{"id":87,"date":"2020-07-28T08:56:56","date_gmt":"2020-07-28T06:56:56","guid":{"rendered":"https:\/\/blogs.ua.es\/messinianalicante\/?p=87"},"modified":"2020-07-28T08:56:56","modified_gmt":"2020-07-28T06:56:56","slug":"the-development-of-the-sinus-illicitanus-i","status":"publish","type":"post","link":"https:\/\/blogs.ua.es\/messinianalicante\/2020\/07\/28\/the-development-of-the-sinus-illicitanus-i\/","title":{"rendered":"The development of the sinus illicitanus (I)"},"content":{"rendered":"

The change of the coastline in the southern part of the province\u00a0of Alicante for the last 15,000 years have been modeled and described in the work of Tent-Manclus (2013). It is obtained by integrating data from different\u00a0sources and especially high-resolution seismic profiles of the nearby marine continental\u00a0shelf. Ten periods have been distinguished in the evolution of the Bajo Segura coastline : 1) 15000 BP- 14600 BP: rapid rise; 2)\u00a014600 BP to 13500 BP: the Older Dryas, slow rise; 3) 13500 BP to 12700 BP:\u00a0stability and descent; 4) 12700 BP to 11700 BP: the Younger Dryas, descent of the\u00a0sea \u200b\u200blevel; 5) 11700 BP to 11300 BP: very fast rise; 6) 11300 BP a\u00a08500 BP: rapid rise; 7) 8500 BP = 6500 AC to 8200 BP = 6200 AC: 8.2 ka event\u00a0stabilization; 8) 6,200 BC to 4,000 BC: rise, \u00a0Tabarca Island is form; 9) 4000 BC to 3000 BC: the slow rise due to subsidence\u00a0sinus ilicitanus forms and 10) 3000 BC to the present day 2000 AD: the\u00a0sinus ilicitanus desiccates.<\/p>\n

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Map of the southern Alicante coast area used in the work<\/p><\/div>\n

Maps at different times are show selected from the 164 maps that have been made.\u00a0This is a first version of how the coastline evolves in the region.\u00a0This work\u00a0It can be a starting point to improve knowledge of the historical landscape evolution..<\/p>\n

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Map of the South Alicante coast 15000 BP. The sea level was 70 m below today level. The rivers Vinalopo and Segura were running parallel.<\/p><\/div>\n

The sinus ilicitanus \u00a0dries until today, the rest of which are the lagoons of the Fondo and Santa Polo Salinas.<\/p>\n

Cite as:\u00a0Tent-Mancl\u00fas, J. E. (2013): Cambios de la l\u00ednea de costa en el Bajo Segura (S de Alicante) en los \u00faltimos 15.000 a\u00f1os. Estudios geogr\u00e1ficos, 74 (275): 684-702. Doi: 10.3989\/estgeogr.201324<\/p>\n","protected":false},"excerpt":{"rendered":"

The change of the coastline in the southern part of the province\u00a0of Alicante for the last 15,000 years have been modeled and described in the work of Tent-Manclus (2013). It is obtained by integrating data from different\u00a0sources and especially high-resolution seismic profiles of the nearby marine continental\u00a0shelf. Ten periods have been distinguished in the evolution […]<\/p>\n","protected":false},"author":4347,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[2324666,2325094,676],"tags":[2324668,89231,2324670,2324666,2324669],"class_list":["post-87","post","type-post","status-publish","format-standard","hentry","category-holocene","category-mediterranean","category-sin-categoria","tag-alicante-coast","tag-bajo-segura","tag-coastal-maps","tag-holocene","tag-sea-level-change"],"_links":{"self":[{"href":"https:\/\/blogs.ua.es\/messinianalicante\/wp-json\/wp\/v2\/posts\/87","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/blogs.ua.es\/messinianalicante\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/blogs.ua.es\/messinianalicante\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/blogs.ua.es\/messinianalicante\/wp-json\/wp\/v2\/users\/4347"}],"replies":[{"embeddable":true,"href":"https:\/\/blogs.ua.es\/messinianalicante\/wp-json\/wp\/v2\/comments?post=87"}],"version-history":[{"count":7,"href":"https:\/\/blogs.ua.es\/messinianalicante\/wp-json\/wp\/v2\/posts\/87\/revisions"}],"predecessor-version":[{"id":144,"href":"https:\/\/blogs.ua.es\/messinianalicante\/wp-json\/wp\/v2\/posts\/87\/revisions\/144"}],"wp:attachment":[{"href":"https:\/\/blogs.ua.es\/messinianalicante\/wp-json\/wp\/v2\/media?parent=87"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.ua.es\/messinianalicante\/wp-json\/wp\/v2\/categories?post=87"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.ua.es\/messinianalicante\/wp-json\/wp\/v2\/tags?post=87"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}