{"id":5191,"date":"2018-03-01T14:49:33","date_gmt":"2018-03-01T13:49:33","guid":{"rendered":"https:\/\/www.geoparcoalpicarniche.org\/?page_id=5191"},"modified":"2018-03-08T16:07:09","modified_gmt":"2018-03-08T15:07:09","slug":"karren","status":"publish","type":"page","link":"https:\/\/www.geoparcoalpicarniche.org\/de\/das-gebiet\/karstformen\/karren\/","title":{"rendered":"Karren"},"content":{"rendered":"<div id=\"pl-5191\"  class=\"panel-layout\" ><div id=\"pg-5191-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-5191-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-5191-0-0-0\" class=\"so-panel widget widget_nav_menu panel-first-child panel-last-child\" data-index=\"0\" ><div class=\"menu-territorio-tedesco-container\"><ul id=\"menu-territorio-tedesco\" class=\"menu\"><li id=\"menu-item-5114\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-has-children menu-item-5114\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/de\/das-gebiet\/\">Das Gebiet<\/a>\n<ul class=\"sub-menu\">\n\t<li id=\"menu-item-5305\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-5305\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/de\/das-gebiet\/geomorfologia\/\">Geomorphologie<\/a><\/li>\n\t<li id=\"menu-item-5116\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-has-children menu-item-5116\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/de\/das-gebiet\/palaeontologie\/\">Pal\u00e4ontologie<\/a>\n\t<ul class=\"sub-menu\">\n\t\t<li id=\"menu-item-5117\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-5117\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/de\/das-gebiet\/palaeontologie\/fossil\/\">Fossilien<\/a><\/li>\n\t<\/ul>\n<\/li>\n\t<li id=\"menu-item-5118\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-5118\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/de\/das-gebiet\/geoseiten\/\">Geopunkte<\/a><\/li>\n\t<li id=\"menu-item-7593\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-7593\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/de\/das-gebiet\/geotopen\/\">Geotopen<\/a><\/li>\n\t<li id=\"menu-item-5119\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-has-children menu-item-5119\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/de\/das-gebiet\/karstformen\/\">Karstformen<\/a>\n\t<ul class=\"sub-menu\">\n\t\t<li id=\"menu-item-5306\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-5306\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/de\/das-gebiet\/karstformen\/hoehlen\/\">H\u00f6hlen<\/a><\/li>\n\t\t<li id=\"menu-item-5307\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-5307\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/de\/das-gebiet\/karstformen\/karren\/\">Karren<\/a><\/li>\n\t\t<li id=\"menu-item-5308\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-5308\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/de\/das-gebiet\/karstformen\/klammen\/\">Klammen<\/a><\/li>\n\t<\/ul>\n<\/li>\n\t<li id=\"menu-item-5120\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-5120\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/de\/das-gebiet\/bergbauseiten\/\">Steinbr\u00fcche und Minen<\/a><\/li>\n\t<li id=\"menu-item-7217\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-7217\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/de\/das-gebiet\/publikationen-download\/\">Publikationen Download<\/a><\/li>\n<\/ul>\n<\/li>\n<\/ul><\/div><\/div><\/div><div id=\"pgc-5191-0-1\"  class=\"panel-grid-cell\" ><div class=\"paddingContentWithSidebar panel-cell-style panel-cell-style-for-5191-0-1\" ><div id=\"panel-5191-0-1-0\" class=\"so-panel widget widget_sow-editor panel-first-child\" data-index=\"1\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<h2>Karren<\/h2>\n<\/div>\n<\/div><\/div><div id=\"panel-5191-0-1-1\" class=\"so-panel widget widget_siteorigin-panels-builder\" data-index=\"2\" ><div