{"id":134146,"date":"1997-01-01T00:00:00","date_gmt":"1997-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estudio-geomorfologico-del-valle-de-jerte-sistema-central-espanol-secuencia-de-procesos-y-dinamica-morfogenetica-actual\/"},"modified":"1997-01-01T00:00:00","modified_gmt":"1997-01-01T00:00:00","slug":"estudio-geomorfologico-del-valle-de-jerte-sistema-central-espanol-secuencia-de-procesos-y-dinamica-morfogenetica-actual","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estudio-geomorfologico-del-valle-de-jerte-sistema-central-espanol-secuencia-de-procesos-y-dinamica-morfogenetica-actual\/","title":{"rendered":"Estudio geomorfologico del valle de jerte (sistema central espa\u00f1ol): secuencia de procesos y dinamica morfogenetica actual."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Rosa Mar\u00eda Carrasco Gonzalez <\/strong><\/h2>\n<p>Este trabajo tiene como objetivo principal la explicacion del relieve del valle del jerte y los principales fenomenos morfogeneticos que originaron el mismo. La memoria se estructura en dos apartados, uno introductorio que sirve para encuadrar el valle en el contexto fisiografico regional y analizar los factores condicionantes del relieve (clima, vegetacion, litolog\u00eda, estructura, etc.), Otro el analisis geomorfologico concreto.  el analisis comienza con un planteamiento de la estructura del relieve del valle, sus grandes lineas maestras, luego analiza cada dominio genetico (glaciar, periglaciar, gravitacional y fluvial), concluyendo un modelo genetico-evolutivo que se basa en la denominada \u00abinversion morfologica\u00bb: generalizacion de un graben distensivo a finales del neogeno principios del cuaternario que corta ortogonalmente a la estructura previa de relieve.  en lo referente a procesos recientes, destaca la contribucion al mejor conocimiento del glaciarismo pleistoceno (se propone un modelo de monteras de hielo), la neotectonica cuaternaria y la dinamica de vertientes (se detectan y analizan por vez primera en una zona del sistema central grandes movimientos gravitacionales) y la accion antropica sobre ellos.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estudio geomorfologico del valle de jerte (sistema central espa\u00f1ol): secuencia de procesos y dinamica morfogenetica actual.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estudio geomorfologico del valle de jerte (sistema central espa\u00f1ol): secuencia de procesos y dinamica morfogenetica actual. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Rosa Mar\u00eda Carrasco Gonzalez <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1997<\/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> Pedraza Gilsanz JavierDe<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Alfredo Perez Gonzalez <\/li>\n<li> Goy Goy Jos\u00e9 Luis (vocal)<\/li>\n<li>Santiago Gonz\u00e1lez Alonso (vocal)<\/li>\n<li>Eduardo Acaso Deltell (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Rosa Mar\u00eda Carrasco Gonzalez Este trabajo tiene como objetivo principal la explicacion del relieve del valle del [&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":[27,986,953,75],"tags":[7559,65341,7597,38972,38973,25094],"class_list":["post-134146","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-complutense-de-madrid","category-geologia","category-geomorfologia","tag-alfredo-perez-gonzalez","tag-eduardo-acaso-deltell","tag-goy-goy-jose-luis","tag-pedraza-gilsanz-javierde","tag-rosa-maria-carrasco-gonzalez","tag-santiago-gonzalez-alonso"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/134146","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=134146"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/134146\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=134146"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=134146"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=134146"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}