Evolution of Sandspits Along the Caribbean Coast of Colombia: Natural and Human Influences

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dc.citation.journalTitleCoastal Research Library
dc.contributor.authorAnfuso, G.spa
dc.contributor.authorRangel-Buitrago, Nelsonspa
dc.contributor.authorCorrea Arango, Ivan Dariospa
dc.contributor.departmentUniversidad EAFIT. Departamento de Geologíaspa
dc.contributor.researchgroupCiencias del Marspa
dc.date.accessioned2021-03-23T20:20:27Z
dc.date.available2021-03-23T20:20:27Z
dc.date.issued2015-01-01
dc.description.abstractThis work deals with the evolution of Bocas de Ceniza-Puerto Caiman, Galerazamba, Isla Cascajo and Punta Canoas coastal sectors, located along the 120 km-long coastline between the Magdalena River mouth and Cartagena de Indias, on the Caribbean coast of Colombia. Comparisons of coastline morphology from reliable ancient charts, modern bathymetric surveys and remote sensing data, show major changes (in some cases at kilometre-scale) related to the rapid erosion and formation of offshore sandy shoals, spits and beaches. These sediment bodies are linked to sediment supply from the Magdalena River. In 1935, after the emplacement of two jetties at the river mouth, sediment was channelled offshore and erosion ensued on the western part of the Magdalena delta. Spits and sandy shoals rapidly migrated down drift. As a result, a spit at Puerto Colombia - present on the 1935 and 1947 aerial photograms – progressively diminished and merged with the coastline between 1953 and 1959. South of this location, a new spit formed before 2000 and it presently shelters a marina at Puerto Velero. At Galerazamba, a 5 km-long spit at a high angle to the coastline, was present until 1864. It was replaced by a new spit, broadly parallel to shoreline, at some point before 1947. This feature was much smaller than the one previously observed and it has migrated down drift until the present. High rates of accretion were also observed around Isla Cascajo, a rocky island that caused the development of a rapidly growing tombolo. At Punta Canoas, a spit formed between 1947 and 1961 and, then migrated southwards.eng
dc.identifierhttps://eafit.fundanetsuite.com/Publicaciones/ProdCientif/PublicacionFrw.aspx?id=2256
dc.identifier.doi10.1007/978-3-319-13716-2_1
dc.identifier.issn22110577
dc.identifier.issn22110585
dc.identifier.otherWOS;000367908700002
dc.identifier.urihttp://hdl.handle.net/10784/26902
dc.language.isoengeng
dc.publisherSPRINGER-VERLAG BERLIN
dc.rightsSPRINGER-VERLAG BERLIN
dc.sourceCoastal Research Library
dc.subject.keywordNova-Scotiaeng
dc.subject.keywordSea-Leveleng
dc.subject.keywordStory Headeng
dc.subject.keywordShorelineeng
dc.subject.keywordBarrierseng
dc.subject.keywordMorphodynamicseng
dc.subject.keywordEventseng
dc.subject.keywordCanadaeng
dc.titleEvolution of Sandspits Along the Caribbean Coast of Colombia: Natural and Human Influenceseng
dc.typeinfo:eu-repo/semantics/articleeng
dc.typearticleeng
dc.typeinfo:eu-repo/semantics/publishedVersioneng
dc.typepublishedVersioneng
dc.type.localArtículospa

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