{"id":4235,"date":"2018-01-29T14:16:49","date_gmt":"2018-01-29T13:16:49","guid":{"rendered":"https:\/\/www.geoparcoalpicarniche.org\/?page_id=4235"},"modified":"2020-03-11T10:16:38","modified_gmt":"2020-03-11T09:16:38","slug":"campi-solcati","status":"publish","type":"page","link":"https:\/\/www.geoparcoalpicarniche.org\/it\/il-territorio\/carsismo\/campi-solcati\/","title":{"rendered":"Campi solcati"},"content":{"rendered":"<div id=\"pl-4235\"  class=\"panel-layout\" ><div id=\"pg-4235-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-4235-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-4235-0-0-0\" class=\"so-panel widget widget_nav_menu panel-first-child panel-last-child\" data-index=\"0\" ><div class=\"menu-territorio-container\"><ul id=\"menu-territorio\" class=\"menu\"><li id=\"menu-item-4668\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-has-children menu-item-4668\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/it\/il-territorio\/\">Il territorio<\/a>\n<ul class=\"sub-menu\">\n\t<li id=\"menu-item-2032\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-2032\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/it\/il-territorio\/evoluzione-geologica\/\">Evoluzione geologica<\/a><\/li>\n\t<li id=\"menu-item-4525\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-has-children menu-item-4525\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/it\/il-territorio\/geomorfologia\/\">Geomorfologia<\/a>\n\t<ul class=\"sub-menu\">\n\t\t<li id=\"menu-item-12197\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-12197\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/it\/il-territorio\/carsismo\/morfologie-fluviali\/\">Morfologie fluviali<\/a><\/li>\n\t\t<li id=\"menu-item-12196\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-12196\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/it\/il-territorio\/carsismo\/morfologie-glaciali-e-periglaciali\/\">Morfologie glaciali e periglaciali<\/a><\/li>\n\t\t<li id=\"menu-item-12195\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-12195\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/it\/il-territorio\/carsismo\/evoluzione-dei-versanti\/\">Evoluzione dei versanti<\/a><\/li>\n\t\t<li id=\"menu-item-4671\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-4671\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/it\/il-territorio\/carsismo\/forre\/\">Forre<\/a><\/li>\n\t<\/ul>\n<\/li>\n\t<li id=\"menu-item-3060\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-has-children menu-item-3060\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/it\/il-territorio\/paleontologia\/\">Paleontologia<\/a>\n\t<ul class=\"sub-menu\">\n\t\t<li id=\"menu-item-4667\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-4667\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/it\/il-territorio\/paleontologia\/fossili\/\">Fossili<\/a><\/li>\n\t<\/ul>\n<\/li>\n\t<li id=\"menu-item-3059\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-3059\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/it\/il-territorio\/geositi\/\">Geositi<\/a><\/li>\n\t<li id=\"menu-item-5995\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-5995\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/it\/il-territorio\/geotopi\/\">Geotopi<\/a><\/li>\n\t<li id=\"menu-item-3061\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-has-children menu-item-3061\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/it\/il-territorio\/carsismo\/\">Carsismo<\/a>\n\t<ul class=\"sub-menu\">\n\t\t<li id=\"menu-item-4669\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-4669\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/it\/il-territorio\/carsismo\/grotte\/\">Grotte<\/a><\/li>\n\t\t<li id=\"menu-item-4670\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-4670\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/it\/il-territorio\/carsismo\/campi-solcati\/\">Campi solcati<\/a><\/li>\n\t<\/ul>\n<\/li>\n\t<li id=\"menu-item-4526\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-4526\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/it\/il-territorio\/siti-minerari\/\">Cave e Miniere<\/a><\/li>\n\t<li id=\"menu-item-7216\" class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-7216\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/it\/il-territorio\/pubblicazioni-scaricabili\/\">Pubblicazioni scaricabili<\/a><\/li>\n<\/ul>\n<\/li>\n<\/ul><\/div><\/div><\/div><div id=\"pgc-4235-0-1\"  class=\"panel-grid-cell\" ><div class=\"paddingContentWithSidebar panel-cell-style panel-cell-style-for-4235-0-1\" ><div id=\"panel-4235-0-1-0\" class=\"so-panel widget widget_text panel-first-child\" data-index=\"1\" >\t\t\t<div class=\"textwidget\"><h2>Le forme Carsiche superficiali: campi solcati e