id=\"pl-w5a9d6fd2500e4\"  class=\"panel-layout\" ><div id=\"pg-w5a9d6fd2500e4-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-w5a9d6fd2500e4-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-w5a9d6fd2500e4-0-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<p>Tra le forme carsiche superficiali, campi solcati e doline sono molto frequenti sul territorio del Geoparco. I campi solcati si formano dove le rocce carbonatiche sono abbastanza pure e allo scoperto: \u00e8 comune, in questi luoghi, osservare fenomeni di dissoluzione di superficie, come scannellature, campi solcati a doccia e vaschette di corrosione.<\/p>\n<\/div>\n<\/div><\/div><\/div><div id=\"pgc-w5a9d6fd2500e4-0-1\"  class=\"panel-grid-cell\" ><div id=\"panel-w5a9d6fd2500e4-0-1-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"1\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<div id='gallery-1' class='gallery galleryid-5191 gallery-columns-1 gallery-size-full'><figure class='gallery-item'>\n\t\t\t<div class='gallery-icon landscape'>\n\t\t\t\t<a href='https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/21.Rocce-carsif_Karren_CaseraBordaglia-1280-1.jpg'><img loading=\"lazy\" decoding=\"async\" width=\"1280\" height=\"720\" src=\"https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/21.Rocce-carsif_Karren_CaseraBordaglia-1280-1.jpg\" class=\"attachment-full size-full\" alt=\"\" srcset=\"https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/21.Rocce-carsif_Karren_CaseraBordaglia-1280-1.jpg 1280w, https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/21.Rocce-carsif_Karren_CaseraBordaglia-1280-1-300x169.jpg 300w, https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/21.Rocce-carsif_Karren_CaseraBordaglia-1280-1-768x432.jpg 768w, https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/21.Rocce-carsif_Karren_CaseraBordaglia-1280-1-1024x576.jpg 1024w, https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/21.Rocce-carsif_Karren_CaseraBordaglia-1280-1-428x242.jpg 428w\" sizes=\"auto, (max-width: 1280px) 100vw, 1280px\" \/><\/a>\n\t\t\t<\/div><\/figure>\n\t\t<\/div>\n\n<\/div>\n<\/div><\/div><\/div><\/div><\/div><\/div><div id=\"panel-5191-0-1-2\" class=\"so-panel widget widget_siteorigin-panels-builder\" data-index=\"3\" ><div class=\"mb panel-widget-style panel-widget-style-for-5191-0-1-2\" ><div id=\"pl-w5a9d6fd2502c5\"  class=\"panel-layout\" ><div id=\"pg-w5a9d6fd2502c5-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-w5a9d6fd2502c5-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-w5a9d6fd2502c5-0-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<p>La dimensione dei campi solcati, all\u2019origine di varie leggende (i vari \u201csentieri dei giganti\u201d), pu\u00f2 arrivare a qualche metro di lunghezza e al decimetro come larghezza, mentre la profondit\u00e0 non supera mai la decina di centimetri.<\/p>\n<p>In corrispondenza di tratti pianeggianti, invece, non \u00e8 raro incontrare doline: i litotipi del Permiano esposti in superficie possono venire profondamente corrosi dalle acque di superficie, dando origine, a causa della solubilizzazione della frazione gessosa, a particolari morfologie quali calanchi, frane, crolli, pinnacoli, cavernosit\u00e0 ecc.<\/p>\n<div class=\"mt\">\n<div id='gallery-2' class='gallery galleryid-5191 gallery-columns-1 gallery-size-full'><figure class='gallery-item'>\n\t\t\t<div class='gallery-icon landscape'>\n\t\t\t\t<a href='https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/20.Carsismo-sup_cop_Pizzul-Zermula-da-torbiera-Valdolce-1280.jpg'><img loading=\"lazy\" decoding=\"async\" width=\"1280\" height=\"585\" src=\"https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/20.Carsismo-sup_cop_Pizzul-Zermula-da-torbiera-Valdolce-1280.jpg\" class=\"attachment-full