{"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-elvetiei-explicata-simplu","status":"publish","type":"post","link":"https:\/\/schweiz.blog\/ro\/geologie-schweiz-einfach-erklaert\/","title":{"rendered":"Geologia Elve\u021biei explicat\u0103 simplu"},"content":{"rendered":"<p class=\"wp-block-paragraph\">Cel\/Cea\/Cei\/Cele <strong>Geologia Elve\u021biei<\/strong> Este unic\u0103 la nivel mondial. Trei unit\u0103\u021bi geologice majore se \u00eent\u00e2lnesc \u00eentr-o zon\u0103 foarte mic\u0103: <strong>Alpi<\/strong>, <strong>Platoul Central<\/strong> \u015fi <strong>Drept<\/strong>. Fiecare regiune are propria istorie geologic\u0103, tipuri de roci \u0219i forme de relief tipice. Acest articol explic\u0103 structura geologic\u0103 a Elve\u021biei \u00eentr-un mod simplu \u0219i u\u0219or de \u00een\u021beles.<\/p>\n\n\n\n<h1 class=\"wp-block-heading\"><strong>1. Elve\u021bia este un mozaic geologic.<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">Elve\u021bia se afl\u0103 \u00een mijlocul zonei \u00een care <strong>Pl\u0103cile tectonice africane \u0219i eurasiatice<\/strong> s-au ciocnit. Aceast\u0103 coliziune a format Alpii \u0219i continu\u0103 s\u0103 influen\u021beze peisajul \u0219i ast\u0103zi.<\/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>Surs\u0103:<\/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\">Presiunea celor dou\u0103 pl\u0103ci a \u00eempins mase de roc\u0103 una peste alta, le-a pliat \u0219i a dus la ridic\u0103ri puternice.<\/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. Alpii \u2013 cel mai t\u00e2n\u0103r lan\u021b muntos din Elve\u021bia<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">Alpii au fost forma\u021bi de <strong>Coliziunea pl\u0103cilor african\u0103 \u0219i eurasiatic\u0103<\/strong> despre <strong>30\u20135 milioane de ani<\/strong>. \u00cen acest proces, roci mai vechi din fostul Ocean Tethys au fost \u00eempinse \u00een sus.<\/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>Surs\u0103:<\/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\">St\u00e2nci tipice ale Alpilor<\/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>ardezie<\/strong><\/li>\n\n\n\n<li><strong>calcar<\/strong><\/li>\n<\/ul>\n\n\n\n<h2 class=\"wp-block-heading\">Caracteristici<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>cele mai \u00eenalte v\u00e2rfuri ale Elve\u021biei<\/li>\n\n\n\n<li>v\u0103i abrupte<\/li>\n\n\n\n<li>Formarea activ\u0103 a mun\u021bilor continu\u0103 p\u00e2n\u0103 \u00een ziua de azi<\/li>\n\n\n\n<li>mul\u021bi ghe\u021bari (\u00een retragere, dar influen\u021bi)<\/li>\n<\/ul>\n\n\n\n<p class=\"wp-block-paragraph\">Alpii sunt alc\u0103tui\u021bi din mai multe unit\u0103\u021bi tectonice, cum ar fi <strong>Masivul Aar<\/strong>, <strong>Masivul Gotthard<\/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. Podi\u0219ul Elve\u021bian \u2013 depresiunea geologic\u0103 dintre Alpi \u0219i Mun\u021bii Jura<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">Cel\/Cea\/Cei\/Cele <strong>Platoul Elve\u021bian<\/strong> Este o depresiune larg\u0103 care a fost umplut\u0103 cu depozite \u00een timpul form\u0103rii Alpilor. A fost creat\u0103 de greutatea \u0219i presiunea Alpilor pe m\u0103sur\u0103 ce ace\u0219tia se ridicau \u00een acea perioad\u0103.<\/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>Surs\u0103:<\/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\">St\u00e2nci tipice ale Podi\u0219ului Elve\u021bian<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Melas\u0103<\/strong> (Gresie, marn\u0103, conglomerate)<\/li>\n\n\n\n<li>sedimente tinere din r\u00e2uri \u0219i lacuri<\/li>\n<\/ul>\n\n\n\n<h2 class=\"wp-block-heading\">Caracteristici<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>c\u00e2mpii fertile<\/li>\n\n\n\n<li>dealuri line<\/li>\n\n\n\n<li>dens populat<\/li>\n\n\n\n<li>Cea mai important\u0103 regiune agricol\u0103 \u0219i economic\u0103 a Elve\u021biei<\/li>\n<\/ul>\n\n\n\n<p class=\"wp-block-paragraph\">Molasa provine din materialul erodat al Alpilor emergen\u021bi \u0219i a fost depus\u0103 \u00een c\u00e2mpuri mari de resturi.