{"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":"gjeologjia-e-zvicres-e-shpjeguar-thjesht","status":"publish","type":"post","link":"https:\/\/schweiz.blog\/sq\/geologie-schweiz-einfach-erklaert\/","title":{"rendered":"Gjeologjia e Zvicr\u00ebs e shpjeguar thjesht"},"content":{"rendered":"<p class=\"wp-block-paragraph\">I\/E\/T\u00eb\/T\u00eb <strong>Gjeologjia e Zvicr\u00ebs<\/strong> \u00cbsht\u00eb unik n\u00eb mbar\u00eb bot\u00ebn. Tre nj\u00ebsi kryesore gjeologjike takohen n\u00eb nj\u00eb zon\u00eb shum\u00eb t\u00eb vog\u00ebl: <strong>Alpet<\/strong>, <strong>Rrafshnalta Qendrore<\/strong> dhe <strong>Ligji<\/strong>. \u00c7do rajon ka historin\u00eb e vet gjeologjike, llojet e shk\u00ebmbinjve dhe format tipike t\u00eb relievit. Ky artikull shpjegon struktur\u00ebn gjeologjike t\u00eb Zvicr\u00ebs n\u00eb nj\u00eb m\u00ebnyr\u00eb t\u00eb thjesht\u00eb dhe t\u00eb kuptueshme.<\/p>\n\n\n\n<h1 class=\"wp-block-heading\"><strong>1. Zvicra \u00ebsht\u00eb nj\u00eb mozaik gjeologjik.<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">Zvicra shtrihet n\u00eb mes t\u00eb zon\u00ebs ku <strong>Pllakat tektonike afrikane dhe euroaziatike<\/strong> u p\u00ebrplas\u00ebn. Kjo p\u00ebrplasje formoi Alpet dhe vazhdon t\u00eb ndikoj\u00eb n\u00eb peizazh edhe sot.<\/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>Burimi:<\/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\">Presioni i dy pllakave shtyu masa shk\u00ebmbinjsh mbi nj\u00ebra-tjetr\u00ebn, i palosi ato dhe \u00e7oi n\u00eb ngritje t\u00eb forta.<\/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. Alpet \u2013 vargmali m\u00eb i ri n\u00eb Zvic\u00ebr<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">Alpet u formuan nga <strong>P\u00ebrplasja e pllakave afrikane dhe euroaziatike<\/strong> rreth <strong>30\u20135 milion\u00eb vjet<\/strong>. N\u00eb k\u00ebt\u00eb proces, shk\u00ebmbinjt\u00eb m\u00eb t\u00eb vjet\u00ebr nga ish-Oqeani Tetis u shtyn\u00eb lart.<\/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>Burimi:<\/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\">Shk\u00ebmbinjt\u00eb tipik\u00eb t\u00eb Alpeve<\/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>propozoj<\/strong><\/li>\n\n\n\n<li><strong>g\u00eblqeror<\/strong><\/li>\n<\/ul>\n\n\n\n<h2 class=\"wp-block-heading\">Karakteristikat<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>majat m\u00eb t\u00eb larta t\u00eb Zvicr\u00ebs<\/li>\n\n\n\n<li>lugina t\u00eb pjerr\u00ebta<\/li>\n\n\n\n<li>Nd\u00ebrtimi aktiv malor vazhdon edhe sot e k\u00ebsaj dite.<\/li>\n\n\n\n<li>shum\u00eb akullnaja (n\u00eb t\u00ebrheqje, por me ndikim)<\/li>\n<\/ul>\n\n\n\n<p class=\"wp-block-paragraph\">Alpet p\u00ebrb\u00ebhen nga disa nj\u00ebsi tektonike, si\u00e7 jan\u00eb <strong>Masivi Aar<\/strong>, <strong>Masivi i Gothardit<\/strong>, <strong>Peninike<\/strong>, <strong>Helvetikum<\/strong> etj.<\/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. Rrafshnalta Zvicerane \u2013 depresioni gjeologjik midis Alpeve dhe Maleve Jura<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">I\/E\/T\u00eb\/T\u00eb <strong>Rrafshnalta Zvicerane<\/strong> \u00cbsht\u00eb nj\u00eb grop\u00eb e gjer\u00eb q\u00eb u mbush me depozita gjat\u00eb formimit t\u00eb Alpeve. U krijua nga pesha dhe presioni i Alpeve nd\u00ebrsa ato ngriheshin n\u00eb at\u00eb koh\u00eb.