{"id":141051,"date":"2026-01-12T17:59:12","date_gmt":"2026-01-12T17:59:12","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/geomorfologia-glaciar-de-las-montanas-de-panticosa-y-la-ribera-de-biescas\/"},"modified":"2026-01-12T17:59:12","modified_gmt":"2026-01-12T17:59:12","slug":"geomorfologia-glaciar-de-las-montanas-de-panticosa-y-la-ribera-de-biescas","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/geomorfologia-glaciar-de-las-montanas-de-panticosa-y-la-ribera-de-biescas\/","title":{"rendered":"Geomorfolog\u00eda glaciar de las monta\u00f1as de panticosa y la ribera de biescas."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Enrique Serrano Ca\u00f1adas <\/strong><\/h2>\n<p>Esta tesis aborda la problematica geomorfologica de un area de alta monta\u00f1a ubicada en el pirineo aragones. A traves de 1000 paginas, su autor con el auxilio de una magnifica cartografia geomorfologica y con una multitud de graficos y figuras (cortes geologicos, perfiles longitudinales y transversales en los valles de la zona, cortes estratigraficos, datos sedimentologicos, etc) ofrece un riguroso estudio sobre la morfogenesis acontecida, especialmente en el cuaternario reciente y el holoceno. Son muy sobresalientes los capitulos dedicados a las formas y a las acumulaciones glaciares y tambien los consagrados al dominio de las manifestaciones periglaciares antiguas y actuales.  en resumen, una magnifica tesis que permite seguir las secuencias paleo-climaticas acaecidas en una de nuestras principales cordilleras.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Geomorfolog\u00eda glaciar de las monta\u00f1as de panticosa y la ribera de biescas.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Geomorfolog\u00eda glaciar de las monta\u00f1as de panticosa y la ribera de biescas. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Enrique Serrano Ca\u00f1adas <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Aut\u00f3noma de Madrid<\/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>Eduardo Martinez De Pison Stampa<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Jos\u00e9 Luis Pe\u00f1a Monne <\/li>\n<li>Julio Mu\u00f1oz Jimenez (vocal)<\/li>\n<li> Garcia Ruiz Jos\u00e9 Mar\u00eda (vocal)<\/li>\n<li>Manuel Frochoso Sanchez (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Enrique Serrano Ca\u00f1adas Esta tesis aborda la problematica geomorfologica de un area de alta monta\u00f1a ubicada en [&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 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