{"id":136836,"date":"2026-01-12T17:00:40","date_gmt":"2026-01-12T17:00:40","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/geomorfologia-fluvial-y-litoral-del-extremo-oriental-de-guipuzcoa\/"},"modified":"2026-01-12T17:00:40","modified_gmt":"2026-01-12T17:00:40","slug":"geomorfologia-fluvial-y-litoral-del-extremo-oriental-de-guipuzcoa","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/geomorfologia-fluvial-y-litoral-del-extremo-oriental-de-guipuzcoa\/","title":{"rendered":"Geomorfolog\u00eda fluvial y litoral del extremo oriental de guipuzcoa."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Edeso Fito Jos\u00e9 Miguel <\/strong><\/h2>\n<p>Las investigaciones efectuadas en el extremo oriental de guipuzcoa ponen de manifiesto la existencia de dos antiguos niveles marinos ubicados a 40-45 m. Por encima del intermareal actual y a 4-8 m. Por encima de la linea maxima de pleamar. Estas acumulaciones son el resultado de variaciones glacioeustaticas y movimientos neotectonicos, siendo su cronolog\u00eda pleistocena (medio y superior). El relleno holoceno de los estuarios y depresiones es el resultado de tres pulsaciones transgresivas separadas por sendas fases regresivas, pudiendo diferenciar: transgresion de herriko barra (7800-6600 b.P.), 1  fase regresiva (6600-4920 b.P.), transgresion jaizkibel (4920-2780 b.P.), 2  fase regresiva (2780-1390 b.P.), Transgresion playaundi (1390 b.P.). Por ultimo a lo largo del valle del oyarzun se reconocen 5 niveles de acumulacion fluvial colgados a distintas alturas, y en el bidasoa, se observan 5 niveles.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Geomorfolog\u00eda fluvial y litoral del extremo oriental de guipuzcoa.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Geomorfolog\u00eda fluvial y litoral del extremo oriental de guipuzcoa. <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Edeso Fito Jos\u00e9 Miguel <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Zaragoza<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1991<\/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>Felix Ugarte<\/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> Gonzalez Martin Juan  Antonio (vocal)<\/li>\n<li>Guy Mary (vocal)<\/li>\n<li>Alejandro Cearreta Bilbao (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Edeso Fito Jos\u00e9 Miguel Las investigaciones efectuadas en el extremo oriental de guipuzcoa ponen de manifiesto la [&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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