{"id":16811,"date":"2020-06-24T13:50:48","date_gmt":"2020-06-24T11:50:48","guid":{"rendered":"https:\/\/www.npsumava.cz\/?page_id=16811"},"modified":"2020-07-27T14:04:45","modified_gmt":"2020-07-27T12:04:45","slug":"naturverhaeltnisse","status":"publish","type":"page","link":"https:\/\/www.npsumava.cz\/de\/natur\/naturverhaeltnisse\/","title":{"rendered":"Naturgegenbenheiten"},"content":{"rendered":"\t\t<div data-elementor-type=\"wp-post\" data-elementor-id=\"16811\" class=\"elementor elementor-16811 elementor-2234\">\n\t\t\t\t\t\t<div class=\"elementor-inner\">\n\t\t\t\t<div class=\"elementor-section-wrap\">\n\t\t\t\t\t\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-560c5a5 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"560c5a5\" data-element_type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t\t\t<div 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class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-image-carousel-wrapper swiper-container\" dir=\"ltr\">\n\t\t\t<div class=\"elementor-image-carousel swiper-wrapper\">\n\t\t\t\t\t\t\t\t<div class=\"swiper-slide\"><a data-elementor-open-lightbox=\"yes\" data-elementor-lightbox-slideshow=\"66aeb92\" data-elementor-lightbox-title=\"Plech\u00fd-Kunc-Vl\" e-action-hash=\"#elementor-action%3Aaction%3Dlightbox%26settings%3DeyJpZCI6NzE1NiwidXJsIjoiaHR0cHM6XC9cL3d3dy5ucHN1bWF2YS5jelwvd3AtY29udGVudFwvdXBsb2Fkc1wvMjAxOVwvMDhcL3BsZWNoeS1rdW5jLXZsLmpwZyIsInNsaWRlc2hvdyI6IjY2YWViOTIifQ%3D%3D\" href=\"https:\/\/www.npsumava.cz\/wp-content\/uploads\/2019\/08\/plechy-kunc-vl.jpg\"><figure class=\"swiper-slide-inner\"><img class=\"swiper-slide-image\" src=\"https:\/\/www.npsumava.cz\/wp-content\/uploads\/elementor\/thumbs\/plechy-kunc-vl-odk11wa8gl42lutm8yxur3c7nybljp8ck671tous7m.jpg\" alt=\"Plech\u00fd-Kunc-Vl\" \/><\/figure><\/a><\/div><div class=\"swiper-slide\"><a 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e-action-hash=\"#elementor-action%3Aaction%3Dlightbox%26settings%3DeyJpZCI6NzE1NCwidXJsIjoiaHR0cHM6XC9cL3d3dy5ucHN1bWF2YS5jelwvd3AtY29udGVudFwvdXBsb2Fkc1wvMjAxOVwvMDhcL21vZHJhdi1zbGF0ZS1ob3Jza2UtdnJjaG8uanBnIiwic2xpZGVzaG93IjoiNjZhZWI5MiJ9\" href=\"https:\/\/www.npsumava.cz\/wp-content\/uploads\/2019\/08\/modrav-slate-horske-vrcho.jpg\"><figure class=\"swiper-slide-inner\"><img class=\"swiper-slide-image\" src=\"https:\/\/www.npsumava.cz\/wp-content\/uploads\/elementor\/thumbs\/modrav-slate-horske-vrcho-odk11x82nf5cxgs93hchbl3o9c6yrec2waujayte1e.jpg\" alt=\"Modrav-slate---horske-vrcho\" \/><\/figure><\/a><\/div>\t\t\t<\/div>\n\t\t\t\t\t\t\t\t\t\t\t\t<div class=\"swiper-pagination\"><\/div>\n\t\t\t\t\t\t\t\t\t\t\t\t\t<div class=\"elementor-swiper-button elementor-swiper-button-prev\">\n\t\t\t\t\t\t<i aria-hidden=\"true\" class=\"eicon-chevron-left\"><\/i>\t\t\t\t\t\t<span class=\"elementor-screen-only\">Zur\u00fcck<\/span>\n\t\t\t\t\t<\/div>\n\t\t\t\t\t<div class=\"elementor-swiper-button elementor-swiper-button-next\">\n\t\t\t\t\t\t<i aria-hidden=\"true\" class=\"eicon-chevron-right\"><\/i>\t\t\t\t\t\t<span