{"id":7,"date":"2017-11-21T17:09:40","date_gmt":"2017-11-21T16:09:40","guid":{"rendered":"http:\/\/www.didalms.it\/wordpress\/?page_id=7"},"modified":"2023-12-12T20:27:26","modified_gmt":"2023-12-12T19:27:26","slug":"homepage","status":"publish","type":"page","link":"https:\/\/www.didalms.it\/wordpress\/","title":{"rendered":"Home"},"content":{"rendered":"<div data-elementor-type=\"post\" data-elementor-id=\"7\" class=\"elementor elementor-7\" data-elementor-settings=\"[]\">\n\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<section class=\"elementor-element elementor-element-fac7e3c elementor-section-boxed elementor-section-height-default elementor-section-height-default elementor-section elementor-top-section\" data-id=\"fac7e3c\" data-element_type=\"section\"><div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t<div class=\"elementor-row\">\n\t\t\t\t<div class=\"elementor-element elementor-element-9c3bde6 elementor-column elementor-col-100 elementor-top-column\" data-id=\"9c3bde6\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-column-wrap  elementor-element-populated\">\n\t\t\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t<div class=\"elementor-element elementor-element-987a2e6 elementor-widget elementor-widget-image-carousel\" data-id=\"987a2e6\" data-element_type=\"widget\" data-settings='{\"slides_to_scroll\":\"3\",\"slides_to_show\":\"5\",\"navigation\":\"both\",\"pause_on_hover\":\"yes\",\"autoplay\":\"yes\",\"autoplay_speed\":5000,\"infinite\":\"yes\",\"speed\":500,\"direction\":\"ltr\"}' data-widget_type=\"image-carousel.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-image-carousel-wrapper elementor-slick-slider\" dir=\"ltr\">\n\t\t\t<div class=\"elementor-image-carousel slick-arrows-inside slick-dots-outside\">\n\t\t\t\t<div class=\"slick-slide\"><figure class=\"slick-slide-inner\"><img decoding=\"async\" class=\"slick-slide-image\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/02\/forra-fosso-marchetto-672x372-150x150.jpg\" alt=\"forra-fosso-marchetto\"\/><figcaption class=\"elementor-image-carousel-caption\">forra-fosso-marchetto<\/figcaption><\/figure><\/div><div class=\"slick-slide\"><figure class=\"slick-slide-inner\"><img decoding=\"async\" class=\"slick-slide-image\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/coscerno_10-150x150.jpg\" alt=\"Monte Coscerno\"\/><figcaption class=\"elementor-image-carousel-caption\">Monte Coscerno<\/figcaption><\/figure><\/div><div class=\"slick-slide\"><figure class=\"slick-slide-inner\"><img decoding=\"async\" class=\"slick-slide-image\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/valdorbia_by-150x150.jpg\" alt=\"Valdorbia\"\/><figcaption class=\"elementor-image-carousel-caption\">Valdorbia<\/figcaption><\/figure><\/div><div class=\"slick-slide\"><figure class=\"slick-slide-inner\"><img decoding=\"async\" class=\"slick-slide-image\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/Cascata_delle_Marmore_2-150x150.jpg\" alt=\"Cascata delle Marmore\"\/><figcaption class=\"elementor-image-carousel-caption\">Cascata delle Marmore<\/figcaption><\/figure><\/div><div class=\"slick-slide\"><figure class=\"slick-slide-inner\"><img decoding=\"async\" class=\"slick-slide-image\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/mortaro-678x381-150x150.jpg\" alt=\"Mortaro Grande\"\/><figcaption class=\"elementor-image-carousel-caption\">Mortaro Grande<\/figcaption><\/figure><\/div><div class=\"slick-slide\"><figure class=\"slick-slide-inner\"><img decoding=\"async\" class=\"slick-slide-image\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/Castelluccio_piana_grande-150x150.jpg\" alt=\"Castelluccio-piana grande\"\/><figcaption class=\"elementor-image-carousel-caption\">Castelluccio-piana grande<\/figcaption><\/figure><\/div><div class=\"slick-slide\"><figure class=\"slick-slide-inner\"><img decoding=\"async\" class=\"slick-slide-image\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/Martanites_prorsiradiatus_top_ridotta-150x150.jpg\" alt=\"Martanites-prorsiradiatus\"\/><figcaption class=\"elementor-image-carousel-caption\">Martanites-prorsiradiatus<\/figcaption><\/figure><\/div><div class=\"slick-slide\"><figure class=\"slick-slide-inner\"><img decoding=\"async\" class=\"slick-slide-image\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/grotta_monte_cucco_Ridotta-150x150.jpg\" alt=\"Grotta Monte Cucco\"\/><figcaption class=\"elementor-image-carousel-caption\">Grotta Monte Cucco<\/figcaption><\/figure><\/div><div class=\"slick-slide\"><figure class=\"slick-slide-inner\"><img decoding=\"async\" class=\"slick-slide-image\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/Bottaccione_Alvarez_iridio-1-150x150.png\" alt=\"gola del Bottaccione\"\/><figcaption class=\"elementor-image-carousel-caption\">gola del Bottaccione<\/figcaption><\/figure><\/div><div class=\"slick-slide\"><figure class=\"slick-slide-inner\"><img decoding=\"async\" class=\"slick-slide-image\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/Foresta_fossile_Dunarobba-150x150.png\" alt=\"Foresta fossile Dunarobba\"\/><figcaption class=\"elementor-image-carousel-caption\">Foresta fossile Dunarobba<\/figcaption><\/figure><\/div><div class=\"slick-slide\"><figure class=\"slick-slide-inner\"><img decoding=\"async\" class=\"slick-slide-image\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/Grotta_Pozzi_Piana-150x150.jpg\" alt=\"OLYMPUS DIGITAL CAMERA\"\/><figcaption class=\"elementor-image-carousel-caption\">Grotte della Piana<\/figcaption><\/figure><\/div><div class=\"slick-slide\"><figure class=\"slick-slide-inner\"><img decoding=\"async\" class=\"slick-slide-image\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/02\/campello_sul_clitunno_-_fonti_web-150x150.jpg\" alt=\"fonti del Clitunno\"\/><figcaption class=\"elementor-image-carousel-caption\">fonti del Clitunno<\/figcaption><\/figure><\/div>\t\t\t<\/div>\n\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<\/div>\n\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t<\/section><section class=\"elementor-element elementor-element-42f7054 elementor-section-boxed elementor-section-height-default elementor-section-height-default elementor-section elementor-top-section\" data-id=\"42f7054\" data-element_type=\"section\"><div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t<div class=\"elementor-row\">\n\t\t\t\t<div class=\"elementor-element elementor-element-343232c elementor-column elementor-col-100 elementor-top-column\" data-id=\"343232c\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-column-wrap  elementor-element-populated\">\n\t\t\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t<div class=\"elementor-element elementor-element-98c131c elementor-widget elementor-widget-text-editor\" data-id=\"98c131c\" 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<div class=\"elementor-text-editor elementor-clearfix\"><p style=\"text-align: center;\">Evoluzione geologica dell&rsquo;Umbria<\/p><\/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<\/div>\n\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t<\/section><section class=\"elementor-element elementor-element-8f0d12a elementor-section-boxed elementor-section-height-default elementor-section-height-default elementor-section elementor-top-section\" data-id=\"8f0d12a\" data-element_type=\"section\"><div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t<div class=\"elementor-row\">\n\t\t\t\t<div class=\"elementor-element elementor-element-493858a elementor-column elementor-col-25 elementor-top-column\" data-id=\"493858a\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-column-wrap  elementor-element-populated\">\n\t\t\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t<div class=\"elementor-element elementor-element-383f021 elementor-widget