Recent coral reefs and geology history of providencia island (western caribbean sea, colombia)
Providencia Island, composed of pre-Miocene and Miocene volcanic rocks, is surrounded by an extensive coral reef complex which, from east to west, can besubdivided morphologically and ecologically into the following subparallel units:a) Fore-reef terrace: a bare rocky flat, from one to several kilom...
- Autores:
-
Geister, Jorn
- Tipo de recurso:
- Article of journal
- Fecha de publicación:
- 1986
- Institución:
- Universidad Nacional de Colombia
- Repositorio:
- Universidad Nacional de Colombia
- Idioma:
- spa
- OAI Identifier:
- oai:repositorio.unal.edu.co:unal/41324
- Acceso en línea:
- https://repositorio.unal.edu.co/handle/unal/41324
http://bdigital.unal.edu.co/31421/
- Palabra clave:
- Geology
Earth Sciences
Pre-Miocene
Miocene
volcanic rocks
coral reef
Fore-reef terrace
Barrier reef
Lagoon
Leeward shelf
Submarine terraces
Pleistocene
Geología
Ciencias de la tierra
Geociencias
Pre-Miocene
Miocene
volcanic rocks
coral reef
Fore-reef terrace
Barrier reef
Lagoon
Leeward shelf
Submarine terraces
Pleistocene
- Rights
- openAccess
- License
- Atribución-NoComercial 4.0 Internacional
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oai:repositorio.unal.edu.co:unal/41324 |
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UNACIONAL2 |
network_name_str |
Universidad Nacional de Colombia |
repository_id_str |
|
dc.title.spa.fl_str_mv |
Recent coral reefs and geology history of providencia island (western caribbean sea, colombia) |
title |
Recent coral reefs and geology history of providencia island (western caribbean sea, colombia) |
spellingShingle |
Recent coral reefs and geology history of providencia island (western caribbean sea, colombia) Geology Earth Sciences Pre-Miocene Miocene volcanic rocks coral reef Fore-reef terrace Barrier reef Lagoon Leeward shelf Submarine terraces Pleistocene Geología Ciencias de la tierra Geociencias Pre-Miocene Miocene volcanic rocks coral reef Fore-reef terrace Barrier reef Lagoon Leeward shelf Submarine terraces Pleistocene |
title_short |
Recent coral reefs and geology history of providencia island (western caribbean sea, colombia) |
title_full |
Recent coral reefs and geology history of providencia island (western caribbean sea, colombia) |
title_fullStr |
Recent coral reefs and geology history of providencia island (western caribbean sea, colombia) |
title_full_unstemmed |
Recent coral reefs and geology history of providencia island (western caribbean sea, colombia) |
title_sort |
Recent coral reefs and geology history of providencia island (western caribbean sea, colombia) |
dc.creator.fl_str_mv |
Geister, Jorn |
dc.contributor.author.spa.fl_str_mv |
Geister, Jorn |
dc.subject.proposal.spa.fl_str_mv |
Geology Earth Sciences Pre-Miocene Miocene volcanic rocks coral reef Fore-reef terrace Barrier reef Lagoon Leeward shelf Submarine terraces Pleistocene Geología Ciencias de la tierra Geociencias Pre-Miocene Miocene volcanic rocks coral reef Fore-reef terrace Barrier reef Lagoon Leeward shelf Submarine terraces Pleistocene |
topic |
Geology Earth Sciences Pre-Miocene Miocene volcanic rocks coral reef Fore-reef terrace Barrier reef Lagoon Leeward shelf Submarine terraces Pleistocene Geología Ciencias de la tierra Geociencias Pre-Miocene Miocene volcanic rocks coral reef Fore-reef terrace Barrier reef Lagoon Leeward shelf Submarine terraces Pleistocene |
description |
Providencia Island, composed of pre-Miocene and Miocene volcanic rocks, is surrounded by an extensive coral reef complex which, from east to west, can besubdivided morphologically and ecologically into the following subparallel units:a) Fore-reef terrace: a bare rocky flat, from one to several kilometers broad, sloping gently from the reef to a morphological break below 30 m which marks the beginning of the outer slope.b) Barrier reef: more than 100 m broad and totalling some 30 km in length, it rises up to near low-tide level. Coherent in the north and in the south, its middle section is a chain of coral pillars. A profuse growth of MiIIepora,Palythoa and abundant coralline algae covers the reef crest, where locally a true algal ridge is developed.c) Lagoon: includes a broad and shallow lagoonal terrace adjacent to barrier reef and a deeper lagoon basin, both locally connected by steep "sand cliffs". From the lagoon floor, covered by bare sand and coral rubble, numerouspatch reefs and coral heads to various heights.d) Leeward shelf: rocky flats with scattered coral growth extend from the shore to a steep escarpment at 20 or more meters depth marking the beginning of the western outer slope. Patch reefs and sandy flats are equally abundant.Submarine terraces, escarpments and valleys, as well as an irregular outline of many reefs reflect a complex geomorphological history of the insular shelf duringPleistocene, which is in part concealed by Holocene reef growth and sedimentation. |