class=\"elementor-screen-only\">Weiter<\/span>\n\t\t\t\t\t<\/div>\n\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"elementor-column elementor-col-50 elementor-top-column elementor-element elementor-element-7ae2750\" data-id=\"7ae2750\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-column-wrap elementor-element-populated\">\n\t\t\t\t\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-820238f elementor-widget elementor-widget-text-editor\" data-id=\"820238f\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t<div class=\"elementor-text-editor elementor-clearfix\">\n\t\t\t\t<p><span lang=\"DE\">Geologische, p\u00e4dologische und geomorphologische Bedingungen stellen grundlegende Voraussetzungen f\u00fcr die Entwicklung der Vegetation und die Grundwasser- und Oberfl\u00e4chenwasserregelung dar. <\/span><\/p><p><span lang=\"DE\">Der gr\u00f6\u00dfte Teil des Gebiets geh\u00f6rt zu dem geomorphologischen Komplex <b>B\u00f6hmerwald<\/b> und zum Teil zu dem <b>B\u00f6hmerwald-Gebirgsvorland<\/b>, das einen Teil des <b>B\u00f6hmerwald-Hochlands<\/b> bildet.<\/span><\/p><p><span lang=\"DE\">Der B\u00f6hmerwald z\u00e4hlt zu den \u00e4ltesten Gebirgen Mitteleuropas. Er weist Erhebungen von rund 700 m. \u00fc. d. M. auf und seine h\u00f6chsten Gipfel, nur auf der bayerischen Seite, \u00fcberragen 1400\u00a0m.<\/span><\/p><p><span lang=\"DE\">Im Quart\u00e4r tieften die Gletscher morphologisch markante Kare, von denen die meisten heute mit Wasser gef\u00fcllt sind. In der gleichen Zeit entstanden auch einige weitere auff\u00e4llige Gel\u00e4ndeformen wie Frostbl\u00f6cke, Felsenw\u00e4lle oder Hang-Steinsch\u00fctten. <\/span><\/p><p>\u00a0<\/p>\t\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-e24c24b elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"e24c24b\" data-element_type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t\t\t<div class=\"elementor-row\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-98d6283\" data-id=\"98d6283\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-column-wrap elementor-element-populated\">\n\t\t\t\t\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-7b7467d elementor-align-left elementor-icon-list--layout-traditional elementor-list-item-link-full_width elementor-widget elementor-widget-icon-list\" data-id=\"7b7467d\" data-element_type=\"widget\" data-widget_type=\"icon-list.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<ul class=\"elementor-icon-list-items\">\n\t\t\t\t\t\t\t<li class=\"elementor-icon-list-item\">\n\t\t\t\t\t\t\t\t\t\t\t<span class=\"elementor-icon-list-icon\">\n\t\t\t\t\t\t\t<i aria-hidden=\"true\" class=\"fas fa-circle\"><\/i>\t\t\t\t\t\t<\/span>\n\t\t\t\t\t\t\t\t\t\t<span class=\"elementor-icon-list-text\">Der h\u00f6chste Gipfel auf der b\u00f6hmischen Seite ist der Plech\u00fd (1378 m. \u00fc. d. M.).