elementor-widget-text-editor\" data-id=\"383f021\" 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<div class=\"elementor-text-editor elementor-clearfix\"><p style=\"text-align: left;\"><span style=\"color: #003300;\">L&rsquo;<strong>Umbria<\/strong>&nbsp;e&#768; caratterizzata da una grande&nbsp;<em>variabilita&#768; geologica<\/em>&nbsp;che si traduce in una complessita&#768; morfologica all&rsquo;interno di una superficie relativamente modesta come quella della regione (8600 Kmq circa); procedendo da NE verso SW, sono &nbsp;individuabili, a grande scala specifiche &ldquo;<em>unita&#768; di paesaggio<\/em>&rdquo;: quella delle&nbsp;<strong>strutture calcaree<\/strong>&nbsp;dell&rsquo;Appennino; quella delle&nbsp;<strong>formazioni arenacee<\/strong>&nbsp;s.l. del preappennino e dell&rsquo;area centrale; le&nbsp;<strong>aree depresse<\/strong>&nbsp;e\/o&nbsp;<strong>ribassate<\/strong>&nbsp;che sono numerose nel territorio umbro&nbsp;&nbsp;e infine l&rsquo;unita&#768; di paesaggio caratterizzata da&nbsp;<strong>rocce ignee<\/strong>, legate all&rsquo;attivita&#768; dell&rsquo;apparato vulcanico di Bolsena. In realta&#768;, il modellato superficiale e&#768; strettamente legato all&rsquo;affioramento di rocce diverse, ma anche alle vicende&nbsp;<strong>tettoniche<\/strong>&nbsp;che hanno interessato l&rsquo;area e dato la prima &ldquo;impronta&rdquo; topografica ed idrografica sui cui poi sono intervenuti, modificandola, gli agenti e i processi morfogenetici&hellip;.<\/span><\/p><p>tratto da:&nbsp;<a href=\"http:\/\/www.geologiaeturismo.it\/node\/189\"><em>L&rsquo;Umbria: Regione di contrasti Litologici e morfologici &ndash;&nbsp;Lucilia Gregori<\/em><\/a><\/p><\/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<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-1794bad elementor-column elementor-col-25 elementor-top-column\" data-id=\"1794bad\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-column-wrap  elementor-element-populated\">\n\t\t\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t<div class=\"elementor-element elementor-element-6e1aac3 elementor-position-top elementor-vertical-align-top elementor-widget elementor-widget-image-box\" data-id=\"6e1aac3\" data-element_type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><img loading=\"lazy\" decoding=\"async\" width=\"500\" height=\"650\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/10mil_a.jpg\" class=\"attachment-full size-full\" alt=\"\" srcset=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/10mil_a-231x300.jpg 231w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/10mil_a.jpg 500w\" sizes=\"(max-width: 500px) 100vw, 500px\"\/><\/figure><div class=\"elementor-image-box-content\"><h4 class=\"elementor-image-box-title\">Umbria nel Pliocene<\/h4><p class=\"elementor-image-box-description\">All&rsquo;inizio del Pliocene (10-2 Ma) il territorio umbro era bagnato dal mar Tirreno fino agli attuali territori di Terni, Orvieto e Lago Trasimeno. <\/p><\/div><\/div>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-15b47d2 elementor-column elementor-col-25 elementor-top-column\" data-id=\"15b47d2\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-column-wrap  elementor-element-populated\">\n\t\t\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t<div class=\"elementor-element elementor-element-480313f elementor-position-top elementor-vertical-align-top elementor-widget elementor-widget-image-box\" data-id=\"480313f\" data-element_type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><img loading=\"lazy\" decoding=\"async\" width=\"500\" height=\"650\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/1mil_a.jpg\" class=\"attachment-full size-full\" alt=\"\" srcset=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/1mil_a-231x300.jpg 231w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/1mil_a.jpg 500w\" sizes=\"(max-width: 500px) 100vw, 500px\"\/><\/figure><div class=\"elementor-image-box-content\"><h4 class=\"elementor-image-box-title\">Umbria nel Quaternario antico<\/h4><p class=\"elementor-image-box-description\">Durante il quaternario antico 1 milione di anni fa l&rsquo;Umbria era ancora per una gran parte sommersa dalle acque del Lago Tiberino<\/p><\/div><\/div>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-26225109 elementor-column elementor-col-25 elementor-top-column\" data-id=\"26225109\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-column-wrap  elementor-element-populated\">\n\t\t\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t<div class=\"elementor-element elementor-element-9a469c9 elementor-position-top elementor-vertical-align-top elementor-widget elementor-widget-image-box\" data-id=\"9a469c9\" data-element_type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><img loading=\"lazy\" decoding=\"async\" width=\"500\" height=\"650\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/60mila_a.jpg\" class=\"attachment-full size-full\" alt=\"\" srcset=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/60mila_a-231x300.jpg 231w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/60mila_a.jpg 500w\" sizes=\"(max-width: 500px) 100vw, 500px\"\/><\/figure><div class=\"elementor-image-box-content\"><h4 class=\"elementor-image-box-title\">Umbria nel Quaternario medio<\/h4><p class=\"elementor-image-box-description\">Il Lago Tiberino &egrave; andato riducendosi fino a scomparire nel quaternario medio (60 mila anni fa circa), l&rsquo;Umbria assume una forma molto simile a quella attuale.<\/p><\/div><\/div>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-dcfce29 elementor-widget elementor-widget-spacer\" data-id=\"dcfce29\" data-element_type=\"widget\" data-widget_type=\"spacer.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-spacer\">\n\t\t\t<div class=\"elementor-spacer-inner\"><\/div>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-f355d7a elementor-widget elementor-widget-spacer\" data-id=\"f355d7a\" data-element_type=\"widget\" data-widget_type=\"spacer.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-spacer\">\n\t\t\t<div class=\"elementor-spacer-inner\"><\/div>\n\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<\/div>\n\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t<\/section><section class=\"elementor-element elementor-element-7ced137 elementor-section-boxed elementor-section-height-default elementor-section-height-default elementor-section elementor-top-section\" data-id=\"7ced137\" data-element_type=\"section\"><div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t<div class=\"elementor-row\">\n\t\t\t\t<div class=\"elementor-element elementor-element-f10670e elementor-column elementor-col-100 elementor-top-column\" data-id=\"f10670e\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-column-wrap  elementor-element-populated\">\n\t\t\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t<div class=\"elementor-element elementor-element-b2d1d81 elementor-widget elementor-widget-text-editor\" data-id=\"b2d1d81\" 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<div class=\"elementor-text-editor elementor-clearfix\"><p style=\"text-align: center;\">Evoluzione geologica del continente europeo<\/p><\/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<\/div>\n\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t<\/section><section class=\"elementor-element elementor-element-28f19c0 elementor-section-boxed elementor-section-height-default elementor-section-height-default elementor-section elementor-top-section\" data-id=\"28f19c0\" data-element_type=\"section\"><div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t<div class=\"elementor-row\">\n\t\t\t\t<div class=\"elementor-element elementor-element-889f1e3 elementor-column elementor-col-33 elementor-top-column\" data-id=\"889f1e3\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-column-wrap  