publishDate |
1986 |
dc.date.issued.spa.fl_str_mv |
1986 |
dc.date.accessioned.spa.fl_str_mv |
2019-06-28T09:57:03Z |
dc.date.available.spa.fl_str_mv |
2019-06-28T09:57:03Z |
dc.type.spa.fl_str_mv |
Artículo de revista |
dc.type.coar.fl_str_mv |
http://purl.org/coar/resource_type/c_2df8fbb1 |
dc.type.driver.spa.fl_str_mv |
info:eu-repo/semantics/article |
dc.type.version.spa.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.coar.spa.fl_str_mv |
http://purl.org/coar/resource_type/c_6501 |
dc.type.coarversion.spa.fl_str_mv |
http://purl.org/coar/version/c_970fb48d4fbd8a85 |
dc.type.content.spa.fl_str_mv |
Text |
dc.type.redcol.spa.fl_str_mv |
http://purl.org/redcol/resource_type/ART |
format |
http://purl.org/coar/resource_type/c_6501 |
status_str |
publishedVersion |
dc.identifier.uri.none.fl_str_mv |
https://repositorio.unal.edu.co/handle/unal/41324 |
dc.identifier.eprints.spa.fl_str_mv |
http://bdigital.unal.edu.co/31421/ |
url |
https://repositorio.unal.edu.co/handle/unal/41324 http://bdigital.unal.edu.co/31421/ |
dc.language.iso.spa.fl_str_mv |
spa |
language |
spa |
dc.relation.spa.fl_str_mv |
http://revistas.unal.edu.co/index.php/geocol/article/view/30591 |
dc.relation.ispartof.spa.fl_str_mv |
Universidad Nacional de Colombia Revistas electrónicas UN Geología Colombiana Geología Colombiana |
dc.relation.ispartofseries.none.fl_str_mv |
Geología Colombiana - An International Journal on Geosciences; Vol. 15 (1986); 115-134 Geología Colombiana; Vol. 15 (1986); 115-134 2357-3767 0072-0992 |
dc.relation.references.spa.fl_str_mv |
Geister, Jorn (1986) Recent coral reefs and geology history of providencia island (western caribbean sea, colombia). Geología Colombiana - An International Journal on Geosciences; Vol. 15 (1986); 115-134 Geología Colombiana; Vol. 15 (1986); 115-134 2357-3767 0072-0992 . |
dc.rights.spa.fl_str_mv |
Derechos reservados - Universidad Nacional de Colombia |
dc.rights.coar.fl_str_mv |
http://purl.org/coar/access_right/c_abf2 |
dc.rights.license.spa.fl_str_mv |
Atribución-NoComercial 4.0 Internacional |
dc.rights.uri.spa.fl_str_mv |
http://creativecommons.org/licenses/by-nc/4.0/ |
dc.rights.accessrights.spa.fl_str_mv |
info:eu-repo/semantics/openAccess |
rights_invalid_str_mv |
Atribución-NoComercial 4.0 Internacional Derechos reservados - Universidad Nacional de Colombia http://creativecommons.org/licenses/by-nc/4.0/ http://purl.org/coar/access_right/c_abf2 |
eu_rights_str_mv |
openAccess |
dc.format.mimetype.spa.fl_str_mv |
application/pdf |
dc.publisher.spa.fl_str_mv |
Departamento de Geociencias |
institution |
Universidad Nacional de Colombia |
bitstream.url.fl_str_mv |
https://repositorio.unal.edu.co/bitstream/unal/41324/1/30591-110744-1-PB.pdf https://repositorio.unal.edu.co/bitstream/unal/41324/2/30591-110744-1-PB.pdf.jpg |
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a90452f213c46bbc1e443a09cda11613 8f8bf3601e9f1782624a5c8db7eadeb4 |
bitstream.checksumAlgorithm.fl_str_mv |
MD5 MD5 |
repository.name.fl_str_mv |
Repositorio Institucional Universidad Nacional de Colombia |
repository.mail.fl_str_mv |
repositorio_nal@unal.edu.co |
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1814090125658816512 |
spelling |
Atribución-NoComercial 4.0 InternacionalDerechos reservados - Universidad Nacional de Colombiahttp://creativecommons.org/licenses/by-nc/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Geister, Jorndd68598c-503f-4999-b044-dee1afeff56b3002019-06-28T09:57:03Z2019-06-28T09:57:03Z1986https://repositorio.unal.edu.co/handle/unal/41324http://bdigital.unal.edu.co/31421/Providencia Island, composed of pre-Miocene and Miocene volcanic rocks, is surrounded by an extensive coral reef complex which, from east to west, can besubdivided morphologically and ecologically into the following subparallel units:a) Fore-reef terrace: a bare rocky flat, from one to several kilometers broad, sloping gently