Shore erosion between Arboletes and Punta San Bernardo, caribbean coast of Colombia

The present morphology and the inventory of the historical shoreline changes (1938-2005) between Arboletes and Punta San Bernardo evidenced a strong erosional trend along 160 of its 180lan tota1-1ength, resulting in the disparition/retreat of numerous beaches, followed by the consequent flooding/ero...

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Autores:
Correa-Arango, Ivan D.
Ríos, A
González, D
Toro, M
Ojeda, G
Restrepo, L
Tipo de recurso:
Fecha de publicación:
2007
Institución:
Universidad EAFIT
Repositorio:
Repositorio EAFIT
Idioma:
spa
OAI Identifier:
oai:repository.eafit.edu.co:10784/1602
Acceso en línea:
http://hdl.handle.net/10784/1602
Palabra clave:
ACANTILADOS
EROSIÓN COSTERA
ESPOLONES
DIAPIROS
GEOMORFOLOGÍA
GEOTECTÓNICA
ECOSISTEMAS COSTEROS
NIVEL DEL MAR
Caribbean Coast
beach erosion
groins
cliff erosion
Coast changes
Jetties
Diapirs
Geomorphology
Geology, structural
Coastal biotic communities
Sea level
Colombia
Costa Caribe
erosión de playas
erosión de acantilados
Rights
License
Acceso restringido
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oai_identifier_str oai:repository.eafit.edu.co:10784/1602
network_acronym_str REPOEAFIT2
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repository_id_str
dc.title.eng.fl_str_mv Shore erosion between Arboletes and Punta San Bernardo, caribbean coast of Colombia
dc.title.spa.fl_str_mv Erosión litoral entre Arboletes y Punta San Bernardo, Costa Caribe Colombiana
title Shore erosion between Arboletes and Punta San Bernardo, caribbean coast of Colombia
spellingShingle Shore erosion between Arboletes and Punta San Bernardo, caribbean coast of Colombia
ACANTILADOS
EROSIÓN COSTERA
ESPOLONES
DIAPIROS
GEOMORFOLOGÍA
GEOTECTÓNICA
ECOSISTEMAS COSTEROS
NIVEL DEL MAR
Caribbean Coast
beach erosion
groins
cliff erosion
Coast changes
Jetties
Diapirs
Geomorphology
Geology, structural
Coastal biotic communities
Sea level
Colombia
Costa Caribe
erosión de playas
erosión de acantilados
title_short Shore erosion between Arboletes and Punta San Bernardo, caribbean coast of Colombia
title_full Shore erosion between Arboletes and Punta San Bernardo, caribbean coast of Colombia
title_fullStr Shore erosion between Arboletes and Punta San Bernardo, caribbean coast of Colombia
title_full_unstemmed Shore erosion between Arboletes and Punta San Bernardo, caribbean coast of Colombia
title_sort Shore erosion between Arboletes and Punta San Bernardo, caribbean coast of Colombia
dc.creator.fl_str_mv Correa-Arango, Ivan D.
Ríos, A
González, D
Toro, M
Ojeda, G
Restrepo, L
dc.contributor.department.spa.fl_str_mv Universidad EAFIT. Departamento de Geología
dc.contributor.eafitauthor.spa.fl_str_mv Ivan D. Correa-Arango (icorrea@eafit.edu.co)
dc.contributor.author.spa.fl_str_mv Correa-Arango, Ivan D.