elementor-element-populated\">\n\t\t\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t<div class=\"elementor-element elementor-element-786a9d8 elementor-position-top elementor-vertical-align-top elementor-widget elementor-widget-image-box\" data-id=\"786a9d8\" data-element_type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"http:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2023\/12\/Geologia-Italia-Zanich-Itinerari_Introduzione.pdf\" target=\"_blank\"><img loading=\"lazy\" decoding=\"async\" width=\"600\" height=\"515\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/Geol.Italie-e1516783817451.jpg\" class=\"attachment-full size-full\" alt=\"\"\/><\/a><\/figure><div class=\"elementor-image-box-content\"><h4 class=\"elementor-image-box-title\"><a href=\"http:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2023\/12\/Geologia-Italia-Zanich-Itinerari_Introduzione.pdf\" target=\"_blank\">Storia geologica dell'Italia<\/a><\/h4><p class=\"elementor-image-box-description\">dal testo:\nGainotti Modelli DENTRO LE SCIENZE INTEGRATE &copy; Zanichelli editore S.p.A. 2011\n<\/p><\/div><\/div>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-d4412ac elementor-column elementor-col-33 elementor-top-column\" data-id=\"d4412ac\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-column-wrap  elementor-element-populated\">\n\t\t\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t<div class=\"elementor-element elementor-element-c3bd7b4 elementor-position-top elementor-vertical-align-top elementor-widget elementor-widget-image-box\" data-id=\"c3bd7b4\" data-element_type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"http:\/\/www.didalms.it\/wordpress\/2018\/01\/24\/storia-geologica-dellitalia\/\" target=\"_blank\"><img loading=\"lazy\" decoding=\"async\" width=\"1159\" height=\"789\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/Dettaglio_Carta_%E2%80%93_e-Geo_umbria.png\" class=\"attachment-full size-full\" alt=\"\" srcset=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/Dettaglio_Carta_&ndash;_e-Geo_umbria-300x204.png 300w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/Dettaglio_Carta_&ndash;_e-Geo_umbria-768x523.png 768w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/Dettaglio_Carta_&ndash;_e-Geo_umbria-1024x697.png 1024w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/Dettaglio_Carta_&ndash;_e-Geo_umbria.png 1159w\" sizes=\"(max-width: 1159px) 100vw, 1159px\"\/><\/a><\/figure><div class=\"elementor-image-box-content\"><h4 class=\"elementor-image-box-title\"><a href=\"http:\/\/www.didalms.it\/wordpress\/2018\/01\/24\/storia-geologica-dellitalia\/\" target=\"_blank\">Storia geologica dell'Umbria<\/a><\/h4><p class=\"elementor-image-box-description\">Fino a 200 milioni di anni fa la penisola italiana non era ancora emersa, ma sotto le acque calde del mare poco profondo chiamato Tetide, erano gi&agrave; iniziati quei processi che dal compattarsi dei sedimenti accumulati sul fondale, avevano portato alla formazione di uno strato di roccia bianca chiamata <a href=\"https:\/\/www.didalms.it\/wordpress\/Glossary\/calcare\/\" data-cmtooltip=\"Il &lt;b&gt;calcare&lt;\/b&gt; &egrave; una &lt;a title=&quot;Roccia sedimentaria&quot; href=&quot;https:\/\/it.wikipedia.org\/wiki\/Roccia_sedimentaria&quot;&gt;roccia sedimentaria&lt;\/a&gt; il cui componente principale &egrave; rappresentato dal &lt;a title=&quot;Minerale&quot; href=&quot;https:\/\/it.wikipedia.org\/wiki\/Minerale&quot;&gt;minerale&lt;\/a&gt; &lt;a title=&quot;Calcite&quot; href=&quot;https:\/\/it.wikipedia.org\/wiki\/Calcite&quot;&gt;calcite&lt;\/a&gt;. I &lt;a title=&quot;Giacimento&quot; href=&quot;https:\/\/it.wikipedia.org\/wiki\/Giacimento&quot;&gt;giacimenti&lt;\/a&gt; di calcare, quindi il minerale stesso, sono pi&ugrave; o meno compenetrati da impurit&agrave; &lt;a title=&quot;Argilla&quot; href=&quot;https:\/\/it.wikipedia.org\/wiki\/Argilla&quot;&gt;argillose&lt;\/a&gt; o &lt;a title=&quot;Quarzo&quot; href=&quot;https:\/\/it.wikipedia.org\/wiki\/Quarzo&quot;&gt;quarzitiche&lt;\/a&gt;. La calcite &egrave; un minerale spesso accoppiato alla &lt;a title=&quot;Dolomite&quot; href=&quot;https:\/\/it.wikipedia.org\/wiki\/Dolomite&quot;&gt;dolomite&lt;\/a&gt;.&lt;br \/&gt;&lt;img src=&quot;http:\/\/www.ilponticello.net\/wp-content\/uploads\/2015\/06\/Immagine2.png&quot; \/&gt;\"  class=\"glossaryLink \">calcare<\/a> massiccio....\n<\/p><\/div><\/div>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-e32c840 elementor-column elementor-col-33 elementor-top-column\" data-id=\"e32c840\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-column-wrap  elementor-element-populated\">\n\t\t\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t<div class=\"elementor-element elementor-element-a0f4700 elementor-position-top elementor-vertical-align-top elementor-widget elementor-widget-image-box\" data-id=\"a0f4700\" data-element_type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"http:\/\/www.siripro.it\/dipgeopa.asp?structure=education&amp;where=regionale&amp;cap=01&amp;lang=it\"><img loading=\"lazy\" decoding=\"async\" width=\"512\" height=\"440\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/512px-1875_Dumonts_geological_map_of_Europe.jpg\" class=\"attachment-full size-full\" alt=\"\" srcset=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/512px-1875_Dumonts_geological_map_of_Europe-200x172.jpg 200w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/512px-1875_Dumonts_geological_map_of_Europe-300x258.jpg 300w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/512px-1875_Dumonts_geological_map_of_Europe-400x344.jpg 400w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/512px-1875_Dumonts_geological_map_of_Europe.jpg 512w\" sizes=\"(max-width: 512px) 100vw, 512px\"\/><\/a><\/figure><div class=\"elementor-image-box-content\"><h4 class=\"elementor-image-box-title\"><a href=\"http:\/\/www.siripro.it\/dipgeopa.asp?structure=education&amp;where=regionale&amp;cap=01&amp;lang=it\">Storia geologica dell'Europa<\/a><\/h4><p class=\"elementor-image-box-description\">L&rsquo;Europa pu&ograve; essere interpretato come la pi&ugrave; piccola parte occidentale del continente Euro-Asiatico che &egrave; di gran lunga pi&ugrave; grande. La catena montuosa degli Urali forma il limite tra Europa e Asia verso Est; verso Sud-Est e Sud questo limite passa attraverso la parte settentrionale dell&rsquo;area del Mar Caspio e del sistema delle montagne del Caucaso.<\/p><\/div><\/div>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t<\/section><section class=\"elementor-element elementor-element-44564dd elementor-section-boxed elementor-section-height-default elementor-section-height-default elementor-section elementor-top-section\" data-id=\"44564dd\" data-element_type=\"section\"><div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t<div class=\"elementor-row\">\n\t\t\t\t<div class=\"elementor-element elementor-element-ec7c6d7 elementor-column elementor-col-100 elementor-top-column\" data-id=\"ec7c6d7\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-column-wrap  elementor-element-populated\">\n\t\t\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t<div class=\"elementor-element elementor-element-8746269 elementor-widget elementor-widget-text-editor\" data-id=\"8746269\" 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<div class=\"elementor-text-editor elementor-clearfix\"><p style=\"text-align: center;\">Le rocce dell&rsquo;Appennino Umbro Marchigiano<\/p><\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-14fd259a elementor-widget elementor-widget-image-carousel\" data-id=\"14fd259a\" data-element_type=\"widget\" data-settings='{\"slides_to_show\":\"3\",\"slides_to_scroll\":\"1\",\"navigation\":\"both\",\"pause_on_hover\":\"yes\",\"autoplay\":\"yes\",\"autoplay_speed\":5000,\"infinite\":\"yes\",\"speed\":500,\"direction\":\"ltr\"}' data-widget_type=\"image-carousel.