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...
- 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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|
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 |
dc.type.coarversion.fl_str_mv |
http://purl.org/coar/version/c_970fb48d4fbd8a85 |
dc.type.coar.fl_str_mv |
http://purl.org/coar/resource_type/c_6501 http://purl.org/coar/resource_type/c_2df8fbb1 |
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 |
dc.rights.coar.fl_str_mv |
http://purl.org/coar/access_right/c_16ec |
dc.rights.local.spa.fl_str_mv |
Acceso restringido |
rights_invalid_str_mv |
Acceso restringido http://purl.org/coar/access_right/c_16ec |
dc.publisher.none.fl_str_mv |
Universidad Industrial de Santander |
publisher.none.fl_str_mv |
Universidad Industrial de Santander |
institution |
Universidad EAFIT |
bitstream.url.fl_str_mv |
https://repository.eafit.edu.co/bitstreams/cd5ed784-ed50-4c80-a8c8-70be06b82fc4/download https://repository.eafit.edu.co/bitstreams/29f302a3-50f4-4fc3-b306-256eac34cc71/download |
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MD5 MD5 |
repository.name.fl_str_mv |
Repositorio Institucional Universidad EAFIT |
repository.mail.fl_str_mv |
repositorio@eafit.edu.co |
_version_ |
1814110272759005184 |
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 |