{"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":"geologie-svycarska-jednoduse-vysvetlena","status":"publish","type":"post","link":"https:\/\/schweiz.blog\/cs\/geologie-schweiz-einfach-erklaert\/","title":{"rendered":"Geologie \u0160v\u00fdcarska vysv\u011btlena jednodu\u0161e"},"content":{"rendered":"<p class=\"wp-block-paragraph\">Ten\/Ta\/To <strong>Geologie \u0160v\u00fdcarska<\/strong> Je to celosv\u011btov\u011b unik\u00e1tn\u00ed. Na velmi mal\u00e9 plo\u0161e se setk\u00e1vaj\u00ed t\u0159i hlavn\u00ed geologick\u00e9 jednotky: <strong>Alpy<\/strong>, <strong>Centr\u00e1ln\u00ed plo\u0161ina<\/strong> a <strong>Z\u00e1kon<\/strong>. Ka\u017ed\u00fd region m\u00e1 svou vlastn\u00ed geologickou historii, typy hornin a typick\u00e9 tvary ter\u00e9nu. Tento \u010dl\u00e1nek vysv\u011btluje geologickou stavbu \u0160v\u00fdcarska jednoduch\u00fdm a srozumiteln\u00fdm zp\u016fsobem.<\/p>\n\n\n\n<h1 class=\"wp-block-heading\"><strong>1. \u0160v\u00fdcarsko je geologick\u00e1 mozaika.<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">\u0160v\u00fdcarsko le\u017e\u00ed uprost\u0159ed z\u00f3ny, kde <strong>Africk\u00e1 a euroasijsk\u00e1 tektonick\u00e1 deska<\/strong> srazily se. Tato sr\u00e1\u017eka vytvo\u0159ila Alpy a dodnes ovliv\u0148uje krajinu.<\/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>Zdroj:<\/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\">Tlak obou desek tla\u010dil masy hornin na sebe, p\u0159eh\u00fdbal je a vedl k siln\u00fdm v\u00fdzdvih\u016fm.<\/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. Alpy \u2013 nejmlad\u0161\u00ed poho\u0159\u00ed ve \u0160v\u00fdcarsku<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">Alpy vznikly d\u00edky <strong>Sr\u00e1\u017eka Africk\u00e9 a Euroasijsk\u00e9 desky<\/strong> o <strong>30\u20135 milion\u016f let<\/strong>. V tomto procesu byly star\u0161\u00ed horniny z b\u00fdval\u00e9ho oce\u00e1nu Tethys tla\u010deny vzh\u016fru.<\/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>Zdroj:<\/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\">Typick\u00e9 sk\u00e1ly Alp<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Ruly<\/strong><\/li>\n\n\n\n<li><strong>\u017eula<\/strong><\/li>\n\n\n\n<li><strong>b\u0159idlice<\/strong><\/li>\n\n\n\n<li><strong>v\u00e1penec<\/strong><\/li>\n<\/ul>\n\n\n\n<h2 class=\"wp-block-heading\">Funkce<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>nejvy\u0161\u0161\u00ed vrcholy \u0160v\u00fdcarska<\/li>\n\n\n\n<li>strm\u00e1 \u00fadol\u00ed<\/li>\n\n\n\n<li>Aktivn\u00ed budov\u00e1n\u00ed hor pokra\u010duje dodnes<\/li>\n\n\n\n<li>mnoho ledovc\u016f (ustupuj\u00edc\u00edch, ale vlivn\u00fdch)<\/li>\n<\/ul>\n\n\n\n<p class=\"wp-block-paragraph\">Alpy se skl\u00e1daj\u00ed z n\u011bkolika tektonick\u00fdch jednotek, jako nap\u0159. <strong>Aarsk\u00fd masiv<\/strong>, <strong>Gotthardsk\u00fd masiv<\/strong>, <strong>Penninsk\u00fd<\/strong>, <strong>Helv\u00e9tikum<\/strong> atd.