{"id":139488,"date":"2026-01-12T17:46:07","date_gmt":"2026-01-12T17:46:07","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/geomorfologia-de-las-cabeceras-de-los-rios-narcea-navia-y-sil-y-del-parque-nacional-de-la-montana-de-covadonga-no-de-la-peninsula-iberica\/"},"modified":"2026-01-12T17:46:07","modified_gmt":"2026-01-12T17:46:07","slug":"geomorfologia-de-las-cabeceras-de-los-rios-narcea-navia-y-sil-y-del-parque-nacional-de-la-montana-de-covadonga-no-de-la-peninsula-iberica","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/geomorfologia-de-las-cabeceras-de-los-rios-narcea-navia-y-sil-y-del-parque-nacional-de-la-montana-de-covadonga-no-de-la-peninsula-iberica\/","title":{"rendered":"Geomorfolog\u00eda de las cabeceras de los rios narcea, navia y sil y del parque nacional de la monta\u00f1a de covadonga (no de la peninsula iberica)."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Alonso Alonso M. Victoria <\/strong><\/h2>\n<p>Se realizo el estudio geomorfologico de dos areas glaciadas de la cordillera cantabrica, con caracteristicas litologicas bien diferenciadas: la zona de villablino-dega\u00f1a, al oeste, con sustrato siliciclastico y el parque nacional de la monta\u00f1a de covadonga, al este, con sustrato calcareo.Se hicieron dos mapas geomorfologicos a escala 1:25000. A partir de esta cartografia y del analisis de los depositos se deduce, para la zona de villablino-dega\u00f1a, dos etapas glaciares separadas por una fase fluvial. Siguio un periodo tardiglaciar, caracterizado por la formacion de glaciares rocosos, con clima frio y seco y otro postglaciar, en el que se produce una respuesta a la deglaciacion. En la actualidad predominan los procesos fluviales y fluviotorrenciales.  en el parque nacional de la monta\u00f1a de covadonga (macizo occidental de los picos de europa), la litolog\u00eda provoco una respuesta distinta a los mismos procesos. Se reconoce una unica fase glaciar seguida del periodo tardiglaciar con la formacion de lenguas de solifluxion y un periodo postglaciar en el que la descomposicion produjo grandes avalanchas de rocas. Tambien como consecuencia de la litolog\u00eda se produjo un relieve caracteristico (mezcla de formas glaciares y karsticas) que en la actualidad evoluciona por procesos de karstificacion.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Geomorfolog\u00eda de las cabeceras de los rios narcea, navia y sil y del parque nacional de la monta\u00f1a de covadonga (no de la peninsula iberica).<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Geomorfolog\u00eda de las cabeceras de los rios narcea, navia y sil y del parque nacional de la monta\u00f1a de covadonga (no de la peninsula iberica). <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Alonso Alonso M. Victoria <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Oviedo<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1992<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n<h3>Direcci\u00f3n y tribunal<\/h3>\n<ul>\n<li><strong>Director de la tesis<\/strong>\n<ul>\n<li>German Flor Rodriguez<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Mateo Guti\u00e9rrez Elorza <\/li>\n<li>Javier Pedraza Gilsanz (vocal)<\/li>\n<li>Antonio Cendrero Uceda (vocal)<\/li>\n<li>Carmen Pol Mendez (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Alonso Alonso M. Victoria Se realizo el estudio geomorfologico de dos areas glaciadas de la cordillera cantabrica, [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"footnotes":""},"categories":[27,953,445,75,8846],"tags":[253987,9167,253988,48134,115934,7599],"class_list":["post-139488","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-geologia","category-geologia-glacial","category-geomorfologia","category-oviedo","tag-alonso-alonso-m-victoria","tag-antonio-cendrero-uceda","tag-carmen-pol-mendez","tag-german-flor-rodriguez","tag-javier-pedraza-gilsanz","tag-mateo-gutierrez-elorza"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/139488","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/comments?post=139488"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/139488\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=139488"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=139488"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=139488"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}