from the reef to a morphological break below 30 m which marks the beginning of the outer slope.b) Barrier reef: more than 100 m broad and totalling some 30 km in length, it rises up to near low-tide level. Coherent in the north and in the south, its middle section is a chain of coral pillars. A profuse growth of MiIIepora,Palythoa and abundant coralline algae covers the reef crest, where locally a true algal ridge is developed.c) Lagoon: includes a broad and shallow lagoonal terrace adjacent to barrier reef and a deeper lagoon basin, both locally connected by steep "sand cliffs". From the lagoon floor, covered by bare sand and coral rubble, numerouspatch reefs and coral heads to various heights.d) Leeward shelf: rocky flats with scattered coral growth extend from the shore to a steep escarpment at 20 or more meters depth marking the beginning of the western outer slope. Patch reefs and sandy flats are equally abundant.Submarine terraces, escarpments and valleys, as well as an irregular outline of many reefs reflect a complex geomorphological history of the insular shelf duringPleistocene, which is in part concealed by Holocene reef growth and sedimentation.Providencia Island, composed of pre-Miocene and Miocene volcanic rocks, is surrounded by an extensive coral reef complex which, from east to west, can besubdivided morphologically and ecologically into the following subparallel units:a) Fore-reef terrace: a bare rocky flat, from one to several kilometers broad, sloping gently from the reef to a morphological break below 30 m which marks the beginning of the outer slope.b) Barrier reef: more than 100 m broad and totalling some 30 km in length, it rises up to near low-tide level. Coherent in the north and in the south, its middle section is a chain of coral pillars. A profuse growth of MiIIepora,Palythoa and abundant coralline algae covers the reef crest, where locally a true algal ridge is developed.c) Lagoon: includes a broad and shallow lagoonal terrace adjacent to barrier reef and a deeper lagoon basin, both locally connected by steep "sand cliffs". From the lagoon floor, covered by bare sand and coral rubble, numerouspatch reefs and coral heads to various heights.d) Leeward shelf: rocky flats with scattered coral growth extend from the shore to a steep escarpment at 20 or more meters depth marking the beginning of the western outer slope. Patch reefs and sandy flats are equally abundant.Submarine terraces, escarpments and valleys, as well as an irregular outline of many reefs reflect a complex geomorphological history of the insular shelf duringPleistocene, which is in part concealed by Holocene reef growth and sedimentationapplication/pdfspaDepartamento de Geocienciashttp://revistas.unal.edu.co/index.php/geocol/article/view/30591Universidad Nacional de Colombia Revistas electrónicas UN Geología ColombianaGeología ColombianaGeología Colombiana - An International Journal on Geosciences; Vol. 15 (1986); 115-134 Geología Colombiana; Vol. 15 (1986); 115-134 2357-3767 0072-0992Geister, Jorn (1986) Recent coral reefs and geology history of providencia island (western caribbean sea, colombia). Geología Colombiana - An International Journal on Geosciences; Vol. 15 (1986); 115-134 Geología Colombiana; Vol. 15 (1986); 115-134 2357-3767 0072-0992 .Recent coral reefs and geology history of providencia island (western caribbean sea, colombia)Artículo de revistainfo:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501http://purl.org/coar/resource_type/c_2df8fbb1http://purl.org/coar/version/c_970fb48d4fbd8a85Texthttp://purl.org/redcol/resource_type/ARTGeologyEarth SciencesPre-MioceneMiocenevolcanic rockscoral reefFore-reef terraceBarrier reefLagoonLeeward shelfSubmarine terracesPleistoceneGeologíaCiencias de la tierraGeocienciasPre-MioceneMiocenevolcanic rockscoral reefFore-reef terraceBarrier reefLagoonLeeward shelfSubmarine terracesPleistoceneORIGINAL30591-110744-1-PB.pdfapplication/pdf15095209https://repositorio.unal.edu.co/bitstream/unal/41324/1/30591-110744-1-PB.pdfa90452f213c46bbc1e443a09cda11613MD51THUMBNAIL30591-110744-1-PB.pdf.jpg30591-110744-1-PB.pdf.jpgGenerated Thumbnailimage/jpeg7276https://repositorio.unal.edu.co/bitstream/unal/41324/2/30591-110744-1-PB.pdf.jpg8f8bf3601e9f1782624a5c8db7eadeb4MD52unal/41324oai:repositorio.unal.edu.co:unal/413242024-01-29 23:07:08.497Repositorio Institucional Universidad Nacional de Colombiarepositorio_nal@unal.edu.co |