<\/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. \u0160v\u00fdcarsk\u00e1 plo\u0161ina \u2013 geologick\u00e1 prohlube\u0148 mezi Alpami a poho\u0159\u00edm Jura<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">Ten\/Ta\/To <strong>\u0160v\u00fdcarsk\u00e1 plo\u0161ina<\/strong> Je to \u0161irok\u00e1 prohlube\u0148, kter\u00e1 byla vypln\u011bna sedimenty b\u011bhem formov\u00e1n\u00ed Alp. Vznikla vlivem t\u00edhy a tlaku Alp, kdy\u017e se v t\u00e9 dob\u011b zvedaly.<\/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>Zdroj:<\/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\">Typick\u00e9 horniny \u0160v\u00fdcarsk\u00e9 plo\u0161iny<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Melasa<\/strong> (P\u00edskovec, sl\u00edn, slepence)<\/li>\n\n\n\n<li>mlad\u00e9 sedimenty z \u0159ek a jezer<\/li>\n<\/ul>\n\n\n\n<h2 class=\"wp-block-heading\">Funkce<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>\u00farodn\u00e9 pl\u00e1n\u011b<\/li>\n\n\n\n<li>m\u00edrn\u00e9 kopce<\/li>\n\n\n\n<li>hust\u011b os\u00eddlen\u00e9<\/li>\n\n\n\n<li>Nejd\u016fle\u017eit\u011bj\u0161\u00ed zem\u011bd\u011blsk\u00fd a hospod\u00e1\u0159sk\u00fd region \u0160v\u00fdcarska<\/li>\n<\/ul>\n\n\n\n<p class=\"wp-block-paragraph\">Molasa poch\u00e1z\u00ed z erodovan\u00e9ho materi\u00e1lu nov\u011b vznikaj\u00edc\u00edch Alp a byla ulo\u017eena ve velk\u00fdch sutinov\u00fdch pol\u00edch.<\/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. Poho\u0159\u00ed Jura \u2013 starobyl\u00e9 vr\u00e1sovit\u00e9 poho\u0159\u00ed z v\u00e1pence<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">Ten\/Ta\/To <strong>Z\u00e1kon<\/strong> Geologicky je mnohem star\u0161\u00ed ne\u017e Alpy. Skl\u00e1d\u00e1 se p\u0159ev\u00e1\u017en\u011b z <strong>v\u00e1penec<\/strong>, kter\u00fd byl ulo\u017een v mo\u0159i p\u0159ed v\u00edce ne\u017e 150 miliony let. V d\u016fsledku tlaku Alp byl zvr\u00e1sn\u011bn sm\u011brem na sever.<\/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>Zdroj:<\/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\">Typick\u00e9 horniny v obdob\u00ed jury<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>v\u00e1penec<\/li>\n\n\n\n<li>sl\u00edn<\/li>\n\n\n\n<li>j\u00edl<\/li>\n<\/ul>\n\n\n\n<h2 class=\"wp-block-heading\">Funkce<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>jemn\u00e9, prot\u00e1hl\u00e9 z\u00e1hyby (v poho\u0159\u00ed Jura typicky ant\u00e9novit\u00e9)<\/li>\n\n\n\n<li>mnoho jeskyn\u00ed (krasov\u00e1 krajina)<\/li>\n\n\n\n<li>rozlehl\u00e9 lesy<\/li>\n\n\n\n<li>N\u00e1horn\u00ed plo\u0161iny a \u00fadol\u00ed<\/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. T\u0159i geologick\u00e9 jednotky v p\u0159\u00edm\u00e9m srovn\u00e1n\u00ed<\/strong><\/h1>\n\n\n\n<figure class=\"wp-block-table\"><table class=\"has-fixed-layout\"><thead><tr><th>kraj<\/th><th>P\u016fvod<\/th><th>sk\u00e1ly<\/th><th>V\u00fd\u0161ka<\/th><th>Krajina<\/th><\/tr><\/thead><tbody><tr><td><strong>Alpy<\/strong><\/td><td>P\u0159ed 30\u20135 miliony let, sr\u00e1\u017eka desek<\/td><td>\u017dula, rula, v\u00e1penec<\/td><td>1 