{"id":39291,"date":"1999-01-01T00:00:00","date_gmt":"1999-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/formas-y-procesos-geomorfologicos-diferenciados-en-las-costas-de-galicia-morfodinamica-y-evolucion-de-un-sector-de-costa-rocosa-cabo-silleiro-a-garda-pontevedra\/"},"modified":"1999-01-01T00:00:00","modified_gmt":"1999-01-01T00:00:00","slug":"formas-y-procesos-geomorfologicos-diferenciados-en-las-costas-de-galicia-morfodinamica-y-evolucion-de-un-sector-de-costa-rocosa-cabo-silleiro-a-garda-pontevedra","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/formas-y-procesos-geomorfologicos-diferenciados-en-las-costas-de-galicia-morfodinamica-y-evolucion-de-un-sector-de-costa-rocosa-cabo-silleiro-a-garda-pontevedra\/","title":{"rendered":"Formas y procesos geomorfologicos diferenciados en las costas de galicia:  morfodinamica y evolucion de un sector de costa rocosa: cabo silleiro a garda  (pontevedra)."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Ramon Blanco Chao <\/strong><\/h2>\n<p>El objetivo principal de este trabajo de investigaci\u00f3n es la formulaci\u00f3n de un primer modelo que permita explicar las grandes l\u00edneas del comportamiento morfodin\u00e1mico de las costas rocosas en diferentes escalas de tiempo. Se plantea la definici\u00f3n de las condiciones din\u00e1micas actuales en una costa rocosa baja, identificando las relaciones entre los aspectos estructurales y litol\u00f3gicos con el conjunto de procesos que operan en la franja litoral, haciendo especial hincapi\u00e9 en la distribuci\u00f3n de la energ\u00eda del oleaje sobre las plataformas intermareales durante el ciclo mareal, la presencia de materiales abrasivos y los aspectos biol\u00f3gicos.  se realiza una propuesta de reconstrucci\u00f3n desde el \u00faltimo interglaciar (eemiense o riss-wurm), que pretende poner de manifiesto la importancia de las herencias en la evoluci\u00f3n a largo plazo. Este aspecto es clave para la hip\u00f3tesis planteda sobre la historia holocena de la costa gallega, en la que los procesos fr\u00edos del \u00faltimo periodo glaciar han jugado un importante papel, estableciendo una din\u00e1mica paraglaciar desde el inicio de la transgresi\u00f3n postglaciar hasta la actualidad.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Formas y procesos geomorfologicos diferenciados en las costas de galicia:  morfodinamica y evolucion de un sector de costa rocosa: cabo silleiro a garda  (pontevedra).<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Formas y procesos geomorfologicos diferenciados en las costas de galicia:  morfodinamica y evolucion de un sector de costa rocosa: cabo silleiro a garda  (pontevedra). <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Ramon Blanco Chao <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Santiago de compostela<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1999<\/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>Augusto P\u00e9rez Albert\u00ed<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Jos\u00e9 manuel Rubio recio <\/li>\n<li>assuncao Araujo (vocal)<\/li>\n<li>amalia Yanes luque (vocal)<\/li>\n<li>Antonio Mart\u00ednez cortizas (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Ramon Blanco Chao El objetivo principal de este trabajo de investigaci\u00f3n es la formulaci\u00f3n de un primer [&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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