size-full\" alt=\"\" srcset=\"https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/20.Carsismo-sup_cop_Pizzul-Zermula-da-torbiera-Valdolce-1280.jpg 1280w, https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/20.Carsismo-sup_cop_Pizzul-Zermula-da-torbiera-Valdolce-1280-300x137.jpg 300w, https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/20.Carsismo-sup_cop_Pizzul-Zermula-da-torbiera-Valdolce-1280-768x351.jpg 768w, https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/20.Carsismo-sup_cop_Pizzul-Zermula-da-torbiera-Valdolce-1280-1024x468.jpg 1024w\" sizes=\"auto, (max-width: 1280px) 100vw, 1280px\" \/><\/a>\n\t\t\t<\/div><\/figure>\n\t\t<\/div>\n\n<\/div>\n<\/div>\n<\/div><\/div><\/div><\/div><\/div><\/div><\/div><div id=\"panel-5191-0-1-3\" class=\"so-panel widget widget_sow-editor\" data-index=\"4\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<h2>Per farsi un\u2019idea<\/h2>\n<p><strong>Qualche esempio di forme carsiche superficiali nell\u2019area del Geoparco<\/strong><\/p>\n<\/div>\n<\/div><\/div><div id=\"panel-5191-0-1-4\" class=\"so-panel widget widget_siteorigin-panels-builder\" data-index=\"5\" ><div class=\"mb panel-widget-style panel-widget-style-for-5191-0-1-4\" ><div id=\"pl-w5a9d705635761\"  class=\"panel-layout\" ><div id=\"pg-w5a9d705635761-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-w5a9d705635761-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-w5a9d705635761-0-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<h3 class=\"mb-none\">Monte Verzegnis<\/h3>\n<p class=\"zona\">Area: Val Tagliamento e Prealpi Tolmezzine<\/p>\n<p>Tra le aree con maggiore variet\u00e0 di morfologie carsiche superficiali c\u2019\u00e8 sicuramente quella del Monte Verzegnis.<br \/>\nTra le macroforme sono frequenti le doline, che interessano principalmente terreni prativi di alta montagna. I pi\u00f9 vistosi si trovano nell\u2019imbuto di Casera Val, nei falsipiani sottostanti Sella Chianalete e Cima Cormolina, nei dintorni delle Casere Lovinzola, nell\u2019imbuto sotto la vetta del Lovinzola.<br \/>\nSi tratta principalmente di doline dalle pareti molto arrotondate, quindi generate per dissoluzione, con un diametro variabile mediamente dai 2 ai 10 metri (ma alcune possono raggiungere i 50 metri). Talvolta risultano allineate lungo evidenti linee di frattura.<br \/>\nSi trovano anche dei piccoli uvala, composti dalla saldatura di 3-4 doline. Non mancano le doline di crollo e i pozzi a neve.<br \/>\nTra le microforme si possono osservare i campi solcati a doccia (Rinnenkarren), di una lunghezza che pu\u00f2 arrivare anche a 10 metri a scannellature (Rillenkarren) simili ai calanchi, ove gli spigoli vivi delle rocce sono stati trasformati dal fenomeno carsico in affilati taglienti. Pi\u00f9 raramente si incontrano minuscoli meandri semipianeggianti e piccole vaschette di corrosione (Kamenitza).<\/p>\n<\/div>\n<\/div><\/div><\/div><div id=\"pgc-w5a9d705635761-0-1\"  class=\"panel-grid-cell\" ><div id=\"panel-w5a9d705635761-0-1-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"1\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<\/div>\n<\/div><\/div><\/div><\/div><\/div><\/div><\/div><div id=\"panel-5191-0-1-5\" class=\"so-panel widget widget_siteorigin-panels-builder\" data-index=\"6\" ><div class=\"mb panel-widget-style panel-widget-style-for-5191-0-1-5\" ><div id=\"pl-w5a9d7056357dc\"  class=\"panel-layout\" ><div id=\"pg-w5a9d7056357dc-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-w5a9d7056357dc-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-w5a9d7056357dc-0-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<h3 class=\"mb-none\">Pian di Lanza e Val Dolce<\/h3>\n<p class=\"zona\">area: Alpi Carniche Occidentali \u2013 Alpi Carniche Orientali<\/p>\n<p>Sul Pian di Lanza, al confine con l\u2019Austria, nei territori tra Paularo e Pontebba, sono presenti doline ancora ben visibili, nonostante l\u2019azione di modellamento glaciale.