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-image-carousel-wrapper elementor-slick-slider\" dir=\"ltr\">\n\t\t\t<div class=\"elementor-image-carousel slick-arrows-outside slick-dots-outside\">\n\t\t\t\t<div class=\"slick-slide\"><figure class=\"slick-slide-inner\"><img decoding=\"async\" class=\"slick-slide-image\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/calc-massiccio-300x214.jpg\" alt=\"calcare massiccio (sasso rosso)\"\/><figcaption class=\"elementor-image-carousel-caption\"><a href=\"https:\/\/www.didalms.it\/wordpress\/Glossary\/calcare\/\" data-cmtooltip=\"Il &lt;b&gt;calcare&lt;\/b&gt; &egrave; una &lt;a title=&quot;Roccia sedimentaria&quot; href=&quot;https:\/\/it.wikipedia.org\/wiki\/Roccia_sedimentaria&quot;&gt;roccia sedimentaria&lt;\/a&gt; il cui componente principale &egrave; rappresentato dal &lt;a title=&quot;Minerale&quot; href=&quot;https:\/\/it.wikipedia.org\/wiki\/Minerale&quot;&gt;minerale&lt;\/a&gt; &lt;a title=&quot;Calcite&quot; href=&quot;https:\/\/it.wikipedia.org\/wiki\/Calcite&quot;&gt;calcite&lt;\/a&gt;. I &lt;a title=&quot;Giacimento&quot; href=&quot;https:\/\/it.wikipedia.org\/wiki\/Giacimento&quot;&gt;giacimenti&lt;\/a&gt; di calcare, quindi il minerale stesso, sono pi&ugrave; o meno compenetrati da impurit&agrave; &lt;a title=&quot;Argilla&quot; href=&quot;https:\/\/it.wikipedia.org\/wiki\/Argilla&quot;&gt;argillose&lt;\/a&gt; o &lt;a title=&quot;Quarzo&quot; href=&quot;https:\/\/it.wikipedia.org\/wiki\/Quarzo&quot;&gt;quarzitiche&lt;\/a&gt;. La calcite &egrave; un minerale spesso accoppiato alla &lt;a title=&quot;Dolomite&quot; href=&quot;https:\/\/it.wikipedia.org\/wiki\/Dolomite&quot;&gt;dolomite&lt;\/a&gt;.&lt;br \/&gt;&lt;img src=&quot;http:\/\/www.ilponticello.net\/wp-content\/uploads\/2015\/06\/Immagine2.png&quot; \/&gt;\"  class=\"glossaryLink \">calcare<\/a> massiccio (sasso rosso)<\/figcaption><\/figure><\/div><div class=\"slick-slide\"><figure class=\"slick-slide-inner\"><img decoding=\"async\" class=\"slick-slide-image\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/corniola-300x214.jpg\" alt=\"corniola\"\/><figcaption class=\"elementor-image-carousel-caption\">corniola<\/figcaption><\/figure><\/div><div class=\"slick-slide\"><figure class=\"slick-slide-inner\"><img decoding=\"async\" class=\"slick-slide-image\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/marne-m.te-Serrone-300x214.jpg\" alt=\"marne m.te Serrone\"\/><figcaption class=\"elementor-image-carousel-caption\">marne m.te Serrone<\/figcaption><\/figure><\/div><div class=\"slick-slide\"><figure class=\"slick-slide-inner\"><img decoding=\"async\" class=\"slick-slide-image\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/rosso-ammonitico-300x214.jpg\" alt=\"rosso ammonitico\"\/><figcaption class=\"elementor-image-carousel-caption\"><a href=\"https:\/\/www.didalms.it\/wordpress\/Glossary\/rosso-ammonitico\/\" data-cmtooltip=\"Si d&agrave; il nome di &lt;b&gt;rosso ammonitico&lt;\/b&gt; ad una lito&lt;a title=&quot;Facies&quot; href=&quot;https:\/\/it.wikipedia.org\/wiki\/Facies&quot;&gt;facies&lt;\/a&gt; diffusa in Italia nelle &lt;a title=&quot;Alpi meridionali&quot; href=&quot;https:\/\/it.wikipedia.org\/wiki\/Alpi_meridionali&quot;&gt;Alpi meridionali&lt;\/a&gt;, nell&#039;&lt;a title=&quot;Appennino umbro-marchigiano&quot; href=&quot;https:\/\/it.wikipedia.org\/wiki\/Appennino_umbro-marchigiano&quot;&gt;Appennino umbro-marchigiano&lt;\/a&gt; e nell&#039;&lt;a title=&quot;Appennino meridionale&quot; href=&quot;https:\/\/it.wikipedia.org\/wiki\/Appennino_meridionale&quot;&gt;Appennino meridionale&lt;\/a&gt; fino alla &lt;a title=&quot;Sicilia&quot; href=&quot;https:\/\/it.wikipedia.org\/wiki\/Sicilia&quot;&gt;Sicilia&lt;\/a&gt;, di &lt;a title=&quot;Ambiente sedimentario&quot; href=&quot;https:\/\/it.wikipedia.org\/wiki\/Ambiente_sedimentario&quot;&gt;ambiente&lt;\/a&gt; pelagico. Il termine &lt;i&gt;rosso ammonitico&lt;\/i&gt; &egrave; generalmente preferito dagli autori italiani, mentre il termine &lt;i&gt;ammonitico rosso&lt;\/i&gt; &egrave; caratteristico degli autori svizzeri e in generale di lingua tedesca, ed &egrave; il pi&ugrave; usato nella letteratura geologica internazionale.&lt;br \/&gt;&lt;img src=&quot;http:\/\/www.parcomontesubasio.it\/wp-content\/uploads\/2015\/08\/Rosso-Amm.jpg&quot; \/&gt;Particolare del Rosso Ammonitico al passaggio con i calcari a Posidonia &ndash; Loc. San Benedetto (monte Subasio)&lt;br \/&gt;&nbsp;&lt;br \/&gt;&nbsp;\"  class=\"glossaryLink \">rosso ammonitico<\/a><\/figcaption><\/figure><\/div><div class=\"slick-slide\"><figure class=\"slick-slide-inner\"><img decoding=\"async\" class=\"slick-slide-image\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/calcari-diasprigni-300x214.jpg\" alt=\"calcari diasprigni\"\/><figcaption class=\"elementor-image-carousel-caption\">calcari diasprigni<\/figcaption><\/figure><\/div><div class=\"slick-slide\"><figure class=\"slick-slide-inner\"><img decoding=\"async\" class=\"slick-slide-image\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/maiolica-300x214.jpg\" alt=\"maiolica\"\/><figcaption class=\"elementor-image-carousel-caption\">maiolica<\/figcaption><\/figure><\/div><div class=\"slick-slide\"><figure class=\"slick-slide-inner\"><img decoding=\"async\" class=\"slick-slide-image\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/marne-a-fucoidi-300x214.jpg\" alt=\"marne a fucoidi\"\/><figcaption class=\"elementor-image-carousel-caption\">marne a fucoidi<\/figcaption><\/figure><\/div><div class=\"slick-slide\"><figure class=\"slick-slide-inner\"><img decoding=\"async\" class=\"slick-slide-image\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/scaglia-bianca-300x214.jpg\" alt=\"scaglia bianca\"\/><figcaption class=\"elementor-image-carousel-caption\">scaglia bianca<\/figcaption><\/figure><\/div><div class=\"slick-slide\"><figure class=\"slick-slide-inner\"><img decoding=\"async\" class=\"slick-slide-image\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/Scaglia-Rossa--300x214.jpeg\" alt=\"scaglia rossa\"\/><figcaption class=\"elementor-image-carousel-caption\"><a href=\"https:\/\/www.didalms.it\/wordpress\/Glossary\/scaglia-rossa\/\" data-cmtooltip=\"La scaglia rossa &egrave; una formazione roccia sedimentaria marina, depostasi prevalentemente in ambiente pelagico, a litologia calcarea selcifera a grana fine, pi&ugrave; o meno marnosi, prevalentemente di colore rosso mattone, che pu&ograve; passare al bianco, al giallo e al grigio cenere.&lt;br \/&gt;La sua distribuzione &egrave; ampia: diffusa lungo l&#039;appennino, in particolare nel bacino umbro-marchigiano, affiora anche nelle alpi calcaree meridionali[1] e nell&#039;area euganea[2].&lt;br \/&gt;La colorazione rossa deriva dalla dispersione nella massa calcarea di ossidi di ferro (limoniti ed ematiti); localmente alcune tinte biancastre possono essere dovute a decolorazione secondaria. I calcari della scaglia rossa presentano sempre una fitta stratificazione regolare e sono stati deposti tra i 90 e i 55 milioni di anni fa, nel Cretaceo superiore, e parzialmente nell&#039;Eocene inferiore. Si tratta di strati che possono arrivare a oltre 100 m di spessore, dove all&#039;interno sono frequenti i noduli di selce di colore rosso. La roccia &egrave; relativamente ricca di fossili: ricci di mare, lamellibranchi e resti di squali.[3]. Il suo contenuto in microfossili &egrave; costituito prevalentemente da foraminiferi planctonici quali: Globotruncanae, Heterohelix e Rosita Contusa (prima dell&#039;Estinzione di massa del Cretaceo-Paleocene) , Morzovellae e Planorotaliae (post K-T).