{"id":895,"date":"2015-12-17T12:10:02","date_gmt":"2015-12-17T11:10:02","guid":{"rendered":"https:\/\/ccgm.org\/produit\/carte-morpho-bathymetrique-de-la-mediterranee-orientale\/"},"modified":"2025-01-22T15:00:53","modified_gmt":"2025-01-22T14:00:53","slug":"carte-morpho-bathymetrique-de-la-mediterranee-orientale","status":"publish","type":"product","link":"https:\/\/ccgm.org\/es\/producto\/mapa-morfo-batimetria-del-mediterraneo-oriental\/","title":{"rendered":"Mapa morfo-batim\u00e9trico del Mediterr\u00e1neo Oriental"},"content":{"rendered":"

Mapa morfo-batim\u00e9trico del Mediterr\u00e1neo Oriental<\/strong><\/p>\n

Este resumen morfobatim\u00e9trico del Mediterr\u00e1neo oriental se ha construido a partir de un modelo digital del terreno (MDT) de 100 m; este modelo se basa en datos batim\u00e9tricos de diversos buques de institutos y organismos perimediterr\u00e1neos, adquiridos a partir de sistemas multihaz a menudo diferentes. Sin embargo, puede estimarse que, a profundidades de agua superiores a 2.000 metros, m\u00e1s de 90% del lecho marino de la cuenca ha sido cartografiado en detalle por estos sistemas.<\/p>\n

El objetivo principal del mapa es utilizar estos datos precisos para ilustrar la variedad de procesos geol\u00f3gicos activos (sedimentarios, tect\u00f3nicos, de escape de fluidos, magm\u00e1ticos) que dan forma y dejan sus espectaculares huellas en el lecho marino de la cuenca oriental del Mediterr\u00e1neo.<\/p>\n

Las opciones gr\u00e1ficas favorecen la representaci\u00f3n detallada de las morfolog\u00edas resultantes de estos procesos en las cuatro grandes zonas de la cuenca especialmente activas geol\u00f3gicamente, de oeste a este: a) el Prisma Calabr\u00e9s (al norte del mar J\u00f3nico), b) la Arruga Mediterr\u00e1nea (zona central), c) el Cono del Nilo (al norte de la costa egipcia) y d) el Monte Erat\u00f3stenes (al sur de la isla de Chipre).<\/p>\n

Fuera de las zonas cubiertas por este MDT, el mapa se complement\u00f3 con datos de GEBCO (http:\/\/www.gebco.net\/data_and_products\/gebco_digital_atlas\/<\/a>) y el proyecto EMODNET (http:\/\/www.emodnet-hydrography.eu\/<\/a>).<\/p>\n

Varios artefactos derivados del uso de estos datos (en particular, la visibilidad de la cuadr\u00edcula) son detectables en la mayor parte de las zonas de margen continental no cartografiadas por sistemas multihaz, as\u00ed como en el sur del mar Adri\u00e1tico. Adem\u00e1s, no ha sido posible corregir sistem\u00e1ticamente todos los errores de ajuste Z no lineales entre los distintos conjuntos de datos MDT de 100 m; estos errores se deben a la yuxtaposici\u00f3n de datos de distintos sistemas de cartograf\u00eda multihaz (por ejemplo, sondas que funcionan a frecuencias diferentes), o a correcciones no id\u00e9nticas de la velocidad del sonido en el agua.<\/p>\n

Mapa morfo-batim\u00e9trico del Mediterr\u00e1neo Oriental<\/strong><\/p>","protected":false},"excerpt":{"rendered":"

Mapa morfo-batim\u00e9trico del Mediterr\u00e1neo Oriental<\/strong><\/p>\n

1\u00aa edici\u00f3n 2015
\nEscala: 1:1.650.000
\nProyecci\u00f3n: Mercator (N 38\u00b0)
\nDimensiones: 119 x 85 cm
\nAutores: La\u00ebtitia Campistron-Brosolo y Jean Mascle
\nCon el apoyo del proyecto Mistrals del INSU\/CNRS<\/p>\n

Mapa morfo-batim\u00e9trico del Mediterr\u00e1neo Oriental<\/strong><\/p>","protected":false},"featured_media":12992,"comment_status":"closed","ping_status":"closed","template":"","meta":{"inline_featured_image":false,"site-sidebar-layout":"default","site-content-layout":"default","ast-site-content-layout":"default","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":"default","adv-header-id-meta":"","stick-header-meta":"default","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"set","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":""}}},"product_cat":[59,54,62,68,61],"product_tag":[523,525,522,524],"class_list":{"0":"post-895","1":"product","2":"type-product","3":"status-publish","4":"has-post-thumbnail","6":"product_cat-tous-nos-produits","7":"product_cat-cartes","8":"product_cat-continents","9":"product_cat-europe","10":"product_cat-meilleures-ventes","11":"product_tag-bathymetrie-de-la-mediterranee-o","12":"product_tag-fonds-des-oceans","13":"product_tag-mediterranee-orientale","14":"product_tag-morphologie-de-la-medierranee-or","15":"pa_echelle-299","16":"pa_emballage-tubeexcarteroulee","17":"pa_emballage-enveloppeexcarteplieeoulivret","18":"pa_largeur-119cm","19":"pa_longueur-85cm","20":"pa_poids-0134kg","21":"desktop-align-left","22":"tablet-align-left","23":"mobile-align-left","24":"ast-product-gallery-layout-horizontal-slider","25":"ast-product-tabs-layout-distributed","27":"first","28":"instock","29":"shipping-taxable","30":"purchasable","31":"product-type-simple"},"_links":{"self":[{"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product\/895"}],"collection":[{"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product"}],"about":[{"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/types\/product"}],"replies":[{"embeddable":true,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/comments?post=895"}],"version-history":[{"count":0,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product\/895\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/media\/12992"}],"wp:attachment":[{"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/media?parent=895"}],"wp:term":[{"taxonomy":"product_cat","embeddable":true,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product_cat?post=895"},{"taxonomy":"product_tag","embeddable":true,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product_tag?post=895"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}