Ríos, A
González, D
Toro, M
Ojeda, G
Restrepo, L
dc.contributor.researchgroup.spa.fl_str_mv Ciencias del Mar
dc.subject.lemb.spa.fl_str_mv ACANTILADOS
EROSIÓN COSTERA
ESPOLONES
DIAPIROS
GEOMORFOLOGÍA
GEOTECTÓNICA
ECOSISTEMAS COSTEROS
NIVEL DEL MAR
topic ACANTILADOS
EROSIÓN COSTERA
ESPOLONES
DIAPIROS
GEOMORFOLOGÍA
GEOTECTÓNICA
ECOSISTEMAS COSTEROS
NIVEL DEL MAR
Caribbean Coast
beach erosion
groins
cliff erosion
Coast changes
Jetties
Diapirs
Geomorphology
Geology, structural
Coastal biotic communities
Sea level
Colombia
Costa Caribe
erosión de playas
erosión de acantilados
dc.subject.keyword.eng.fl_str_mv Caribbean Coast
beach erosion
groins
cliff erosion
Coast changes
Jetties
Diapirs
Geomorphology
Geology, structural
Coastal biotic communities
Sea level
dc.subject.keyword.spa.fl_str_mv Colombia
Costa Caribe
erosión de playas
erosión de acantilados
description The present morphology and the inventory of the historical shoreline changes (1938-2005) between Arboletes and Punta San Bernardo evidenced a strong erosional trend along 160 of its 180lan tota1-1ength, resulting in the disparition/retreat of numerous beaches, followed by the consequent flooding/erosion of the adjacent littoral terraces and mangrove swamps. In general terms, the littoral Arbo1etes-Punta San Bernardo retreated 30 to 100m during the last seven decades, at rates between 0.5 and 1.5 m/year; maximum values were found at some critical sectors in the Arboletes-Punta Brava shore segment where magnitudes of coastline retreat were in the order of 900-1.500m at erosion rates up to 70 m/year during the period 19601975. Shore erosion in the study area results both from marine and subaerial processes and the combination of geological factors (neotectonism and effects of mud diapirism, minor stocks of sands, relative sea level rise, poor geotechnical characteristics of cliff's rocks) and human interventions (intensive sand mining from beaches and rivers, land uses with inadequate water management practices, adverse effects of groins and other rigid structures of defense). The precise definition of each one of these factors is necessary for planning the development of the area considering the future sea level rise associated to the Global Climate Change.
publishDate 2007
dc.date.issued.none.fl_str_mv 2007-07-02
dc.date.available.none.fl_str_mv 2014-05-12T20:22:08Z
dc.date.accessioned.none.fl_str_mv 2014-05-12T20:22:08Z
dc.type.eng.fl_str_mv info:eu-repo/semantics/article
article
info:eu-repo/semantics/publishedVersion
publishedVersion
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dc.type.local.spa.fl_str_mv Artículo
status_str publishedVersion
dc.identifier.issn.none.fl_str_mv 0120-0283
dc.identifier.uri.none.fl_str_mv http://hdl.handle.net/10784/1602
identifier_str_mv 0120-0283
url http://hdl.handle.net/10784/1602
dc.language.iso.eng.fl_str_mv spa
language spa
dc.relation.ispartof.spa.fl_str_mv Boletín de Geología Vol. 29, No. 2,julío -diciembre de 2007, pp 115-130
dc.relation.uri.none.fl_str_mv http://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/459
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dc.rights.local.spa.fl_str_mv Acceso restringido
rights_invalid_str_mv Acceso restringido
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dc.publisher.none.fl_str_mv Universidad Industrial de Santander
publisher.none.fl_str_mv Universidad Industrial de Santander
institution Universidad EAFIT