doline<\/h2>\n<\/div>\n\t\t<\/div><div id=\"panel-4235-0-1-1\" class=\"so-panel widget widget_siteorigin-panels-builder\" data-index=\"2\" ><div id=\"pl-w5a9d64e3a4797\"  class=\"panel-layout\" ><div id=\"pg-w5a9d64e3a4797-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-w5a9d64e3a4797-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-w5a9d64e3a4797-0-0-0\" class=\"so-panel widget widget_text panel-first-child panel-last-child\" data-index=\"0\" >\t\t\t<div class=\"textwidget\"><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\t\t<\/div><\/div><div id=\"pgc-w5a9d64e3a4797-0-1\"  class=\"panel-grid-cell\" ><div id=\"panel-w5a9d64e3a4797-0-1-0\" class=\"so-panel widget widget_text panel-first-child panel-last-child\" data-index=\"1\" >\t\t\t<div class=\"textwidget\"><div id='gallery-1' class='gallery galleryid-0 gallery-columns-1 gallery-size-large'><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=\"1024\" height=\"576\" src=\"https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/21.Rocce-carsif_Karren_CaseraBordaglia-1280-1-1024x576.jpg\" class=\"attachment-large size-large\" alt=\"\" srcset=\"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-1280-1-300x169.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-1280-1-428x242.jpg 428w, https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/21.Rocce-carsif_Karren_CaseraBordaglia-1280-1.jpg 1280w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/a>\n\t\t\t<\/div><\/figure>\n\t\t<\/div>\n\n<\/div>\n\t\t<\/div><\/div><\/div><\/div><\/div><div id=\"panel-4235-0-1-2\" class=\"so-panel widget widget_siteorigin-panels-builder\" data-index=\"3\" ><div class=\"mb panel-widget-style panel-widget-style-for-4235-0-1-2\" ><div id=\"pl-w5a9d64e3a4828\"  class=\"panel-layout\" ><div id=\"pg-w5a9d64e3a4828-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-w5a9d64e3a4828-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-w5a9d64e3a4828-0-0-0\" class=\"so-panel widget widget_text panel-first-child panel-last-child\" data-index=\"0\" >\t\t\t<div class=\"textwidget\"><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-0 gallery-columns-1 gallery-size-large'><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=\"1024\" height=\"468\" src=\"https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/20.Carsismo-sup_cop_Pizzul-Zermula-da-torbiera-Valdolce-1280-1024x468.jpg\" class=\"attachment-large size-large\" alt=\"\" srcset=\"https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/20.Carsismo-sup_cop_Pizzul-Zermula-da-torbiera-Valdolce-1280-1024x468.jpg 1024w, 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.jpg 1280w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/a>\n\t\t\t<\/div><\/figure>\n\t\t<\/div>\n\n<\/div>\n<\/div>\n\t\t<\/div><\/div><\/div><\/div><\/div><\/div><div id=\"panel-4235-0-1-3\" class=\"so-panel widget widget_text\" data-index=\"4\" >\t\t\t<div class=\"textwidget\"><h2>Per farsi un&#8217;idea<\/h2>\n<p><strong>Qualche esempio di forme carsiche superficiali nell\u2019area del Geoparco<\/strong><\/p>\n<\/div>\n\t\t<\/div><div id=\"panel-4235-0-1-4\" class=\"so-panel widget widget_siteorigin-panels-builder\" data-index=\"5\" ><div class=\"mb panel-widget-style panel-widget-style-for-4235-0-1-4\" ><div id=\"pl-w5a7049e6b49e6\"  class=\"panel-layout\" ><div id=\"pg-w5a7049e6b49e6-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-w5a7049e6b49e6-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-w5a7049e6b49e6-0-0-0\" class=\"so-panel widget widget_text panel-first-child panel-last-child\" data-index=\"0\" >\t\t\t<div class=\"textwidget\"><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\t\t<\/div><\/div><div id=\"pgc-w5a7049e6b49e6-0-1\"  class=\"panel-grid-cell\" ><div id=\"panel-w5a7049e6b49e6-0-1-0\" class=\"so-panel widget widget_text panel-first-child panel-last-child\" data-index=\"1\" >\t\t\t<div class=\"textwidget\"><\/div>\n\t\t<\/div><\/div><\/div><\/div><\/div><\/div><div id=\"panel-4235-0-1-5\" class=\"so-panel widget widget_siteorigin-panels-builder\" data-index=\"6\" ><div class=\"mb panel-widget-style panel-widget-style-for-4235-0-1-5\" ><div id=\"pl-w5a9d64e3a48a3\"  class=\"panel-layout\" ><div id=\"pg-w5a9d64e3a48a3-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-w5a9d64e3a48a3-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-w5a9d64e3a48a3-0-0-0\" class=\"so-panel widget widget_text panel-first-child panel-last-child\" data-index=\"0\" >\t\t\t<div class=\"textwidget\"><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\t\t<\/div><\/div><div id=\"pgc-w5a9d64e3a48a3-0-1\"  class=\"panel-grid-cell\" ><div id=\"panel-w5a9d64e3a48a3-0-1-0\" class=\"so-panel widget widget_text panel-first-child panel-last-child\" data-index=\"1\" >\t\t\t<div class=\"textwidget\"><div id='gallery-3' class='gallery galleryid-0 gallery-columns-1 gallery-size-large'><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=\"1024\" height=\"688\" src=\"https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/22.Doline-Val-Dolce-Paularo-1280-1-1024x688.jpg\" class=\"attachment-large size-large\" alt=\"\" srcset=\"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-1280-1-300x202.