<\/p>\n<\/div>\n<\/div><\/div><\/div><div id=\"pgc-w5a9d7056357dc-0-1\"  class=\"panel-grid-cell\" ><div id=\"panel-w5a9d7056357dc-0-1-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"1\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<div id='gallery-3' class='gallery galleryid-5191 gallery-columns-1 gallery-size-full'><figure class='gallery-item'>\n\t\t\t<div class='gallery-icon landscape'>\n\t\t\t\t<a href='https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/22.Doline-Val-Dolce-Paularo-1280-1.jpg'><img loading=\"lazy\" decoding=\"async\" width=\"1280\" height=\"860\" src=\"https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/22.Doline-Val-Dolce-Paularo-1280-1.jpg\" class=\"attachment-full size-full\" alt=\"\" srcset=\"https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/22.Doline-Val-Dolce-Paularo-1280-1.jpg 1280w, https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/22.Doline-Val-Dolce-Paularo-1280-1-300x202.jpg 300w, https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/22.Doline-Val-Dolce-Paularo-1280-1-768x516.jpg 768w, https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/22.Doline-Val-Dolce-Paularo-1280-1-1024x688.jpg 1024w, https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/22.Doline-Val-Dolce-Paularo-1280-1-272x182.jpg 272w\" sizes=\"auto, (max-width: 1280px) 100vw, 1280px\" \/><\/a>\n\t\t\t<\/div><\/figure>\n\t\t<\/div>\n\n<\/div>\n<\/div><\/div><\/div><\/div><\/div><\/div><\/div><div id=\"panel-5191-0-1-6\" class=\"so-panel widget widget_siteorigin-panels-builder\" data-index=\"7\" ><div class=\"mb panel-widget-style panel-widget-style-for-5191-0-1-6\" ><div id=\"pl-w5a9d7056359a7\"  class=\"panel-layout\" ><div id=\"pg-w5a9d7056359a7-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-w5a9d7056359a7-0-0\"  class=\"panel-grid-cell panel-grid-cell-mobile-last\" ><div id=\"panel-w5a9d7056359a7-0-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<h3 class=\"mb-none\">Paluzza,<\/h3>\n<p class=\"zona\">Area: Alpi Carniche Occidentali<\/p>\n<p>Nell\u2019area di Timau, nei pressi del Pal Piccolo sono visibili varie forme di carsismo superficiale, come i campi solcati<\/p>\n<\/div>\n<\/div><\/div><\/div><div id=\"pgc-w5a9d7056359a7-0-1\"  class=\"panel-grid-cell panel-grid-cell-empty\" ><\/div><\/div><\/div><\/div><\/div><div id=\"panel-5191-0-1-7\" class=\"so-panel widget widget_siteorigin-panels-builder\" data-index=\"8\" ><div class=\"mb panel-widget-style panel-widget-style-for-5191-0-1-7\" ><div id=\"pl-w5a9d7056359f6\"  class=\"panel-layout\" ><div id=\"pg-w5a9d7056359f6-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-w5a9d7056359f6-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-w5a9d7056359f6-0-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<h3 class=\"mb-none\">Paluzza<\/h3>\n<p class=\"zona\">Area: Alpi Carniche Occidentali<\/p>\n<p><strong>Nell\u2019area della Chianevate, presso Casera Monumenz<\/strong>, a quota 1950-2000 metri si possono osservare singolari morfologie carsiche a crepacci sviluppate nei calcari devoniani e denominate, appunto, Monumenz (in friulano, monumenti) per la loro particolare forma.<\/p>\n<\/div>\n<\/div><\/div><\/div><div id=\"pgc-w5a9d7056359f6-0-1\"  class=\"panel-grid-cell\" ><div id=\"panel-w5a9d7056359f6-0-1-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"1\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<div id='gallery-4' class='gallery galleryid-5191 gallery-columns-1 gallery-size-full'><figure class='gallery-item'>\n\t\t\t<div class='gallery-icon landscape'>\n\t\t\t\t<a href='https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/23.Campi-solcati-Casera-Monumenz-1280.jpg'><img loading=\"lazy\" decoding=\"async\" width=\"1280\" height=\"860\" src=\"https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/23.Campi-solcati-Casera-Monumenz-1280.jpg\" class=\"attachment-full