{"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":"geologija-svicarske-jednostavno-objasnjena","status":"publish","type":"post","link":"https:\/\/schweiz.blog\/hr\/geologie-schweiz-einfach-erklaert\/","title":{"rendered":"Geologija \u0160vicarske obja\u0161njena jednostavno"},"content":{"rendered":"<p class=\"wp-block-paragraph\">The <strong>Geologija \u0160vicarske<\/strong> Jedinstven je u svijetu. Tri glavne geolo\u0161ke jedinice susre\u0107u se na vrlo malom podru\u010dju: <strong>Alpe<\/strong>, <strong>Sredi\u0161nja visoravan<\/strong> i <strong>Zakon<\/strong>. Svaka regija ima svoju geolo\u0161ku povijest, vrste stijena i tipi\u010dne oblike reljefa. Ovaj \u010dlanak obja\u0161njava geolo\u0161ku strukturu \u0160vicarske na jednostavan i razumljiv na\u010din.<\/p>\n\n\n\n<h1 class=\"wp-block-heading\"><strong>1. \u0160vicarska je geolo\u0161ki mozaik.<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">\u0160vicarska se nalazi u sredini zone u kojoj se <strong>Afri\u010dke i euroazijske tektonske plo\u010de<\/strong> sudario se. Taj sudar je oblikovao Alpe i i danas utje\u010de na krajolik.<\/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>Izvor:<\/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\">Pritisak dviju plo\u010da gurnuo je mase stijena jednu preko druge, presavio ih i doveo do sna\u017enih izdizanja.<\/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. Alpe \u2013 najmla\u0111i planinski lanac u \u0160vicarskoj<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">Alpe su nastale od strane <strong>Sudar Afri\u010dke i Euroazijske plo\u010de<\/strong> oko <strong>30\u20135 milijuna godina<\/strong>. U tom procesu, starije stijene iz biv\u0161eg oceana Tethys bile su potisnute prema gore.<\/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>Izvor:<\/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\">Tipi\u010dne stijene Alpa<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Gnejs<\/strong><\/li>\n\n\n\n<li><strong>granit<\/strong><\/li>\n\n\n\n<li><strong>\u0161kriljevca<\/strong><\/li>\n\n\n\n<li><strong>vapnenac<\/strong><\/li>\n<\/ul>\n\n\n\n<h2 class=\"wp-block-heading\">Zna\u010dajke<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>najvi\u0161i vrhovi \u0160vicarske<\/li>\n\n\n\n<li>strme doline<\/li>\n\n\n\n<li>Aktivno formiranje planina nastavlja se i danas<\/li>\n\n\n\n<li>mnogi ledenjaci (povla\u010de se, ali imaju utjecaj)<\/li>\n<\/ul>\n\n\n\n<p class=\"wp-block-paragraph\">Alpe se sastoje od nekoliko tektonskih jedinica kao \u0161to su <strong>Aar masiv<\/strong>, <strong>Gotthardski masiv<\/strong>, <strong>Peninski<\/strong>, <strong>Helveticum<\/strong> itd.<\/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. \u0160vicarska visoravan \u2013 geolo\u0161ka depresija izme\u0111u Alpa i gorja Jura<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">The <strong>\u0160vicarska visoravan<\/strong> To je \u0161iroka depresija koja je bila ispunjena naslagama tijekom formiranja Alpa. Nastala je te\u017einom i pritiskom Alpa dok su se u to vrijeme uzdizale.<\/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>Izvor:<\/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\">Tipi\u010dne stijene \u0160vicarske visoravni<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Melasa<\/strong> (Pje\u0161\u010denjak, lapor, konglomerati)<\/li>\n\n\n\n<li>mladi sedimenti iz rijeka i jezera<\/li>\n<\/ul>\n\n\n\n<h2 class=\"wp-block-heading\">Zna\u010dajke<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>plodne ravnice<\/li>\n\n\n\n<li>blaga brda<\/li>\n\n\n\n<li>gusto naseljeno<\/li>\n\n\n\n<li>Najva\u017enija poljoprivredna i gospodarska regija \u0160vicarske<\/li>\n<\/ul>\n\n\n\n<p class=\"wp-block-paragraph\">Molasa potje\u010de od erodiranog materijala nadolaze\u0107ih Alpa i talo\u017eena je u velikim poljima krhotina.<\/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. Jurske planine \u2013 drevni naborani planinski lanac od vapnenca<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">The <strong>Zakon<\/strong> Geolo\u0161ki je mnogo stariji od Alpa. Sastoji se uglavnom od <strong>vapnenac<\/strong>, koji je natalo\u017een u moru prije vi\u0161e od 150 milijuna godina. Zbog pritiska Alpa, naborao se prema sjeveru.