\"  class=\"glossaryLink \">scaglia rossa<\/a><\/figcaption><\/figure><\/div><div class=\"slick-slide\"><figure class=\"slick-slide-inner\"><img decoding=\"async\" class=\"slick-slide-image\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/scaglia-variegata-300x214.jpg\" alt=\"scaglia variegata\"\/><figcaption class=\"elementor-image-carousel-caption\">scaglia variegata<\/figcaption><\/figure><\/div><div class=\"slick-slide\"><figure class=\"slick-slide-inner\"><img decoding=\"async\" class=\"slick-slide-image\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/scaglia-cinerea-300x214.jpg\" alt=\"scaglia cinerea\"\/><figcaption class=\"elementor-image-carousel-caption\">scaglia cinerea<\/figcaption><\/figure><\/div><div class=\"slick-slide\"><figure class=\"slick-slide-inner\"><img decoding=\"async\" class=\"slick-slide-image\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/bisciaro-300x214.jpg\" alt=\"bisciaro\"\/><figcaption class=\"elementor-image-carousel-caption\">bisciaro<\/figcaption><\/figure><\/div><div class=\"slick-slide\"><figure class=\"slick-slide-inner\"><img decoding=\"async\" class=\"slick-slide-image\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/marnoso-arenacea-300x214.jpg\" alt=\"marnoso arenacea\"\/><figcaption class=\"elementor-image-carousel-caption\">marnoso arenacea<\/figcaption><\/figure><\/div>\t\t\t<\/div>\n\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<\/div>\n\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t<\/section><section class=\"elementor-element elementor-element-c54f1f5 elementor-section-boxed elementor-section-height-default elementor-section-height-default elementor-section elementor-top-section\" data-id=\"c54f1f5\" data-element_type=\"section\"><div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t<div class=\"elementor-row\">\n\t\t\t\t<div class=\"elementor-element elementor-element-188dbde elementor-column elementor-col-100 elementor-top-column\" data-id=\"188dbde\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-column-wrap  elementor-element-populated\">\n\t\t\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t<div class=\"elementor-element elementor-element-3d92139 elementor-widget elementor-widget-spacer\" data-id=\"3d92139\" data-element_type=\"widget\" data-widget_type=\"spacer.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-spacer\">\n\t\t\t<div class=\"elementor-spacer-inner\"><\/div>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-8c9809e elementor-widget elementor-widget-text-editor\" data-id=\"8c9809e\" 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<div class=\"elementor-text-editor elementor-clearfix\"><p style=\"text-align: center;\">Ambiti geologici<\/p><\/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<\/div>\n\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t<\/section><section class=\"elementor-element elementor-element-57a4e45 elementor-section-boxed elementor-section-height-default elementor-section-height-default elementor-section elementor-top-section\" data-id=\"57a4e45\" data-element_type=\"section\"><div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t<div class=\"elementor-row\">\n\t\t\t\t<div class=\"elementor-element elementor-element-4954341 elementor-column elementor-col-25 elementor-top-column\" data-id=\"4954341\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-column-wrap  elementor-element-populated\">\n\t\t\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t<div class=\"elementor-element elementor-element-11c6ddb elementor-position-top elementor-vertical-align-top elementor-widget elementor-widget-image-box\" data-id=\"11c6ddb\" data-element_type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"http:\/\/www.didalms.it\/wordpress\/2018\/01\/26\/la-successione-stratigrafica-umbro-marchigiana\/\" target=\"_blank\"><img loading=\"lazy\" decoding=\"async\" width=\"200\" height=\"235\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/serieumbromarchigiana1-e1518077065513.png\" class=\"attachment-full size-full\" alt=\"\"\/><\/a><\/figure><div class=\"elementor-image-box-content\"><h5 class=\"elementor-image-box-title\"><a href=\"http:\/\/www.didalms.it\/wordpress\/2018\/01\/26\/la-successione-stratigrafica-umbro-marchigiana\/\" target=\"_blank\">Successione stratigrafica Umbro Marchigiana<\/a><\/h5><p class=\"elementor-image-box-description\">Nel territorio umbro affiorano le formazioni prevalentemente calcaree della &ldquo;Serie Umbro-Marchigiana&rdquo; e ne vengono brevemente richiamati i caratteri salienti<\/p><\/div><\/div>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-53387a7 elementor-widget elementor-widget-divider\" data-id=\"53387a7\" data-element_type=\"widget\" data-widget_type=\"divider.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-divider\">\n\t\t\t<span class=\"elementor-divider-separator\"><\/span>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-a29828b elementor-position-top elementor-vertical-align-top elementor-widget elementor-widget-image-box\" data-id=\"a29828b\" data-element_type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"https:\/\/www.openstarts.units.it\/bitstream\/10077\/12084\/1\/Gregori.pdf\"><img loading=\"lazy\" decoding=\"async\" width=\"576\" height=\"515\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/orvieto.jpg\" class=\"attachment-full size-full\" alt=\"\" srcset=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/orvieto-200x179.jpg 200w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/orvieto-300x268.jpg 300w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/orvieto-400x358.jpg 400w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/orvieto.jpg 576w\" sizes=\"(max-width: 576px) 100vw, 576px\"\/><\/a><\/figure><div class=\"elementor-image-box-content\"><h5 class=\"elementor-image-box-title\"><a href=\"https:\/\/www.openstarts.units.it\/bitstream\/10077\/12084\/1\/Gregori.pdf\">La cartografia di Geologia Urbana in Umbria<\/a><\/h5><p class=\"elementor-image-box-description\">La <a href=\"https:\/\/www.didalms.it\/wordpress\/Glossary\/geologia\/\" data-cmtooltip=\"La &lt;b&gt;geologia&lt;\/b&gt; (dal &lt;a title=&quot;Lingua greca antica&quot; href=&quot;https:\/\/it.wikipedia.org\/wiki\/Lingua_greca_antica&quot;&gt;greco&lt;\/a&gt; &gamma;&#8134;, &lt;i&gt;g&ecirc;&lt;\/i&gt;, &quot;terra&quot; e &lambda;&#972;&gamma;&omicron;&sigmaf;, &lt;i&gt;&lt;a title=&quot;Logos&quot; href=&quot;https:\/\/it.wikipedia.org\/wiki\/Logos&quot;&gt;logos&lt;\/a&gt;&lt;\/i&gt;, &quot;studio&quot;) &egrave; la branca delle &lt;a title=&quot;Scienze della Terra&quot; href=&quot;https:\/\/it.wikipedia.org\/wiki\/Scienze_della_Terra&quot;&gt;scienze della Terra&lt;\/a&gt; che studia la &lt;a title=&quot;Terra&quot; href=&quot;https:\/\/it.wikipedia.org\/wiki\/Terra&quot;&gt;Terra&lt;\/a&gt; e i processi che la plasmano e la cambiano. Nei tempi moderni la geologia &egrave; importante per la valutazione delle risorse idriche, per la previsione e la comprensione dei pericoli naturali, per l&#039;individuazione ed il risanamento dei problemi ambientali, per la pianificazione territoriale e la realizzazione di opere pubbliche e private, per il rilevamento di risorse naturali ad esempio &lt;a title=&quot;Minerale&quot; href=&quot;https:\/\/it.wikipedia.org\/wiki\/Minerale&quot;&gt;minerali&lt;\/a&gt; ed &lt;a title=&quot;Idrocarburi&quot; href=&quot;https:\/\/it.wikipedia.org\/wiki\/Idrocarburi&quot;&gt;idrocarburi&lt;\/a&gt; (in primis &lt;a title=&quot;Petrolio&quot; href=&quot;https:\/\/it.wikipedia.org\/wiki\/Petrolio&quot;&gt;petrolio&lt;\/a&gt; e &lt;a title=&quot;Metano&quot; href=&quot;https:\/\/it.wikipedia.org\/wiki\/Metano&quot;&gt;metano&lt;\/a&gt;), per l&#039;estrazione di molti materiali d&#039;uso commerciale e industriale, per lo studio sui mutamenti del &lt;a title=&quot;Clima&quot; href=&quot;https:\/\/it.wikipedia.org\/wiki\/Clima&quot;&gt;clima&lt;\/a&gt; e dell&#039;ambiente, per la conoscenza del sottosuolo (geognostica) e dei relativi parametri geotecnici, fondamentali per la corretta progettazione di qualunque opera costruttiva.