{"id":2293,"date":"2025-09-26T17:15:58","date_gmt":"2025-09-26T17:15:58","guid":{"rendered":"https:\/\/stesa.com\/mapas\/?post_type=ficha&p=2293"},"modified":"2025-09-26T17:15:58","modified_gmt":"2025-09-26T17:15:58","slug":"mapa-geologico-de-castilla-y-leon","status":"publish","type":"ficha","link":"https:\/\/stesa.com\/mapas\/doc\/mapa-geologico-de-castilla-y-leon\/","title":{"rendered":"Mapa geol\u00f3gico de Castilla y Le\u00f3n"},"content":{"rendered":"

Geolog\u00eda de Castilla y Le\u00f3n<\/strong><\/p>\n

\"Mapa<\/a>
(formato PDF)<\/a>. El archivo original est\u00e1 en muy alta resoluci\u00f3n. Es posible que no se cargue correctamente o que su navegador se bloquee al abrirlo en tama\u00f1o completo.<\/label><\/figcaption><\/figure>\n

La Meseta septentrional est\u00e1 constituida por z\u00f3calos paleozoicos. Al principio del Mesozoico, una vez finalizado el plegamiento herciniano que elev\u00f3 la actual Centroeuropa y la zona galaica de Espa\u00f1a, los materiales depositados fueron arrastrados por la acci\u00f3n erosiva de los r\u00edos.<\/p>\n

Durante el plegamiento alpino, los materiales que formaban la meseta se rompieron por m\u00faltiples puntos. De esta fractura se elevaron los montes de Le\u00f3n, con monta\u00f1as de no mucha altura y, constituyendo la espina dorsal de la Meseta, la cordillera Cant\u00e1brica y el sistema Central, formado de materiales como el granito o las pizarras metam\u00f3rficas.<\/p>\n

El complejo k\u00e1rstico de Ojo Guare\u00f1a, formado por 110 km de galer\u00edas\u200b y sus cuevas formadas en materiales carbon\u00e1ticos del Coniaciense que se sit\u00faan sobre un nivel de margas impermeables, es el segundo m\u00e1s grande de la pen\u00ednsula.<\/p>\n

Esta configuraci\u00f3n geol\u00f3gica ha permitido afloramientos de agua minero-medicinal o termal, aprovechados ahora o en el pasado, en Almeida de Sayago, Bo\u00f1ar, Calabor, Caldas de Luna, Castromonte, Cucho, Gejuelo del Barro, Morales de Campos, Trescasas, \u00a0lateja y Villarijo, entre otros lugares.<\/p>\n

\"Tipos<\/a>
(formato PDF)<\/a>.<\/label><\/figcaption><\/figure>\n","protected":false},"excerpt":{"rendered":"

Geolog\u00eda de Castilla y Le\u00f3n. La Meseta septentrional est\u00e1 constituida por z\u00f3calos paleozoicos. Al principio del Mesozoico, una vez finalizado el plegamiento …<\/p>\n","protected":false},"author":1,"featured_media":2294,"template":"","categoria_ficha":[1922],"class_list":["post-2293","ficha","type-ficha","status-publish","has-post-thumbnail","hentry","categoria_ficha-mapas-de-castilla-y-leon"],"yoast_head":"\nMapa geol\u00f3gico de Castilla y Le\u00f3n - Galer\u00eda de mapas<\/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:\/\/gifex.com\/mapas\/doc\/mapa-geologico-de-castilla-y-leon\/\" \/>\n<meta property=\"og:locale\" content=\"es_ES\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Mapa geol\u00f3gico de Castilla y Le\u00f3n - Galer\u00eda de mapas\" \/>\n<meta property=\"og:description\" content=\"Geolog\u00eda de Castilla y Le\u00f3n. La Meseta septentrional est\u00e1 constituida por z\u00f3calos paleozoicos. 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