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spelling 2014-05-12T20:22:08Z2007-07-022014-05-12T20:22:08Z0120-0283http://hdl.handle.net/10784/1602The present morphology and the inventory of the historical shoreline changes (1938-2005) between Arboletes and Punta San Bernardo evidenced a strong erosional trend along 160 of its 180lan tota1-1ength, resulting in the disparition/retreat of numerous beaches, followed by the consequent flooding/erosion of the adjacent littoral terraces and mangrove swamps. In general terms, the littoral Arbo1etes-Punta San Bernardo retreated 30 to 100m during the last seven decades, at rates between 0.5 and 1.5 m/year; maximum values were found at some critical sectors in the Arboletes-Punta Brava shore segment where magnitudes of coastline retreat were in the order of 900-1.500m at erosion rates up to 70 m/year during the period 19601975. Shore erosion in the study area results both from marine and subaerial processes and the combination of geological factors (neotectonism and effects of mud diapirism, minor stocks of sands, relative sea level rise, poor geotechnical characteristics of cliff's rocks) and human interventions (intensive sand mining from beaches and rivers, land uses with inadequate water management practices, adverse effects of groins and other rigid structures of defense). The precise definition of each one of these factors is necessary for planning the development of the area considering the future sea level rise associated to the Global Climate Change.Las morfología actual y el inventario de cambios de la línea de costa (1938-2005) del litoral Arboletes-Punta San Bernardo evidencian su carácter fuertemente erosional, caracterizado a lo largo de su mayor longitud (160 de 180lan) por la desaparición/retroceso de numerosas playas y la erosión/inundación consecuente de las terrazas litorales y/o pantanos de manglar adyacentes. En términos generales, el litoral Arboletes-Punta San Bernardo retrocedió entre 30 y 100m durante las siete últimas décadas, a tasas entre 0.5 y 1.5 m/año, superadas en varios sectores críticos (Arboletes-Punta Brava) en los cuales las magnitudes de la erosión fueron del orden de los 900-1.500m a velocidades de 70 m/año durante 19601975. La erosión litoral en la zona resulta tanto de procesos marinos como subaéreos, y de la combinación de factores geológicos (neotectonismo/diapirismo de Iodos, pocos aportes arenosos, ascenso relativo del nivel del mar, características geotécnicas pobres de las rocas) y antrópicos -minería intensiva de arenas de playas y ríos, usos diversos sin manejo de aguas lluvias y residuales, efectos de espolones y obras de defensa. La definición precisa de estos factores es necesaria para planificar el desarrollo litoral considerando aspectos como el ascenso futuro del nivel del mar asociado al Cambio Climático Global.spaUniversidad Industrial de SantanderBoletín de Geología Vol. 29, No. 2,julío -diciembre de 2007, pp 115-130http://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/459Shore erosion between Arboletes and Punta San Bernardo, caribbean coast of ColombiaErosión litoral entre Arboletes y Punta San Bernardo, Costa Caribe Colombianainfo:eu-repo/semantics/articlearticleinfo:eu-repo/semantics/publishedVersionpublishedVersionArtículohttp://purl.org/coar/version/c_970fb48d4fbd8a85http://purl.org/coar/resource_type/c_6501http://purl.org/coar/resource_type/c_2df8fbb1Acceso restringidohttp://purl.org/coar/access_right/c_16ecACANTILADOSEROSIÓN COSTERAESPOLONESDIAPIROSGEOMORFOLOGÍAGEOTECTÓNICAECOSISTEMAS COSTEROSNIVEL DEL MARCaribbean Coastbeach erosiongroinscliff erosionCoast changesJettiesDiapirsGeomorphologyGeology, structuralCoastal biotic communitiesSea levelColombiaCosta Caribeerosión de playaserosión de acantiladosUniversidad EAFIT. Departamento de GeologíaIvan D. Correa-Arango (icorrea@eafit.edu.co)Correa-Arango, Ivan D.Ríos, AGonzález, DToro, MOjeda, GRestrepo, LCiencias del MarBoletín de GeologíaLICENSElicense.txtlicense.txttext/plain; charset=utf-81748https://repository.eafit.edu.co/bitstreams/cd5ed784-ed50-4c80-a8c8-70be06b82fc4/download8a4605be74aa9ea9d79846c1fba20a33MD52ORIGINALErosion Litoral entre Arboletes y Punta San Bernardo.pdfErosion Litoral entre Arboletes y Punta San Bernardo.pdfTexto completoapplication/pdf11793689https://repository.eafit.edu.co/bitstreams/29f302a3-50f4-4fc3-b306-256eac34cc71/download5462290ebc3f4ff199686d056e313c60MD5310784/1602oai:repository.eafit.edu.co:10784/16022022-08-26 09:27:23.403open.accesshttps://repository.eafit.edu.coRepositorio Institucional Universidad EAFITrepositorio@eafit.edu.co