strong>Lag<\/strong><\/td><td>f\u00f6r 150\u201310 miljoner \u00e5r sedan, rynkning<\/td><td>kalksten<\/td><td>800\u20131 600 m<\/td><td>l\u00e5nga rynkor, 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. Glaci\u00e4rer formade stora delar av det schweiziska landskapet<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">Under de senaste istiderna var stora delar av Schweiz t\u00e4ckta av is. Glaci\u00e4rerna:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>modellerade dalar (t.ex. Limmat-, Rh\u00f4ne- och Reuss-dalarna)<\/li>\n\n\n\n<li>l\u00e4mnade efter sig sj\u00f6ar (t.ex. Z\u00fcrichsj\u00f6n, Vierwaldst\u00e4ttersj\u00f6n, Bodensj\u00f6n)<\/li>\n\n\n\n<li>transporterade enorma m\u00e4ngder sten<\/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\/sv\/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>K\u00e4lla:<\/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\">\u00c4n idag formar glaci\u00e4rer Alperna, \u00e4ven om de drar sig tillbaka avsev\u00e4rt.<\/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. Varf\u00f6r Schweiz geologiska m\u00e5ngfald \u00e4r unik<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">Schweiz \u00e4r geologiskt unikt eftersom:<\/p>\n\n\n\n<ol class=\"wp-block-list\">\n<li><strong>Tre stora bergskedjor p\u00e5 ett litet omr\u00e5de<\/strong> m\u00f6ta.<\/li>\n\n\n\n<li><strong>Dussintals bergarter<\/strong> ligga vertikalt ovanp\u00e5 varandra.<\/li>\n\n\n\n<li>De \u00e4r en av de <strong>b\u00e4st studerade omr\u00e5den v\u00e4rlden \u00f6ver<\/strong> \u00e4r.<\/li>\n\n\n\n<li>Landskapen varierar extremt \u2013 fr\u00e5n h\u00f6ga Alper till kalkstensveckor.<\/li>\n\n\n\n<li>Regioner som Engadine, Valais eller Jura <strong>oberoende geologiska historier<\/strong> ha.<\/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. Slutsats<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">De <strong>Schweiz geologi<\/strong> Detta f\u00f6rklarar varf\u00f6r landet \u00e4r s\u00e5 m\u00e5ngsidigt: h\u00f6ga Alper, mjuka kullar, den breda schweiziska plat\u00e5n och de veckade Jurabergen. Dess bildande \u00e4r en kombination av plattkollisioner, sedimentavs\u00e4ttning, h\u00f6jning och erosion \u2013 en geologisk historia som fortfarande \u00e4r synlig idag.<\/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\/sv\/wp-json\/wp\/v2\/posts\/850","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/schweiz.blog\/sv\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/schweiz.blog\/sv\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/schweiz.blog\/sv\/wp-json\/wp\/v2\/users\/274216737"}],"replies":[{"embeddable":true,"href":"https:\/\/schweiz.blog\/sv\/wp-json\/wp\/v2\/comments?post=850"}],"version-history":[{"count":2,"href":"https:\/\/schweiz.blog\/sv\/wp-json\/wp\/v2\/posts\/850\/revisions"}],"predecessor-version":[{"id":854,"href":"https:\/\/schweiz.blog\/sv\/wp-json\/wp\/v2\/posts\/850\/revisions\/854"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/schweiz.blog\/sv\/wp-json\/wp\/v2\/media\/852"}],"wp:attachment":[{"href":"https:\/\/schweiz.blog\/sv\/wp-json\/wp\/v2\/media?parent=850"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/schweiz.blog\/sv\/wp-json\/wp\/v2\/categories?post=850"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/schweiz.blog\/sv\/wp-json\/wp\/v2\/tags?post=850"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}