<\/span>\n\t\t\t\t\t\t\t\t\t<\/li>\n\t\t\t\t\t\t\t\t<li class=\"elementor-icon-list-item\">\n\t\t\t\t\t\t\t\t\t\t\t<span class=\"elementor-icon-list-icon\">\n\t\t\t\t\t\t\t<i aria-hidden=\"true\" class=\"fas fa-circle\"><\/i>\t\t\t\t\t\t<\/span>\n\t\t\t\t\t\t\t\t\t\t<span class=\"elementor-icon-list-text\">Den Kern des Gebirges bildet das Plateau \u0160umavsk\u00e9 pl\u00e1n\u011b, eine ausgedehnte Bergebene mit einer Meeresh\u00f6he von rund 1000 m.<\/span>\n\t\t\t\t\t\t\t\t\t<\/li>\n\t\t\t\t\t\t\t\t<li class=\"elementor-icon-list-item\">\n\t\t\t\t\t\t\t\t\t\t\t<span class=\"elementor-icon-list-icon\">\n\t\t\t\t\t\t\t<i aria-hidden=\"true\" class=\"fas fa-circle\"><\/i>\t\t\t\t\t\t<\/span>\n\t\t\t\t\t\t\t\t\t\t<span class=\"elementor-icon-list-text\">Richtung Nordwesten verl\u00e4uft das Bergland \u017deleznorudsk\u00e1 hornatina und Richtung S\u00fcdosten der Bergkamm des Berglands Trojmezensk\u00e1 hornatina und der inl\u00e4ndische Kamm des Berglands Boub\u00ednsk\u00e1 und \u017delnavsk\u00e1 hornatina, die von dem flachen Tal Vltavick\u00e1 br\u00e1zda voneinander getrennt sind. <\/span>\n\t\t\t\t\t\t\t\t\t<\/li>\n\t\t\t\t\t\t\t\t<li class=\"elementor-icon-list-item\">\n\t\t\t\t\t\t\t\t\t\t\t<span class=\"elementor-icon-list-icon\">\n\t\t\t\t\t\t\t<i aria-hidden=\"true\" class=\"fas fa-circle\"><\/i>\t\t\t\t\t\t<\/span>\n\t\t\t\t\t\t\t\t\t\t<span class=\"elementor-icon-list-text\">Ganz spezifische Gebilde sind ausgedehnte, m\u00e4\u00dfig gew\u00f6lbte Hochmoore sowie Niedermoore. <\/span>\n\t\t\t\t\t\t\t\t\t<\/li>\n\t\t\t\t\t\t<\/ul>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t","protected":false},"excerpt":{"rendered":"<p>P\u0159edchoz\u00ed Dal\u0161\u00ed Geologische, p\u00e4dologische und geomorphologische Bedingungen stellen grundlegende Voraussetzungen f\u00fcr die Entwicklung der Vegetation und die Grundwasser- und Oberfl\u00e4chenwasserregelung dar. Der gr\u00f6\u00dfte Teil des Gebiets geh\u00f6rt zu dem geomorphologischen Komplex B\u00f6hmerwald und zum Teil zu dem B\u00f6hmerwald-Gebirgsvorland, das einen Teil des B\u00f6hmerwald-Hochlands bildet. Der B\u00f6hmerwald z\u00e4hlt zu den \u00e4ltesten Gebirgen Mitteleuropas. Er weist Erhebungen&#8230;<\/p>\n","protected":false},"author":2,"featured_media":24838,"parent":16772,"menu_order":227,"comment_status":"closed","ping_status":"closed","template":"","meta":[],"acf":[],"_links":{"self":[{"href":"https:\/\/www.npsumava.cz\/de\/wp-json\/wp\/v2\/pages\/16811"}],"collection":[{"href":"https:\/\/www.npsumava.cz\/de\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.npsumava.cz\/de\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.npsumava.cz\/de\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/www.npsumava.cz\/de\/wp-json\/wp\/v2\/comments?post=16811"}],"version-history":[{"count":0,"href":"https:\/\/www.npsumava.cz\/de\/wp-json\/wp\/v2\/pages\/16811\/revisions"}],"up":[{"embeddable":true,"href":"https:\/\/www.npsumava.cz\/de\/wp-json\/wp\/v2\/pages\/16772"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.npsumava.cz\/de\/wp-json\/wp\/v2\/media\/24838"}],"wp:attachment":[{"href":"https:\/\/www.npsumava.cz\/de\/wp-json\/wp\/v2\/media?parent=16811"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}