<\/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>Izvor:<\/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\">Tipi\u010dne stijene iz jure<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>vapnenac<\/li>\n\n\n\n<li>lapor<\/li>\n\n\n\n<li>glina<\/li>\n<\/ul>\n\n\n\n<h2 class=\"wp-block-heading\">Zna\u010dajke<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>blagi, izdu\u017eeni nabori (obi\u010dno u obliku antene u planinama Jura)<\/li>\n\n\n\n<li>mnoge \u0161pilje (kr\u0161ki krajolici)<\/li>\n\n\n\n<li>\u0161iroke \u0161ume<\/li>\n\n\n\n<li>Platoi i doline<\/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. Tri geolo\u0161ke jedinice u izravnoj usporedbi<\/strong><\/h1>\n\n\n\n<figure class=\"wp-block-table\"><table class=\"has-fixed-layout\"><thead><tr><th>regija<\/th><th>Podrijetlo<\/th><th>stijene<\/th><th>Visina<\/th><th>Krajolik<\/th><\/tr><\/thead><tbody><tr><td><strong>Alpe<\/strong><\/td><td>Prije 30\u20135 milijuna godina, sudar plo\u010da<\/td><td>Granit, gnajs, vapnenac<\/td><td>1500\u20134600 m<\/td><td>strmi, visoki vrhovi<\/td><\/tr><tr><td><strong>Sredi\u0161nja visoravan<\/strong><\/td><td>Sedimenti iz alpske formacije<\/td><td>Melasa<\/td><td>300\u2013800 m<\/td><td>blage ravnice<\/td><\/tr><tr><td><strong>Zakon<\/strong><\/td><td>Prije 150\u201310 milijuna godina, nabiranje<\/td><td>vapnenac<\/td><td>800\u20131600 m<\/td><td>duge bore, kr\u0161<\/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. Ledenjaci su oblikovali velike dijelove \u0161vicarskog krajolika<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">Tijekom posljednjih ledenih doba, veliki dijelovi \u0160vicarske bili su prekriveni ledom. Gle\u010deri:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>modelirane doline (npr. doline Limmat, Rh\u00f4ne, Reuss)<\/li>\n\n\n\n<li>zaostala jezera (npr. Ciri\u0161ko jezero, Luzernsko jezero, Bodensko jezero)<\/li>\n\n\n\n<li>prevozio ogromne koli\u010dine kamenja<\/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\/hr\/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>Izvor:<\/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\">\u010cak i danas, ledenjaci oblikuju Alpe, iako se znatno povla\u010de.<\/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. Za\u0161to je \u0161vicarska geolo\u0161ka raznolikost jedinstvena<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">\u0160vicarska je geolo\u0161ki jedinstvena jer:<\/p>\n\n\n\n<ol class=\"wp-block-list\">\n<li><strong>Tri velika planinska lanca na malom podru\u010dju<\/strong> susresti se.<\/li>\n\n\n\n<li><strong>Deseci vrsta stijena<\/strong> le\u017ee okomito jedna na drugoj.<\/li>\n\n\n\n<li>Oni su jedni od <strong>najbolje prou\u010denih podru\u010dja u svijetu<\/strong> je.<\/li>\n\n\n\n<li>Krajolici su izuzetno raznoliki - od visokih Alpa do vapnena\u010dkih nabora.<\/li>\n\n\n\n<li>Regije poput Engadina, Valaisa ili Jure <strong>neovisne geolo\u0161ke povijesti<\/strong> imati.<\/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. Zaklju\u010dak<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">The <strong>Geologija \u0160vicarske<\/strong> To obja\u0161njava za\u0161to je zemlja toliko raznolika: visoke Alpe, blaga podno\u017eja, \u0161iroka \u0160vicarska visoravan i naborano gorje Jura. Njezino formiranje je kombinacija sudara plo\u010da, talo\u017eenja sedimenta, izdizanja i erozije \u2013 geolo\u0161ke povijesti koja je i danas vidljiva.<\/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\/hr\/wp-json\/wp\/v2\/posts\/850","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/schweiz.blog\/hr\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/schweiz.blog\/hr\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/schweiz.blog\/hr\/wp-json\/wp\/v2\/users\/274216737"}],"replies":[{"embeddable":true,"href":"https:\/\/schweiz.blog\/hr\/wp-json\/wp\/v2\/comments?post=850"}],"version-history":[{"count":2,"href":"https:\/\/schweiz.blog\/hr\/wp-json\/wp\/v2\/posts\/850\/revisions"}],"predecessor-version":[{"id":854,"href":"https:\/\/schweiz.blog\/hr\/wp-json\/wp\/v2\/posts\/850\/revisions\/854"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/schweiz.blog\/hr\/wp-json\/wp\/v2\/media\/852"}],"wp:attachment":[{"href":"https:\/\/schweiz.blog\/hr\/wp-json\/wp\/v2\/media?parent=850"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/schweiz.blog\/hr\/wp-json\/wp\/v2\/categories?post=850"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/schweiz.blog\/hr\/wp-json\/wp\/v2\/tags?post=850"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}