{"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":"geologia-da-suica-explicada-de-forma-simples","status":"publish","type":"post","link":"https:\/\/schweiz.blog\/pt\/geologie-schweiz-einfach-erklaert\/","title":{"rendered":"Geologia da Su\u00ed\u00e7a explicada de forma simples"},"content":{"rendered":"<p class=\"wp-block-paragraph\">O <strong>Geologia da Su\u00ed\u00e7a<\/strong> \u00c9 um fen\u00f4meno \u00fanico no mundo. Tr\u00eas grandes unidades geol\u00f3gicas se encontram em uma \u00e1rea muito pequena: <strong>Alpes<\/strong>, <strong>Planalto Central<\/strong> e <strong>Lei<\/strong>. Cada regi\u00e3o possui sua pr\u00f3pria hist\u00f3ria geol\u00f3gica, tipos de rochas e formas de relevo t\u00edpicas. Este artigo explica a estrutura geol\u00f3gica da Su\u00ed\u00e7a de forma simples e compreens\u00edvel.<\/p>\n\n\n\n<h1 class=\"wp-block-heading\"><strong>1. A Su\u00ed\u00e7a \u00e9 um mosaico geol\u00f3gico.<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">A Su\u00ed\u00e7a situa-se no meio da zona onde o <strong>placas tect\u00f4nicas africanas e eurasi\u00e1ticas<\/strong> colidiram. Essa colis\u00e3o formou os Alpes e continua a influenciar a paisagem at\u00e9 hoje.<\/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>Fonte:<\/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\">A press\u00e3o das duas placas empurrou massas de rocha umas sobre as outras, dobrando-as e provocando fortes eleva\u00e7\u00f5es.<\/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. Os Alpes \u2013 a cordilheira mais jovem da Su\u00ed\u00e7a<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">Os Alpes foram formados pelos <strong>Colis\u00e3o das placas africana e eurasi\u00e1tica<\/strong> sobre <strong>30 a 5 milh\u00f5es de anos<\/strong>. Nesse processo, rochas mais antigas do antigo Oceano T\u00e9tis foram empurradas para cima.<\/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>Fonte:<\/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\">Rochas t\u00edpicas dos Alpes<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Gneis<\/strong><\/li>\n\n\n\n<li><strong>granito<\/strong><\/li>\n\n\n\n<li><strong>ard\u00f3sia<\/strong><\/li>\n\n\n\n<li><strong>calc\u00e1rio<\/strong><\/li>\n<\/ul>\n\n\n\n<h2 class=\"wp-block-heading\">Caracter\u00edsticas<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>picos mais altos da Su\u00ed\u00e7a<\/li>\n\n\n\n<li>vales \u00edngremes<\/li>\n\n\n\n<li>A forma\u00e7\u00e3o ativa de montanhas continua at\u00e9 hoje.<\/li>\n\n\n\n<li>muitas geleiras (em recuo, mas influentes)<\/li>\n<\/ul>\n\n\n\n<p class=\"wp-block-paragraph\">Os Alpes s\u00e3o constitu\u00eddos por diversas unidades tect\u00f4nicas, como os <strong>Maci\u00e7o de Aar<\/strong>, <strong>Maci\u00e7o de Gotthard<\/strong>, <strong>Pen\u00ednico<\/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. O Planalto Su\u00ed\u00e7o \u2013 a depress\u00e3o geol\u00f3gica entre os Alpes e as Montanhas Jura<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">O <strong>Planalto Su\u00ed\u00e7o<\/strong> Trata-se de uma ampla depress\u00e3o que foi preenchida com dep\u00f3sitos durante a forma\u00e7\u00e3o dos Alpes. Ela foi criada pelo peso e pela press\u00e3o dos Alpes \u00e0 medida que estes se elevavam naquela \u00e9poca.<\/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>Fonte:<\/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\">Rochas t\u00edpicas do Planalto Su\u00ed\u00e7o<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Mela\u00e7o<\/strong> (Arenito, marga, conglomerados)<\/li>\n\n\n\n<li>sedimentos jovens de rios e lagos<\/li>\n<\/ul>\n\n\n\n<h2 class=\"wp-block-heading\">Caracter\u00edsticas<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>plan\u00edcies f\u00e9rteis<\/li>\n\n\n\n<li>colinas suaves<\/li>\n\n\n\n<li>densamente povoado<\/li>\n\n\n\n<li>A regi\u00e3o agr\u00edcola e econ\u00f4mica mais importante da Su\u00ed\u00e7a<\/li>\n<\/ul>\n\n\n\n<p class=\"wp-block-paragraph\">O mela\u00e7o tem origem no material erodido dos Alpes emergentes e foi depositado em grandes campos de detritos.<\/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. As Montanhas Jura \u2013 uma antiga cordilheira dobrada composta de calc\u00e1rio.<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">O <strong>Lei<\/strong> \u00c9 geologicamente muito mais antigo que os Alpes. Consiste principalmente em <strong>calc\u00e1rio<\/strong>, que foi depositada no mar h\u00e1 mais de 150 milh\u00f5es de anos. Devido \u00e0 press\u00e3o dos Alpes, foi dobrada para o norte.