500\u20134 600 m<\/td><td>drsn\u00e9, vysok\u00e9 vrcholy<\/td><\/tr><tr><td><strong>Centr\u00e1ln\u00ed plo\u0161ina<\/strong><\/td><td>Sedimenty z alpsk\u00e9ho \u00fatvaru<\/td><td>Melasa<\/td><td>300\u2013800 m<\/td><td>m\u00edrn\u00e9 pl\u00e1n\u011b<\/td><\/tr><tr><td><strong>Z\u00e1kon<\/strong><\/td><td>P\u0159ed 150\u201310 miliony let, vr\u00e1sn\u011bn\u00ed<\/td><td>v\u00e1penec<\/td><td>800\u20131 600 m<\/td><td>dlouh\u00e9 vr\u00e1sky, kras<\/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. Ledovce formovaly velkou \u010d\u00e1st \u0161v\u00fdcarsk\u00e9 krajiny<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">B\u011bhem posledn\u00edch dob ledov\u00fdch byly velk\u00e9 \u010d\u00e1sti \u0160v\u00fdcarska pokryty ledem. Ledovce:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>modelovan\u00e1 \u00fadol\u00ed (nap\u0159. \u00fadol\u00ed Limmat, Rh\u00f4ny, Reuss)<\/li>\n\n\n\n<li>zanechan\u00e1 jezera (nap\u0159. Cury\u0161sk\u00e9 jezero, Lucernsk\u00e9 jezero, Bodamsk\u00e9 jezero)<\/li>\n\n\n\n<li>p\u0159epravoval obrovsk\u00e9 mno\u017estv\u00ed hornin<\/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\/cs\/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>Zdroj:<\/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\">I dnes ledovce formuj\u00ed Alpy, a\u010dkoliv v\u00fdrazn\u011b ustupuj\u00ed.<\/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. Pro\u010d je geologick\u00e1 rozmanitost \u0160v\u00fdcarska jedine\u010dn\u00e1<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">\u0160v\u00fdcarsko je geologicky unik\u00e1tn\u00ed, proto\u017ee:<\/p>\n\n\n\n<ol class=\"wp-block-list\">\n<li><strong>T\u0159i velk\u00e1 poho\u0159\u00ed na mal\u00e9m \u00fazem\u00ed<\/strong> setkat se.<\/li>\n\n\n\n<li><strong>Des\u00edtky druh\u016f hornin<\/strong> le\u017e\u00ed svisle na sob\u011b.<\/li>\n\n\n\n<li>Jsou jedn\u00edm z <strong>nejl\u00e9pe prozkouman\u00fdch oblast\u00ed na sv\u011bt\u011b<\/strong> je.<\/li>\n\n\n\n<li>Krajina se extr\u00e9mn\u011b li\u0161\u00ed \u2013 od vysok\u00fdch Alp a\u017e po v\u00e1pencov\u00e9 vr\u00e1sny.<\/li>\n\n\n\n<li>Regiony jako Engadin, Wallis nebo Jura <strong>nez\u00e1visl\u00e9 geologick\u00e9 d\u011bjiny<\/strong> m\u00edt.<\/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. Z\u00e1v\u011br<\/strong><\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">Ten\/Ta\/To <strong>Geologie \u0160v\u00fdcarska<\/strong> To vysv\u011btluje, pro\u010d je zem\u011b tak rozmanit\u00e1: vysok\u00e9 Alpy, m\u00edrn\u00e9 podh\u016f\u0159\u00ed, \u0161irok\u00e1 \u0160v\u00fdcarsk\u00e1 plo\u0161ina a vr\u00e1sn\u011bn\u00e9 poho\u0159\u00ed Jura. Jej\u00ed vznik je kombinac\u00ed sr\u00e1\u017eek desek, usazov\u00e1n\u00ed sediment\u016f, vyzdvihov\u00e1n\u00ed a eroze \u2013 geologick\u00e1 historie, kter\u00e1 je viditeln\u00e1 dodnes.<\/p>","protected":false},"excerpt":{"rendered":"Die Geologie der Schweiz ist weltweit einzigartig. 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