size-full\" alt=\"\" srcset=\"https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/23.Campi-solcati-Casera-Monumenz-1280.jpg 1280w, https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/23.Campi-solcati-Casera-Monumenz-1280-300x202.jpg 300w, https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/23.Campi-solcati-Casera-Monumenz-1280-768x516.jpg 768w, https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/23.Campi-solcati-Casera-Monumenz-1280-1024x688.jpg 1024w, https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/23.Campi-solcati-Casera-Monumenz-1280-272x182.jpg 272w\" sizes=\"auto, (max-width: 1280px) 100vw, 1280px\" \/><\/a>\n\t\t\t<\/div><\/figure>\n\t\t<\/div>\n\n<\/div>\n<\/div><\/div><\/div><\/div><\/div><\/div><\/div><div id=\"panel-5191-0-1-8\" class=\"so-panel widget widget_siteorigin-panels-builder panel-last-child\" data-index=\"9\" ><div class=\"mb panel-widget-style panel-widget-style-for-5191-0-1-8\" ><div id=\"pl-w69f6508a3757e\"  class=\"panel-layout\" ><div id=\"pg-w69f6508a3757e-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-w69f6508a3757e-0-0\"  class=\"panel-grid-cell panel-grid-cell-mobile-last\" ><div id=\"panel-w69f6508a3757e-0-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<h3 class=\"mb-none\">Sauris<\/h3>\n<p class=\"zona\">Area: Alpi Carniche Occidentali<\/p>\n<p><strong>Presso Sella Malins, a nord di Sauris<\/strong>, si possono osservare numerose <strong>doline di suffusione<\/strong>: si tratta di depressioni doliniformi in rocce non carsificabili, sprofondamenti in genere perfettamente circolari dovuti a collassi per adattamento del substrato a vuoti che si generano in rocce solubili sottostanti.<\/p>\n<\/div>\n<\/div><\/div><\/div><div id=\"pgc-w69f6508a3757e-0-1\"  class=\"panel-grid-cell panel-grid-cell-empty\" ><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div>","protected":false},"excerpt":{"rendered":"<p>Karren Per farsi un\u2019idea Qualche esempio di forme carsiche superficiali nell\u2019area del Geoparco<\/p>\n","protected":false},"author":2,"featured_media":3041,"parent":4979,"menu_order":91,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_acf_changed":false,"inline_featured_image":false,"ngg_post_thumbnail":0,"footnotes":""},"class_list":{"0":"post-5191","1":"page","2":"type-page","3":"status-publish","4":"has-post-thumbnail","6":"clearfix","7":"article"},"acf":[],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.5 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>Karren - Geoparco Alpi Carniche<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/www.geoparcoalpicarniche.org\/de\/das-gebiet\/karstformen\/karren\/\" \/>\n<meta property=\"og:locale\" content=\"de_DE\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Karren - Geoparco Alpi Carniche\" \/>\n<meta property=\"og:description\" content=\"Karren Per farsi un\u2019idea Qualche esempio di forme carsiche superficiali nell\u2019area del Geoparco\" \/>\n<meta property=\"og:url\" content=\"https:\/\/www.geoparcoalpicarniche.org\/de\/das-gebiet\/karstformen\/karren\/\" \/>\n<meta property=\"og:site_name\" content=\"Geoparco Alpi Carniche\" \/>\n<meta property=\"article:modified_time\" content=\"2018-03-08T15:07:09+00:00\" \/>\n<meta property=\"og:image\" content=\"https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/0.COPERTINA-SEZ_Grotta-Magico-Alverman.jpg\" \/>\n\t<meta property=\"og:image:width\" content=\"3008\" \/>\n\t<meta property=\"og:image:height\" content=\"2000\" \/>\n\t<meta property=\"og:image:type\" content=\"image\/jpeg\" \/>\n<meta name=\"twitter:card\" content=\"summary_large_image\" \/>\n<meta name=\"twitter:label1\" content=\"Gesch\u00e4tzte Lesezeit\" \/>\n\t<meta name=\"twitter:data1\" content=\"3 