<\/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>Burimi:<\/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\">Shk\u00ebmbinjt\u00eb tipik\u00eb t\u00eb Rrafshnalt\u00ebs Zvicerane<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Melas\u00eb<\/strong> (Gur ranor, mergel, konglomerate)<\/li>\n\n\n\n<li>sedimente t\u00eb reja nga lumenjt\u00eb dhe liqenet<\/li>\n<\/ul>\n\n\n\n<h2 class=\"wp-block-heading\">Karakteristikat<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>fusha pjellore<\/li>\n\n\n\n<li>kodra t\u00eb buta<\/li>\n\n\n\n<li>me popullsi t\u00eb dendur<\/li>\n\n\n\n<li>Rajoni m\u00eb i r\u00ebnd\u00ebsish\u00ebm bujq\u00ebsor dhe ekonomik i Zvicr\u00ebs<\/li>\n<\/ul>\n\n\n\n<p class=\"wp-block-paragraph\">Melasa buron nga materiali i erozionit t\u00eb Alpeve n\u00eb zhvillim dhe \u00ebsht\u00eb depozituar n\u00eb fusha t\u00eb m\u00ebdha mbeturinash.<\/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. Malet Jura \u2013 nj\u00eb vargmal i lasht\u00eb i p\u00ebrb\u00ebr\u00eb nga gur g\u00eblqeror<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">I\/E\/T\u00eb\/T\u00eb <strong>Ligji<\/strong> Gjeologjikisht \u00ebsht\u00eb shum\u00eb m\u00eb i vjet\u00ebr se Alpet. P\u00ebrb\u00ebhet kryesisht nga <strong>g\u00eblqeror<\/strong>, i cili u depozitua n\u00eb det mbi 150 milion\u00eb vjet m\u00eb par\u00eb. P\u00ebr shkak t\u00eb presionit t\u00eb Alpeve, ai u palos n\u00eb veri.<\/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>Burimi:<\/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\">Shk\u00ebmbinjt\u00eb tipik\u00eb n\u00eb periudh\u00ebn Jurasike<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>g\u00eblqeror<\/li>\n\n\n\n<li>mergel<\/li>\n\n\n\n<li>argjil\u00eb<\/li>\n<\/ul>\n\n\n\n<h2 class=\"wp-block-heading\">Karakteristikat<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>palosje t\u00eb buta, t\u00eb zgjatura (zakonisht n\u00eb form\u00eb antene n\u00eb malet Jura)<\/li>\n\n\n\n<li>shum\u00eb shpella (peizazhe karstike)<\/li>\n\n\n\n<li>pyje t\u00eb gjera<\/li>\n\n\n\n<li>Pllajat dhe luginat<\/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 nj\u00ebsi gjeologjike n\u00eb krahasim t\u00eb drejtp\u00ebrdrejt\u00eb<\/strong><\/h1>\n\n\n\n<figure class=\"wp-block-table\"><table class=\"has-fixed-layout\"><thead><tr><th>rajon<\/th><th>Origjina<\/th><th>shk\u00ebmbinj<\/th><th>Lart\u00ebsia<\/th><th>Peizazh<\/th><\/tr><\/thead><tbody><tr><td><strong>Alpet<\/strong><\/td><td>30\u20135 milion vjet m\u00eb par\u00eb, p\u00ebrplasja e pllakave<\/td><td>Granit, gneiss, gur g\u00eblqeror<\/td><td>1,500\u20134,600 m<\/td><td>maja t\u00eb larta dhe t\u00eb ashpra<\/td><\/tr><tr><td><strong>Rrafshnalta Qendrore<\/strong><\/td><td>Sedimentet nga formacioni alpin<\/td><td>Melas\u00eb<\/td><td>300\u2013800 m<\/td><td>fusha t\u00eb buta<\/td><\/tr><tr><td><strong>Ligji<\/strong><\/td><td>150\u201310 milion\u00eb vjet m\u00eb par\u00eb, duke u rrudhur<\/td><td>g\u00eblqeror<\/td><td>800\u20131,600 m<\/td><td>rrudha t\u00eb gjata, karstike<\/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. Akullnajat formuan pjes\u00eb t\u00eb m\u00ebdha t\u00eb peizazhit zviceran<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">Gjat\u00eb epokave t\u00eb