{"id":79136,"date":"2018-03-09T23:24:58","date_gmt":"2018-03-09T23:24:58","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/tipo-y-evolucion-de-las-costas-rocosas-de-mallorca\/"},"modified":"2018-03-09T23:24:58","modified_gmt":"2018-03-09T23:24:58","slug":"tipo-y-evolucion-de-las-costas-rocosas-de-mallorca","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/tipo-y-evolucion-de-las-costas-rocosas-de-mallorca\/","title":{"rendered":"Tipo y evoluci\u00f3n de las costas rocosas de mallorca"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Pablo Balaguer Huguet <\/strong><\/h2>\n<p>Tipos y evoluci\u00f3n de las costas rocosas de mallorca es una tesis doctoral que se ocupa de los aspectos relacionados con el estudio de las costas rocosas de mallorca. La estructura de la memoria puede dividirse en cuatro partes. La primera parte es una introducci\u00f3n en la que se describe el contexto f\u00edsico en el que se encuentra la isla de mallorca, se describen los principales tipos de costas (playa, sistemas playa-duna, albuferas y marismas y costas rocosas) con la finalidad de ofrecer una imagen de conjunto del \u00e1rea de estudio antes de centrarse \u00fanicamente en las costas rocosas. La primera parte finaliza con un detallado estudio bibliogr\u00e1fico en el que se contemplan los trabajos, de tipo descriptivo-evolutivo, que se ocupan de diversos aspectos geomorfol\u00f3gicos de las costas rocosas de mallorca (cuaternario, morfog\u00e9nesis de calas, karst litoral, estudios de clasificaci\u00f3n y din\u00e1mica). la segunda parte se basa en la realizaci\u00f3n de una clasificaci\u00f3n de las costas rocosas de mallorca seg\u00fan criterios de forma, altura, disposici\u00f3n de los materiales y litolog\u00eda. Dicha clasificaci\u00f3n intenta establecer una relaci\u00f3n entre las unidades morfoestructurales de mallorca (serra de tramuntana, serres de llevant, marinas de migjorn y llevant y cuencas postorog\u00e9nicas -palma, campos, alcudia y pollen\u00ed\u00a7a-). En la tercera parte se estudian una serie de procesos de erosi\u00f3n que afectan a las costas rocosas de mallorca desde un punto de vista macroescalar (movimientos de masas y desprendimientos), mesoescalar (estudio de los fragmentos rocosos desplazados o arrancados) y microescalar (estudio de la disgregaci\u00f3n granular de las paredes de los acantilados y de los procesos bioerosivos de los organismos -gaster\u00f3podos y moluscos- que viven en la interfase tierra-mar de las costas rocosas), calcul\u00e1ndose para cada proceso la tasas de retroceso lineal de la l\u00ednea de costa. Finalmente se establecen unas conclusiones generales y se se\u00f1alan algunas ap<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Tipo y evoluci\u00f3n de las costas rocosas de mallorca<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Tipo y evoluci\u00f3n de las costas rocosas de mallorca <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Pablo Balaguer Huguet <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Illes balears<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 20\/03\/2006<\/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>Juan  Jos\u00e9 Forn\u00f3s Ast\u00f3<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: vicen\u00ed\u00a7 m. Rossell\u00f3 verger <\/li>\n<li> Mateos ruiz rosa Mar\u00eda (vocal)<\/li>\n<li>joaquin Gines gracia (vocal)<\/li>\n<li>joaquin Tintore subirana (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Pablo Balaguer Huguet Tipos y evoluci\u00f3n de las costas rocosas de mallorca es una tesis doctoral que [&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":[27,5742,5741,19034],"tags":[169936,19636,169935,62474,149012,26821],"class_list":["post-79136","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-ciencias-geograficas","category-geografia-fisica","category-illes-balears","tag-joaquin-gines-gracia","tag-joaquin-tintore-subirana","tag-juan-jose-fornos-asto","tag-mateos-ruiz-rosa-maria","tag-pablo-balaguer-huguet","tag-viceni-m-rossello-verger"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/79136","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=79136"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/79136\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=79136"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=79136"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=79136"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}