minutes\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\\\/\\\/schema.org\",\"@graph\":[{\"@type\":\"WebPage\",\"@id\":\"https:\\\/\\\/www.geoparcoalpicarniche.org\\\/de\\\/das-gebiet\\\/karstformen\\\/karren\\\/\",\"url\":\"https:\\\/\\\/www.geoparcoalpicarniche.org\\\/de\\\/das-gebiet\\\/karstformen\\\/karren\\\/\",\"name\":\"Karren - Geoparco Alpi Carniche\",\"isPartOf\":{\"@id\":\"https:\\\/\\\/www.geoparcoalpicarniche.org\\\/de\\\/#website\"},\"primaryImageOfPage\":{\"@id\":\"https:\\\/\\\/www.geoparcoalpicarniche.org\\\/de\\\/das-gebiet\\\/karstformen\\\/karren\\\/#primaryimage\"},\"image\":{\"@id\":\"https:\\\/\\\/www.geoparcoalpicarniche.org\\\/de\\\/das-gebiet\\\/karstformen\\\/karren\\\/#primaryimage\"},\"thumbnailUrl\":\"https:\\\/\\\/www.geoparcoalpicarniche.org\\\/wp-content\\\/uploads\\\/2018\\\/01\\\/0.COPERTINA-SEZ_Grotta-Magico-Alverman.jpg\",\"datePublished\":\"2018-03-01T13:49:33+00:00\",\"dateModified\":\"2018-03-08T15:07:09+00:00\",\"breadcrumb\":{\"@id\":\"https:\\\/\\\/www.geoparcoalpicarniche.org\\\/de\\\/das-gebiet\\\/karstformen\\\/karren\\\/#breadcrumb\"},\"inLanguage\":\"de-DE\",\"potentialAction\":[{\"@type\":\"ReadAction\",\"target\":[\"https:\\\/\\\/www.geoparcoalpicarniche.org\\\/de\\\/das-gebiet\\\/karstformen\\\/karren\\\/\"]}]},{\"@type\":\"ImageObject\",\"inLanguage\":\"de-DE\",\"@id\":\"https:\\\/\\\/www.geoparcoalpicarniche.org\\\/de\\\/das-gebiet\\\/karstformen\\\/karren\\\/#primaryimage\",\"url\":\"https:\\\/\\\/www.geoparcoalpicarniche.org\\\/wp-content\\\/uploads\\\/2018\\\/01\\\/0.COPERTINA-SEZ_Grotta-Magico-Alverman.jpg\",\"contentUrl\":\"https:\\\/\\\/www.geoparcoalpicarniche.org\\\/wp-content\\\/uploads\\\/2018\\\/01\\\/0.COPERTINA-SEZ_Grotta-Magico-Alverman.jpg\",\"width\":3008,\"height\":2000},{\"@type\":\"BreadcrumbList\",\"@id\":\"https:\\\/\\\/www.geoparcoalpicarniche.org\\\/de\\\/das-gebiet\\\/karstformen\\\/karren\\\/#breadcrumb\",\"itemListElement\":[{\"@type\":\"ListItem\",\"position\":1,\"name\":\"Home\",\"item\":\"https:\\\/\\\/www.geoparcoalpicarniche.org\\\/de\\\/\"},{\"@type\":\"ListItem\",\"position\":2,\"name\":\"Das Gebiet\",\"item\":\"https:\\\/\\\/www.geoparcoalpicarniche.org\\\/de\\\/das-gebiet\\\/\"},{\"@type\":\"ListItem\",\"position\":3,\"name\":\"Karstformen\",\"item\":\"https:\\\/\\\/www.geoparcoalpicarniche.org\\\/de\\\/das-gebiet\\\/karstformen\\\/\"},{\"@type\":\"ListItem\",\"position\":4,\"name\":\"Karren\"}]},{\"@type\":\"WebSite\",\"@id\":\"https:\\\/\\\/www.geoparcoalpicarniche.org\\\/de\\\/#website\",\"url\":\"https:\\\/\\\/www.geoparcoalpicarniche.org\\\/de\\\/\",\"name\":\"Geoparco Alpi Carniche\",\"description\":\"Custode del patrimonio geologico transfrontaliero\",\"potentialAction\":[{\"@type\":\"SearchAction\",\"target\":{\"@type\":\"EntryPoint\",\"urlTemplate\":\"https:\\\/\\\/www.geoparcoalpicarniche.org\\\/de\\\/?s={search_term_string}\"},\"query-input\":{\"@type\":\"PropertyValueSpecification\",\"valueRequired\":true,\"valueName\":\"search_term_string\"}}],\"inLanguage\":\"de-DE\"}]}<\/script>\n<!-- \/ Yoast SEO plugin. -->","yoast_head_json":{"title":"Karren - Geoparco Alpi Carniche","robots":{"index":"index","follow":"follow","max-snippet":"max-snippet:-1","max-image-preview":"max-image-preview:large","max-video-preview":"max-video-preview:-1"},"canonical":"https:\/\/www.geoparcoalpicarniche.org\/de\/das-gebiet\/karstformen\/karren\/","og_locale":"de_DE","og_type":"article","og_title":"Karren - Geoparco Alpi Carniche","og_description":"Karren Per farsi un\u2019idea Qualche esempio di forme carsiche superficiali nell\u2019area del Geoparco","og_url":"https:\/\/www.geoparcoalpicarniche.org\/de\/das-gebiet\/karstformen\/karren\/","og_site_name":"Geoparco Alpi