<\/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. Mun\u021bii Jura \u2013 un lan\u021b muntos antic, pliat, format din calcar<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">Cel\/Cea\/Cei\/Cele <strong>Drept<\/strong> Este geologic mult mai vechi dec\u00e2t Alpii. Este alc\u0103tuit \u00een principal din <strong>calcar<\/strong>, care a fost depus\u0103 \u00een mare acum peste 150 de milioane de ani. Din cauza presiunii exercitate de Alpi, aceasta a fost pliat\u0103 spre 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>Surs\u0103:<\/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\">Roci tipice din perioada Jurasicului<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>calcar<\/li>\n\n\n\n<li>marn\u0103<\/li>\n\n\n\n<li>lut<\/li>\n<\/ul>\n\n\n\n<h2 class=\"wp-block-heading\">Caracteristici<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>pliuri u\u0219oare, alungite (de obicei \u00een form\u0103 de anten\u0103 \u00een mun\u021bii Jura)<\/li>\n\n\n\n<li>multe pe\u0219teri (peisaje carstice)<\/li>\n\n\n\n<li>p\u0103duri \u00eentinse<\/li>\n\n\n\n<li>Podi\u0219uri \u0219i v\u0103i<\/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. Trei unit\u0103\u021bi geologice \u00een compara\u021bie direct\u0103<\/strong><\/h1>\n\n\n\n<figure class=\"wp-block-table\"><table class=\"has-fixed-layout\"><thead><tr><th>regiune<\/th><th>Origine<\/th><th>roci<\/th><th>\u00cen\u0103l\u0163ime<\/th><th>Peisaj<\/th><\/tr><\/thead><tbody><tr><td><strong>Alpi<\/strong><\/td><td>Acum 30\u20135 milioane de ani, coliziunea pl\u0103cilor<\/td><td>Granit, gnais, calcar<\/td><td>1.500\u20134.600 m<\/td><td>v\u00e2rfuri \u00eenalte \u0219i accidentate<\/td><\/tr><tr><td><strong>Platoul Central<\/strong><\/td><td>Sedimente din forma\u021biunea alpin\u0103<\/td><td>Melas\u0103<\/td><td>300\u2013800 m<\/td><td>c\u00e2mpii line<\/td><\/tr><tr><td><strong>Drept<\/strong><\/td><td>Acum 150\u201310 milioane de ani, \u00eencre\u021bindu-se<\/td><td>calcar<\/td><td>800\u20131.600 m<\/td><td>riduri lungi, carst<\/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. Ghe\u021barii au modelat mari p\u0103r\u021bi din peisajul elve\u021bian<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">\u00cen timpul ultimelor ere glaciare, mari p\u0103r\u021bi ale Elve\u021biei au fost acoperite de ghea\u021b\u0103. Ghe\u021barii:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>v\u0103i modelate (de exemplu, v\u0103ile Limmat, Ron, Reuss)<\/li>\n\n\n\n<li>lacuri l\u0103sate \u00een urm\u0103 (de exemplu, Lacul Zurich, Lacul Lucerna, Lacul Constance)<\/li>\n\n\n\n<li>transportat cantit\u0103\u021bi enorme de roc\u0103<\/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\/ro\/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>Surs\u0103:<\/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\">Chiar \u0219i ast\u0103zi, ghe\u021barii modeleaz\u0103 Alpii, de\u0219i se retrag semnificativ.<\/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. De ce este unic\u0103 diversitatea geologic\u0103 a Elve\u021biei<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">Elve\u021bia este unic\u0103 din punct de vedere geologic deoarece:<\/p>\n\n\n\n<ol class=\"wp-block-list\">\n<li><strong>Trei lan\u021buri muntoase mari \u00eentr-o zon\u0103 mic\u0103<\/strong> \u00eent\u00e2lni.<\/li>\n\n\n\n<li><strong>Zeci de tipuri de roci<\/strong> a\u0219eza\u021bi vertical unul peste altul.<\/li>\n\n\n\n<li>Ei sunt unul dintre <strong>cele mai bine studiate zone din \u00eentreaga lume<\/strong> este.<\/li>\n\n\n\n<li>Peisajele variaz\u0103 extrem de mult \u2013 de la Alpii \u00eenal\u021bi p\u00e2n\u0103 la cute calcaroase.<\/li>\n\n\n\n<li>Regiuni precum Engadina, Valais sau Jura <strong>istorii geologice independente<\/strong> a avea.<\/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. Concluzie<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">Cel\/Cea\/Cei\/Cele <strong>Geologia Elve\u021biei<\/strong> Aceasta explic\u0103 de ce \u021bara este at\u00e2t de divers\u0103: Alpi \u00eenal\u021bi, poalele line, vastul Platou Elve\u021bian \u0219i Mun\u021bii Jura, cuta\u021bi. Formarea sa este o combina\u021bie de coliziuni ale pl\u0103cilor tectonice, depunere de sedimente, ridicare \u0219i eroziune - o istorie geologic\u0103 vizibil\u0103 \u0219i ast\u0103zi.<\/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\/ro\/wp-json\/wp\/v2\/posts\/850","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/schweiz.blog\/ro\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/schweiz.blog\/ro\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/schweiz.blog\/ro\/wp-json\/wp\/v2\/users\/274216737"}],"replies":[{"embeddable":true,"href":"https:\/\/schweiz.blog\/ro\/wp-json\/wp\/v2\/comments?post=850"}],"version-history":[{"count":2,"href":"https:\/\/schweiz.blog\/ro\/wp-json\/wp\/v2\/posts\/850\/revisions"}],"predecessor-version":[{"id":854,"href":"https:\/\/schweiz.blog\/ro\/wp-json\/wp\/v2\/posts\/850\/revisions\/854"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/schweiz.blog\/ro\/wp-json\/wp\/v2\/media\/852"}],"wp:attachment":[{"href":"https:\/\/schweiz.blog\/ro\/wp-json\/wp\/v2\/media?parent=850"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/schweiz.blog\/ro\/wp-json\/wp\/v2\/categories?post=850"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/schweiz.blog\/ro\/wp-json\/wp\/v2\/tags?post=850"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}