\"  class=\"glossaryLink \">Geologia<\/a> Urbana si occupa di tutti i problemi geologico-ambientali legati alle aree urbane; le citt&agrave; attraverso il loro tessuto e edificato urbano si sviluppano ed evolvono, profondamente condizio- nate dalle caratteristiche del substrato geologico e geomorfologia...<\/p><\/div><\/div>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-01e2ea7 elementor-column elementor-col-25 elementor-top-column\" data-id=\"01e2ea7\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-column-wrap  elementor-element-populated\">\n\t\t\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t<div class=\"elementor-element elementor-element-4a2a694 elementor-position-top elementor-vertical-align-top elementor-widget elementor-widget-image-box\" data-id=\"4a2a694\" data-element_type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"http:\/\/www.didalms.it\/wordpress\/i-fossili-dellappennino-umbro-marchigiano\/\"><img loading=\"lazy\" decoding=\"async\" width=\"600\" height=\"859\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/evoluz_ammonit_umbro_march.jpg\" class=\"attachment-full size-full\" alt=\"\" srcset=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/evoluz_ammonit_umbro_march-200x286.jpg 200w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/evoluz_ammonit_umbro_march-210x300.jpg 210w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/evoluz_ammonit_umbro_march-400x573.jpg 400w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/evoluz_ammonit_umbro_march.jpg 600w\" sizes=\"(max-width: 600px) 100vw, 600px\"\/><\/a><\/figure><div class=\"elementor-image-box-content\"><h5 class=\"elementor-image-box-title\"><a href=\"http:\/\/www.didalms.it\/wordpress\/i-fossili-dellappennino-umbro-marchigiano\/\">I Fossili dell'Appennino Umbro Marchigiano<\/a><\/h5><p class=\"elementor-image-box-description\">Gli Ammoniti (Phylum: Mollusca &ndash; Classe: Cephalopoda &ndash; Sottoclasse: Ammonoidea) sono molluschi cefalopodi comparsi nel Devoniano (ca. 400 milioni di anni fa) ...<\/p><\/div><\/div>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-63bc6c4 elementor-widget elementor-widget-divider\" data-id=\"63bc6c4\" data-element_type=\"widget\" data-widget_type=\"divider.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-divider\">\n\t\t\t<span class=\"elementor-divider-separator\"><\/span>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-b91c464 elementor-position-top elementor-vertical-align-top elementor-widget elementor-widget-image-box\" data-id=\"b91c464\" data-element_type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"https:\/\/www.comune.sanvenanzo.tr.it\/parco-e-museo-vulcanologico\/\"><img loading=\"lazy\" decoding=\"async\" width=\"1324\" height=\"920\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/vulcani-sanvenanzo.jpg\" class=\"attachment-full size-full\" alt=\"\" srcset=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/vulcani-sanvenanzo-200x139.jpg 200w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/vulcani-sanvenanzo-300x208.jpg 300w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/vulcani-sanvenanzo-400x278.jpg 400w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/vulcani-sanvenanzo-600x417.jpg 600w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/vulcani-sanvenanzo-768x534.jpg 768w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/vulcani-sanvenanzo-800x556.jpg 800w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/vulcani-sanvenanzo-1024x712.jpg 1024w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/vulcani-sanvenanzo-1200x834.jpg 1200w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/vulcani-sanvenanzo.jpg 1324w\" sizes=\"(max-width: 1324px) 100vw, 1324px\"\/><\/a><\/figure><div class=\"elementor-image-box-content\"><h5 class=\"elementor-image-box-title\"><a href=\"https:\/\/www.comune.sanvenanzo.tr.it\/parco-e-museo-vulcanologico\/\">Il vulcanismo in Umbria<\/a><\/h5><p class=\"elementor-image-box-description\">Tre vulcani nel raggio di qualche centinaio di metri, la famosa venanzite, l&rsquo;antica breccia ossifera e un museo particolare che alloggia i resti dell&rsquo;elefante preistorico e della tigre dai denti a sciabola.San Venanzo merita una visita accurata. Il piccolo borgo, di antichissime origini, &egrave; edificato proprio sul margine del cratere di un vulcano.<\/p><\/div><\/div>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-f20ac19 elementor-column elementor-col-25 elementor-top-column\" data-id=\"f20ac19\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-column-wrap  elementor-element-populated\">\n\t\t\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t<div class=\"elementor-element elementor-element-e2d8dad elementor-position-top elementor-vertical-align-top elementor-widget elementor-widget-image-box\" data-id=\"e2d8dad\" data-element_type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"https:\/\/ingvterremoti.wordpress.com\/2018\/01\/22\/speciale-2017-un-anno-di-terremoti\/\"><img loading=\"lazy\" decoding=\"async\" width=\"428\" height=\"490\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/faglie_attive_APP_centrale.png\" class=\"attachment-medium_large size-medium_large\" alt=\"\" srcset=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/faglie_attive_APP_centrale-200x229.png 200w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/faglie_attive_APP_centrale-262x300.png 262w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/faglie_attive_APP_centrale-400x458.png 400w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/faglie_attive_APP_centrale.png 428w\" sizes=\"(max-width: 428px) 100vw, 428px\"\/><\/a><\/figure><div class=\"elementor-image-box-content\"><h5 class=\"elementor-image-box-title\"><a href=\"https:\/\/ingvterremoti.wordpress.com\/2018\/01\/22\/speciale-2017-un-anno-di-terremoti\/\">L' Umbria e i terremoti<\/a><\/h5><p class=\"elementor-image-box-description\">I terremoti che hanno interessato Lazio,  Marche ed Umbria sono da ricondurre ad uno &ldquo;stiramento&rdquo; dell&rsquo;Appennino, un processo di estensione da est verso ovest,  ...<\/p><\/div><\/div>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-5e55d7f elementor-widget elementor-widget-divider\" data-id=\"5e55d7f\" data-element_type=\"widget\" data-widget_type=\"divider.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-divider\">\n\t\t\t<span class=\"elementor-divider-separator\"><\/span>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-e2564ec elementor-position-top elementor-vertical-align-top elementor-widget elementor-widget-image-box\" data-id=\"e2564ec\" data-element_type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"http:\/\/www.didalms.it\/wordpress\/2018\/01\/31\/rischio-geologico-da-frana-in-umbria\/\"><img loading=\"lazy\" decoding=\"async\" width=\"471\" height=\"600\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/RU-suscettibilit%C3%A0-zonazione_frane.jpg\" class=\"attachment-full size-full\" alt=\"\" srcset=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/RU-suscettibilit&agrave;-zonazione_frane-200x255.jpg 200w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/RU-suscettibilit&agrave;-zonazione_frane-236x300.jpg 236w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/RU-suscettibilit&agrave;-zonazione_frane-400x510.jpg 400w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/RU-suscettibilit&agrave;-zonazione_frane.jpg 471w\" sizes=\"(max-width: 471px) 100vw, 471px\"\/><\/a><\/figure><div class=\"elementor-image-box-content\"><h5 class=\"elementor-image-box-title\"><a href=\"http:\/\/www.didalms.it\/wordpress\/2018\/01\/31\/rischio-geologico-da-frana-in-umbria\/\">L' Umbria e le frane<\/a><\/h5><p class=\"elementor-image-box-description\">La conoscenza degli aspetti geologici regionale &egrave; importante  per comprendere  i rapporti con la franosit&agrave; del territorio ed individuarne quindi le cause per prevenirne i rischi.