Carniche","article_modified_time":"2018-03-08T15:07:09+00:00","og_image":[{"width":3008,"height":2000,"url":"https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/0.COPERTINA-SEZ_Grotta-Magico-Alverman.jpg","type":"image\/jpeg"}],"twitter_card":"summary_large_image","twitter_misc":{"Gesch\u00e4tzte Lesezeit":"3 minutes"},"schema":{"@context":"https:\/\/schema.org","@graph":[{"@type":"WebPage","@id":"https:\/\/www.geoparcoalpicarniche.org\/de\/das-gebiet\/karstformen\/karren\/","url":"https:\/\/www.geoparcoalpicarniche.org\/de\/das-gebiet\/karstformen\/karren\/","name":"Karren - Geoparco Alpi Carniche","isPartOf":{"@id":"https:\/\/www.geoparcoalpicarniche.org\/de\/#website"},"primaryImageOfPage":{"@id":"https:\/\/www.geoparcoalpicarniche.org\/de\/das-gebiet\/karstformen\/karren\/#primaryimage"},"image":{"@id":"https:\/\/www.geoparcoalpicarniche.org\/de\/das-gebiet\/karstformen\/karren\/#primaryimage"},"thumbnailUrl":"https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/0.COPERTINA-SEZ_Grotta-Magico-Alverman.jpg","datePublished":"2018-03-01T13:49:33+00:00","dateModified":"2018-03-08T15:07:09+00:00","breadcrumb":{"@id":"https:\/\/www.geoparcoalpicarniche.org\/de\/das-gebiet\/karstformen\/karren\/#breadcrumb"},"inLanguage":"de-DE","potentialAction":[{"@type":"ReadAction","target":["https:\/\/www.geoparcoalpicarniche.org\/de\/das-gebiet\/karstformen\/karren\/"]}]},{"@type":"ImageObject","inLanguage":"de-DE","@id":"https:\/\/www.geoparcoalpicarniche.org\/de\/das-gebiet\/karstformen\/karren\/#primaryimage","url":"https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/0.COPERTINA-SEZ_Grotta-Magico-Alverman.jpg","contentUrl":"https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/0.COPERTINA-SEZ_Grotta-Magico-Alverman.jpg","width":3008,"height":2000},{"@type":"BreadcrumbList","@id":"https:\/\/www.geoparcoalpicarniche.org\/de\/das-gebiet\/karstformen\/karren\/#breadcrumb","itemListElement":[{"@type":"ListItem","position":1,"name":"Home","item":"https:\/\/www.geoparcoalpicarniche.org\/de\/"},{"@type":"ListItem","position":2,"name":"Das Gebiet","item":"https:\/\/www.geoparcoalpicarniche.org\/de\/das-gebiet\/"},{"@type":"ListItem","position":3,"name":"Karstformen","item":"https:\/\/www.geoparcoalpicarniche.org\/de\/das-gebiet\/karstformen\/"},{"@type":"ListItem","position":4,"name":"Karren"}]},{"@type":"WebSite","@id":"https:\/\/www.geoparcoalpicarniche.org\/de\/#website","url":"https:\/\/www.geoparcoalpicarniche.org\/de\/","name":"Geoparco Alpi Carniche","description":"Custode del patrimonio geologico transfrontaliero","potentialAction":[{"@type":"SearchAction","target":{"@type":"EntryPoint","urlTemplate":"https:\/\/www.geoparcoalpicarniche.org\/de\/?s={search_term_string}"},"query-input":{"@type":"PropertyValueSpecification","valueRequired":true,"valueName":"search_term_string"}}],"inLanguage":"de-DE"}]}},"_links":{"self":[{"href":"https:\/\/www.geoparcoalpicarniche.org\/de\/wp-json\/wp\/v2\/pages\/5191","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.geoparcoalpicarniche.org\/de\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.geoparcoalpicarniche.org\/de\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.geoparcoalpicarniche.org\/de\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/www.geoparcoalpicarniche.org\/de\/wp-json\/wp\/v2\/comments?post=5191"}],"version-history":[{"count":5,"href":"https:\/\/www.geoparcoalpicarniche.org\/de\/wp-json\/wp\/v2\/pages\/5191\/revisions"}],"predecessor-version":[{"id":6821,"href":"https:\/\/www.geoparcoalpicarniche.org\/de\/wp-json\/wp\/v2\/pages\/5191\/revisions\/6821"}],"up":[{"embeddable":true,"href":"https:\/\/www.geoparcoalpicarniche.org\/de\/wp-json\/wp\/v2\/pages\/4979"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.geoparcoalpicarniche.org\/de\/wp-json\/wp\/v2\/media\/3041"}],"wp:attachment":[{"href":"https:\/\/www.geoparcoalpicarniche.org\/de\/wp-json\/wp\/v2\/media?parent=5191"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}