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-1280-1-272x182.jpg 272w, https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/22.Doline-Val-Dolce-Paularo-1280-1.jpg 1280w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/a>\n\t\t\t<\/div><\/figure>\n\t\t<\/div>\n\n<\/div>\n\t\t<\/div><\/div><\/div><\/div><\/div><\/div><div id=\"panel-4235-0-1-6\" class=\"so-panel widget widget_siteorigin-panels-builder\" data-index=\"7\" ><div class=\"mb panel-widget-style panel-widget-style-for-4235-0-1-6\" ><div id=\"pl-w5a7048083e50b\"  class=\"panel-layout\" ><div id=\"pg-w5a7048083e50b-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-w5a7048083e50b-0-0\"  class=\"panel-grid-cell panel-grid-cell-mobile-last\" ><div id=\"panel-w5a7048083e50b-0-0-0\" class=\"so-panel widget widget_text panel-first-child panel-last-child\" data-index=\"0\" >\t\t\t<div class=\"textwidget\"><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\t\t<\/div><\/div><div id=\"pgc-w5a7048083e50b-0-1\"  class=\"panel-grid-cell panel-grid-cell-empty\" ><\/div><\/div><\/div><\/div><\/div><div id=\"panel-4235-0-1-7\" class=\"so-panel widget widget_siteorigin-panels-builder\" data-index=\"8\" ><div class=\"mb panel-widget-style panel-widget-style-for-4235-0-1-7\" ><div id=\"pl-w5a9d64e3a4919\"  class=\"panel-layout\" ><div id=\"pg-w5a9d64e3a4919-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-w5a9d64e3a4919-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-w5a9d64e3a4919-0-0-0\" class=\"so-panel widget widget_text panel-first-child panel-last-child\" data-index=\"0\" >\t\t\t<div class=\"textwidget\"><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\t\t<\/div><\/div><div id=\"pgc-w5a9d64e3a4919-0-1\"  class=\"panel-grid-cell\" ><div id=\"panel-w5a9d64e3a4919-0-1-0\" class=\"so-panel widget widget_text panel-first-child panel-last-child\" data-index=\"1\" >\t\t\t<div class=\"textwidget\"><div id='gallery-4' class='gallery galleryid-0 gallery-columns-1 gallery-size-large'><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=\"1024\" height=\"688\" src=\"https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/23.Campi-solcati-Casera-Monumenz-1280-1024x688.jpg\" class=\"attachment-large size-large\" alt=\"\" srcset=\"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-1280-300x202.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-1280-272x182.jpg 272w, https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2018\/01\/23.Campi-solcati-Casera-Monumenz-1280.jpg 1280w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/a>\n\t\t\t<\/div><\/figure>\n\t\t<\/div>\n\n<\/div>\n\t\t<\/div><\/div><\/div><\/div><\/div><\/div><div id=\"panel-4235-0-1-8\" class=\"so-panel widget widget_siteorigin-panels-builder panel-last-child\" data-index=\"9\" ><div class=\"mb panel-widget-style panel-widget-style-for-4235-0-1-8\" ><div id=\"pl-w5a7048ea66a04\"  class=\"panel-layout\" ><div id=\"pg-w5a7048ea66a04-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-w5a7048ea66a04-0-0\"  class=\"panel-grid-cell panel-grid-cell-mobile-last\" ><div id=\"panel-w5a7048ea66a04-0-0-0\" class=\"so-panel widget widget_text panel-first-child panel-last-child\" data-index=\"0\" >\t\t\t<div class=\"textwidget\"><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\t\t<\/div><\/div><div id=\"pgc-w5a7048ea66a04-0-1\"  class=\"panel-grid-cell panel-grid-cell-empty\" ><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div>","protected":false},"excerpt":{"rendered":"<p>Le forme Carsiche superficiali: campi solcati e doline Per farsi un&#8217;idea Qualche esempio di forme carsiche superficiali nell\u2019area del Geoparco<\/p>\n","protected":false},"author":2,"featured_media":3039,"parent":3049,"menu_order":89,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_acf_changed":false,"inline_featured_image":false,"ngg_post_thumbnail":0,"footnotes":""},"class_list":{"0":"post-4235","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 v27.3 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>Campi solcati - 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\/it\/il-territorio\/carsismo\/campi-solcati\/\" \/>\n<meta property=\"og:locale\" content=\"it_IT\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Campi solcati - Geoparco 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