<\/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>Fonte:<\/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\">Rochas t\u00edpicas do per\u00edodo Jur\u00e1ssico<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>calc\u00e1rio<\/li>\n\n\n\n<li>marga<\/li>\n\n\n\n<li>argila<\/li>\n<\/ul>\n\n\n\n<h2 class=\"wp-block-heading\">Caracter\u00edsticas<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>dobras suaves e alongadas (tipicamente em forma de antena nas montanhas do Jura)<\/li>\n\n\n\n<li>muitas cavernas (paisagens c\u00e1rsticas)<\/li>\n\n\n\n<li>vastas florestas<\/li>\n\n\n\n<li>Planaltos e vales<\/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. Tr\u00eas unidades geol\u00f3gicas em compara\u00e7\u00e3o direta<\/strong><\/h1>\n\n\n\n<figure class=\"wp-block-table\"><table class=\"has-fixed-layout\"><thead><tr><th>regi\u00e3o<\/th><th>Origem<\/th><th>rochas<\/th><th>Altura<\/th><th>Paisagem<\/th><\/tr><\/thead><tbody><tr><td><strong>Alpes<\/strong><\/td><td>Entre 30 e 5 milh\u00f5es de anos atr\u00e1s, colis\u00e3o de placas tect\u00f4nicas<\/td><td>Granito, gnaisse, calc\u00e1rio<\/td><td>1.500\u20134.600 m<\/td><td>picos altos e acidentados<\/td><\/tr><tr><td><strong>Planalto Central<\/strong><\/td><td>Sedimentos da forma\u00e7\u00e3o alpina<\/td><td>Mela\u00e7o<\/td><td>300\u2013800 m<\/td><td>plan\u00edcies suaves<\/td><\/tr><tr><td><strong>Lei<\/strong><\/td><td>H\u00e1 150 a 10 milh\u00f5es de anos, enrugamento<\/td><td>calc\u00e1rio<\/td><td>800\u20131.600 m<\/td><td>longas rugas, c\u00e1rstico<\/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. As geleiras moldaram grandes partes da paisagem su\u00ed\u00e7a.<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">Durante as \u00faltimas eras glaciais, grandes \u00e1reas da Su\u00ed\u00e7a ficaram cobertas de gelo. As geleiras:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>vales modelados (por exemplo, vales do Limmat, R\u00f3dano e Reuss)<\/li>\n\n\n\n<li>lagos remanescentes (por exemplo, Lago de Zurique, Lago de Lucerna, Lago de Constan\u00e7a)<\/li>\n\n\n\n<li>transportaram enormes quantidades de rocha<\/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\/pt\/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>Fonte:<\/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\">Ainda hoje, as geleiras moldam os Alpes, embora estejam recuando significativamente.<\/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. Por que a diversidade geol\u00f3gica da Su\u00ed\u00e7a \u00e9 \u00fanica<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">A Su\u00ed\u00e7a \u00e9 geologicamente \u00fanica porque:<\/p>\n\n\n\n<ol class=\"wp-block-list\">\n<li><strong>Tr\u00eas grandes cadeias de montanhas em uma pequena \u00e1rea<\/strong> encontrar.<\/li>\n\n\n\n<li><strong>Dezenas de tipos de rocha<\/strong> Est\u00e3o empilhadas verticalmente umas sobre as outras.<\/li>\n\n\n\n<li>Eles s\u00e3o um dos <strong>\u00e1reas mais estudadas em todo o mundo<\/strong> \u00e9.<\/li>\n\n\n\n<li>As paisagens variam extremamente \u2013 desde os altos Alpes at\u00e9 as dobras calc\u00e1rias.<\/li>\n\n\n\n<li>Regi\u00f5es como Engadina, Valais ou Jura <strong>hist\u00f3rias geol\u00f3gicas independentes<\/strong> ter.<\/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. Conclus\u00e3o<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">O <strong>Geologia da Su\u00ed\u00e7a<\/strong> Isso explica por que o pa\u00eds \u00e9 t\u00e3o diverso: altos Alpes, suaves colinas, o amplo Planalto Su\u00ed\u00e7o e as montanhas dobradas do Jura. Sua forma\u00e7\u00e3o \u00e9 uma combina\u00e7\u00e3o de colis\u00f5es de placas tect\u00f4nicas, deposi\u00e7\u00e3o de sedimentos, soerguimento e eros\u00e3o \u2013 uma hist\u00f3ria geol\u00f3gica que ainda \u00e9 vis\u00edvel hoje.<\/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\/pt\/wp-json\/wp\/v2\/posts\/850","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/schweiz.blog\/pt\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/schweiz.blog\/pt\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/schweiz.blog\/pt\/wp-json\/wp\/v2\/users\/274216737"}],"replies":[{"embeddable":true,"href":"https:\/\/schweiz.blog\/pt\/wp-json\/wp\/v2\/comments?post=850"}],"version-history":[{"count":2,"href":"https:\/\/schweiz.blog\/pt\/wp-json\/wp\/v2\/posts\/850\/revisions"}],"predecessor-version":[{"id":854,"href":"https:\/\/schweiz.blog\/pt\/wp-json\/wp\/v2\/posts\/850\/revisions\/854"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/schweiz.blog\/pt\/wp-json\/wp\/v2\/media\/852"}],"wp:attachment":[{"href":"https:\/\/schweiz.blog\/pt\/wp-json\/wp\/v2\/media?parent=850"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/schweiz.blog\/pt\/wp-json\/wp\/v2\/categories?post=850"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/schweiz.blog\/pt\/wp-json\/wp\/v2\/tags?post=850"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}