<\/p><\/div><\/div>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-192c297 elementor-column elementor-col-25 elementor-top-column\" data-id=\"192c297\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-column-wrap  elementor-element-populated\">\n\t\t\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t<div class=\"elementor-element elementor-element-3227cb3 elementor-position-top elementor-vertical-align-top elementor-widget elementor-widget-image-box\" data-id=\"3227cb3\" data-element_type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"http:\/\/www.siripro.it\/dipgeopa.asp?structure=education&amp;where=regionale&amp;cap=06&amp;lang=it\"><img loading=\"lazy\" decoding=\"async\" width=\"507\" height=\"646\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/appennino-Umbro-Marchigiano.png\" class=\"attachment-full size-full\" alt=\"\" srcset=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/appennino-Umbro-Marchigiano-200x255.png 200w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/appennino-Umbro-Marchigiano-235x300.png 235w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/appennino-Umbro-Marchigiano-400x510.png 400w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/appennino-Umbro-Marchigiano.png 507w\" sizes=\"(max-width: 507px) 100vw, 507px\"\/><\/a><\/figure><div class=\"elementor-image-box-content\"><h5 class=\"elementor-image-box-title\"><a href=\"http:\/\/www.siripro.it\/dipgeopa.asp?structure=education&amp;where=regionale&amp;cap=06&amp;lang=it\">App. Umbro M. \"Inquadramento geologico\"<\/a><\/h5><p class=\"elementor-image-box-description\">L' App. UM forma la parte SE dell' App.Settentrionale: delimitato dalla Colata della Val Marecchia a N, dai M. della Laga a S e dalla depressione Val di Chiana  &ndash;  Valle del Paglia a  W<\/p><\/div><\/div>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-f7c0922 elementor-widget elementor-widget-divider\" data-id=\"f7c0922\" data-element_type=\"widget\" data-widget_type=\"divider.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-divider\">\n\t\t\t<span class=\"elementor-divider-separator\"><\/span>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-ccfdf5d elementor-position-top elementor-vertical-align-top elementor-widget elementor-widget-image-box\" data-id=\"ccfdf5d\" data-element_type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"http:\/\/www.didalms.it\/wordpress\/2018\/01\/31\/idrogeologia-umbria\/\"><img loading=\"lazy\" decoding=\"async\" width=\"1177\" height=\"847\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/Idrogeo_Sud_Umbria-1.png\" class=\"attachment-full size-full\" alt=\"\" srcset=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/Idrogeo_Sud_Umbria-1-200x144.png 200w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/Idrogeo_Sud_Umbria-1-300x216.png 300w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/Idrogeo_Sud_Umbria-1-400x288.png 400w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/Idrogeo_Sud_Umbria-1-600x432.png 600w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/Idrogeo_Sud_Umbria-1-768x553.png 768w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/Idrogeo_Sud_Umbria-1-800x576.png 800w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/Idrogeo_Sud_Umbria-1-1024x737.png 1024w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/01\/Idrogeo_Sud_Umbria-1.png 1177w\" sizes=\"(max-width: 1177px) 100vw, 1177px\"\/><\/a><\/figure><div class=\"elementor-image-box-content\"><h5 class=\"elementor-image-box-title\"><a href=\"http:\/\/www.didalms.it\/wordpress\/2018\/01\/31\/idrogeologia-umbria\/\">L'Umbria e le acque<\/a><\/h5><p class=\"elementor-image-box-description\">l territorio regionale umbro &egrave; compreso quasi interamente all&rsquo;interno del bacino idrografico del fiume Tevere. Solo limitate porzioni, nell&rsquo;area orientale della regione, ricadono nella parte montana di bacini idrografici di corsi d&rsquo;acqua che dopo aver attraversato il territorio della regione Marche, sfociano nel Mare Adriatico: Metauro, Esino, Potenza e Chienti.<\/p><\/div><\/div>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t<\/section><section class=\"elementor-element elementor-element-544be11 elementor-section-boxed elementor-section-height-default elementor-section-height-default elementor-section elementor-top-section\" data-id=\"544be11\" data-element_type=\"section\"><div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t<div class=\"elementor-row\">\n\t\t\t\t<div class=\"elementor-element elementor-element-2448f1a elementor-column elementor-col-100 elementor-top-column\" data-id=\"2448f1a\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-column-wrap  elementor-element-populated\">\n\t\t\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t<div class=\"elementor-element elementor-element-88411ab elementor-widget elementor-widget-divider\" data-id=\"88411ab\" data-element_type=\"widget\" data-widget_type=\"divider.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-divider\">\n\t\t\t<span class=\"elementor-divider-separator\"><\/span>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-9f134ad elementor-widget elementor-widget-text-editor\" data-id=\"9f134ad\" 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<div class=\"elementor-text-editor elementor-clearfix\"><p style=\"text-align: center;\">strumenti e attrezzature di campagna<\/p><\/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<\/div>\n\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t<\/section><section class=\"elementor-element elementor-element-facaed7 elementor-section-boxed elementor-section-height-default elementor-section-height-default elementor-section elementor-top-section\" data-id=\"facaed7\" data-element_type=\"section\" data-settings='{\"background_background\":\"classic\"}'><div class=\"elementor-background-overlay\"><\/div>\n\t\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t<div class=\"elementor-row\">\n\t\t\t\t<div class=\"elementor-element elementor-element-1d2890a elementor-column elementor-col-25 elementor-top-column\" data-id=\"1d2890a\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-column-wrap  elementor-element-populated\">\n\t\t\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t<div class=\"elementor-element elementor-element-cd9161f elementor-position-top elementor-vertical-align-top elementor-widget elementor-widget-image-box\" data-id=\"cd9161f\" data-element_type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"http:\/\/www.didalms.it\/wordpress\/cartografia\/\"><img loading=\"lazy\" decoding=\"async\" width=\"800\" height=\"1024\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/02\/cartageo_spoleto_WEB.jpg\" class=\"attachment-full size-full\" alt=\"\" srcset=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/02\/cartageo_spoleto_WEB-200x256.jpg 200w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/02\/cartageo_spoleto_WEB-234x300.jpg 234w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/02\/cartageo_spoleto_WEB-400x512.jpg 400w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/02\/cartageo_spoleto_WEB-600x768.jpg 600w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/02\/cartageo_spoleto_WEB-768x983.jpg 768w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/02\/cartageo_spoleto_WEB.jpg 800w\" sizes=\"(max-width: 800px) 100vw, 800px\"\/><\/a><\/figure><div class=\"elementor-image-box-content\"><h5 class=\"elementor-image-box-title\"><a href=\"http:\/\/www.didalms.it\/wordpress\/cartografia\/\">cartografia<\/a><\/h5><p class=\"elementor-image-box-description\">La carta geologica, quale strumento di base per la conoscenza fisica del territorio, costituisce il presupposto fondamentale per qualsiasi intervento finalizzato sia alla difesa del suolo, ...