fundit t\u00eb akullnajave, pjes\u00eb t\u00eb m\u00ebdha t\u00eb Zvicr\u00ebs ishin t\u00eb mbuluara me akull. Akullnajat:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>lugina t\u00eb modeluara (p.sh. luginat e Limmat, Ron, Reuss)<\/li>\n\n\n\n<li>liqene t\u00eb l\u00ebna pas (p.sh. Liqeni i Cyrihut, Liqeni i Lucern\u00ebs, Liqeni i Konstanc\u00ebs)<\/li>\n\n\n\n<li>transportoi sasi t\u00eb m\u00ebdha shk\u00ebmbinjsh<\/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\/sq\/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>Burimi:<\/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\">Edhe sot, akullnajat i japin form\u00eb Alpeve, megjith\u00ebse po t\u00ebrhiqen ndjesh\u00ebm.<\/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. Pse diversiteti gjeologjik i Zvicr\u00ebs \u00ebsht\u00eb unik<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">Zvicra \u00ebsht\u00eb gjeologjikisht unike sepse:<\/p>\n\n\n\n<ol class=\"wp-block-list\">\n<li><strong>Tre vargmale t\u00eb m\u00ebdha n\u00eb nj\u00eb zon\u00eb t\u00eb vog\u00ebl<\/strong> takohen.<\/li>\n\n\n\n<li><strong>Dhjet\u00ebra lloje shk\u00ebmbinjsh<\/strong> shtrihen vertikalisht nj\u00ebra mbi tjetr\u00ebn.<\/li>\n\n\n\n<li>Ata jan\u00eb nj\u00eb nga <strong>zonat m\u00eb t\u00eb studiuara n\u00eb t\u00eb gjith\u00eb bot\u00ebn<\/strong> \u00ebsht\u00eb.<\/li>\n\n\n\n<li>Peizazhet ndryshojn\u00eb jasht\u00ebzakonisht shum\u00eb - nga Alpet e larta deri te palosjet g\u00eblqerore.<\/li>\n\n\n\n<li>Rajone t\u00eb tilla si Engadine, Valais ose Jura <strong>historit\u00eb gjeologjike t\u00eb pavarura<\/strong> kam.<\/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. P\u00ebrfundim<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">I\/E\/T\u00eb\/T\u00eb <strong>Gjeologjia e Zvicr\u00ebs<\/strong> Kjo shpjegon pse vendi \u00ebsht\u00eb kaq i larmish\u00ebm: Alpe t\u00eb larta, kodra t\u00eb buta, Rrafshnalta e gjer\u00eb Zvicerane dhe Malet e palosur Jura. Formimi i tij \u00ebsht\u00eb nj\u00eb kombinim i p\u00ebrplasjeve t\u00eb pllakave, depozitimit t\u00eb sedimenteve, ngritjes dhe erozionit - nj\u00eb histori gjeologjike q\u00eb \u00ebsht\u00eb ende e dukshme sot.<\/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\/sq\/wp-json\/wp\/v2\/posts\/850","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/schweiz.blog\/sq\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/schweiz.blog\/sq\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/schweiz.blog\/sq\/wp-json\/wp\/v2\/users\/274216737"}],"replies":[{"embeddable":true,"href":"https:\/\/schweiz.blog\/sq\/wp-json\/wp\/v2\/comments?post=850"}],"version-history":[{"count":2,"href":"https:\/\/schweiz.blog\/sq\/wp-json\/wp\/v2\/posts\/850\/revisions"}],"predecessor-version":[{"id":854,"href":"https:\/\/schweiz.blog\/sq\/wp-json\/wp\/v2\/posts\/850\/revisions\/854"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/schweiz.blog\/sq\/wp-json\/wp\/v2\/media\/852"}],"wp:attachment":[{"href":"https:\/\/schweiz.blog\/sq\/wp-json\/wp\/v2\/media?parent=850"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/schweiz.blog\/sq\/wp-json\/wp\/v2\/categories?post=850"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/schweiz.blog\/sq\/wp-json\/wp\/v2\/tags?post=850"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}