<\/p><\/div><\/div>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-12d8ef8 elementor-column elementor-col-25 elementor-top-column\" data-id=\"12d8ef8\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-column-wrap  elementor-element-populated\">\n\t\t\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t<div class=\"elementor-element elementor-element-93dfe00 elementor-position-top elementor-vertical-align-top elementor-widget elementor-widget-image-box\" data-id=\"93dfe00\" data-element_type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"http:\/\/www.didalms.it\/wordpress\/2018\/02\/19\/pubblicazioni\/\"><img loading=\"lazy\" decoding=\"async\" width=\"135\" height=\"235\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/02\/BEMAumbromarchigiano_1_0000.jpg\" class=\"attachment-full size-full\" alt=\"\"\/><\/a><\/figure><div class=\"elementor-image-box-content\"><h5 class=\"elementor-image-box-title\"><a href=\"http:\/\/www.didalms.it\/wordpress\/2018\/02\/19\/pubblicazioni\/\">pubblicazioni e guide geologiche<\/a><\/h5><\/div><\/div>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-4bb3974 elementor-column elementor-col-25 elementor-top-column\" data-id=\"4bb3974\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-column-wrap  elementor-element-populated\">\n\t\t\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t<div class=\"elementor-element elementor-element-abffad5 elementor-position-top elementor-vertical-align-top elementor-widget elementor-widget-image-box\" data-id=\"abffad5\" data-element_type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"http:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2023\/12\/Giardino_Geologico_Venturini_misurare_superfici_linee.pdf\"><img loading=\"lazy\" decoding=\"async\" width=\"500\" height=\"500\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2023\/12\/brunton2.jpg\" class=\"attachment-full size-full\" alt=\"\" srcset=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2023\/12\/brunton2-66x66.jpg 66w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2023\/12\/brunton2-150x150.jpg 150w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2023\/12\/brunton2-200x200.jpg 200w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2023\/12\/brunton2-300x300.jpg 300w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2023\/12\/brunton2-400x400.jpg 400w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2023\/12\/brunton2.jpg 500w\" sizes=\"(max-width: 500px) 100vw, 500px\"\/><\/a><\/figure><div class=\"elementor-image-box-content\"><h5 class=\"elementor-image-box-title\"><a href=\"http:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2023\/12\/Giardino_Geologico_Venturini_misurare_superfici_linee.pdf\">bussola da Geologo<\/a><\/h5><\/div><\/div>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-3183e7f elementor-column elementor-col-25 elementor-top-column\" data-id=\"3183e7f\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-column-wrap  elementor-element-populated\">\n\t\t\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t<div class=\"elementor-element elementor-element-e911d1a elementor-position-top elementor-vertical-align-top elementor-widget elementor-widget-image-box\" data-id=\"e911d1a\" data-element_type=\"widget\" data-widget_type=\"image-box.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<div class=\"elementor-image-box-wrapper\"><figure class=\"elementor-image-box-img\"><a href=\"http:\/\/www.didalms.it\/wordpress\/smartphone-e-gps\/\" target=\"_blank\"><img loading=\"lazy\" decoding=\"async\" width=\"576\" height=\"1024\" src=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/02\/iphone_ctr10000_web.jpg\" class=\"attachment-full size-full\" alt=\"\" srcset=\"https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/02\/iphone_ctr10000_web-169x300.jpg 169w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/02\/iphone_ctr10000_web-200x356.jpg 200w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/02\/iphone_ctr10000_web-400x711.jpg 400w, https:\/\/www.didalms.it\/wordpress\/wp-content\/uploads\/2018\/02\/iphone_ctr10000_web.jpg 576w\" sizes=\"(max-width: 576px) 100vw, 576px\"\/><\/a><\/figure><div class=\"elementor-image-box-content\"><h5 class=\"elementor-image-box-title\"><a href=\"http:\/\/www.didalms.it\/wordpress\/smartphone-e-gps\/\" target=\"_blank\">smartphone e gps<\/a><\/h5><p class=\"elementor-image-box-description\">Lo smartphone, grazie ai suoi sensori, pu&ograve; essere di grande aiuto nelle escursioni in campagna, utilizzando alcune app specifiche....<\/p><\/div><\/div>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t<\/section><section class=\"elementor-element elementor-element-8b6dff5 elementor-section-boxed elementor-section-height-default elementor-section-height-default elementor-section elementor-top-section\" data-id=\"8b6dff5\" data-element_type=\"section\"><div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t<div class=\"elementor-row\">\n\t\t\t\t<div class=\"elementor-element elementor-element-4bf3c0e elementor-column elementor-col-100 elementor-top-column\" data-id=\"4bf3c0e\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-column-wrap  elementor-element-populated\">\n\t\t\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t<div class=\"elementor-element elementor-element-dc9eb43 elementor-widget elementor-widget-shortcode\" data-id=\"dc9eb43\" data-element_type=\"widget\" data-widget_type=\"shortcode.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<div class=\"elementor-shortcode\"><iframe loading=\"lazy\" width=\"100%\" height=\"300px\" frameborder=\"0\" allowfullscreen src=\"https:\/\/umap.openstreetmap.fr\/it\/map\/mappa_umbria_326279?scaleControl=false&amp;miniMap=false&amp;scrollWheelZoom=false&amp;zoomControl=true&amp;allowEdit=false&amp;moreControl=true&amp;searchControl=null&amp;tilelayersControl=null&amp;embedControl=null&amp;datalayersControl=true&amp;onLoadPanel=databrowser&amp;captionBar=false\"><\/iframe><p><a href=\"https:\/\/umap.openstreetmap.fr\/it\/map\/mappa_umbria_326279\">Visualizza a schermo intero<\/a><\/p><\/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<\/div>\n\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t<\/section><\/div>\n\t\t\t<\/div>\n\t\t<\/div>","protected":false},"excerpt":{"rendered":"<p>forra-fosso-marchetto Monte Coscerno Valdorbia Cascata delle Marmore Mortaro Grande Castelluccio-piana [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"ngg_post_thumbnail":0,"footnotes":""},"tags":[],"_links":{"self":[{"href":"https:\/\/www.didalms.it\/wordpress\/wp-json\/wp\/v2\/pages\/7"}],"collection":[{"href":"https:\/\/www.didalms.it\/wordpress\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.didalms.it\/wordpress\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.didalms.it\/wordpress\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.didalms.it\/wordpress\/wp-json\/wp\/v2\/comments?post=7"}],"version-history":[{"count":184,"href":"https:\/\/www.didalms.it\/wordpress\/wp-json\/wp\/v2\/pages\/7\/revisions"}],"predecessor-version":[{"id":13242,"href":"https:\/\/www.didalms.it\/wordpress\/wp-json\/wp\/v2\/pages\/7\/revisions\/13242"}],"wp:attachment":[{"href":"https:\/\/www.didalms.it\/wordpress\/wp-json\/wp\/v2\/media?parent=7"}],"wp:term":[{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.didalms.it\/wordpress\/wp-json\/wp\/v2\/tags?post=7"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}