The hydro-sediments characterization and the erosive processes of the rivers Cesar and Guatapurí, medium course
The Cesar River originates in the South East edge of the Sierra Nevada of Santa Marta, and crosses the departament of the Cesar, the Guatapurí River is also born in the Sierra Nevada of Santa Marta, it ends in the right bank of the Cesar River, down watters Valledupar City. Geologically both are fra...
- Autores:
- Tipo de recurso:
- http://purl.org/coar/resource_type/c_6744
- Fecha de publicación:
- 2017
- Institución:
- Universidad Pedagógica y Tecnológica de Colombia
- Repositorio:
- RiUPTC: Repositorio Institucional UPTC
- Idioma:
- spa
- OAI Identifier:
- oai:repositorio.uptc.edu.co:001/12155
- Acceso en línea:
- https://revistas.uptc.edu.co/index.php/ingenieria_sogamoso/article/view/880
https://repositorio.uptc.edu.co/handle/001/12155
- Palabra clave:
- hydro-sedimentology
sedimentation bar
lateral migration
accretion deposits
point bars
braided
bank
superficial glide
hidrosedimentología
meandriforme
barra de sedimentación
migración lateral
depósitos acrecionales
barras de puntas
talud
escurrimiento superficial
- Rights
- License
- Derechos de autor 2008 Ingeniería Investigación y Desarrollo
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2017-02-082024-07-05T18:47:37Z2024-07-05T18:47:37Zhttps://revistas.uptc.edu.co/index.php/ingenieria_sogamoso/article/view/880https://repositorio.uptc.edu.co/handle/001/12155The Cesar River originates in the South East edge of the Sierra Nevada of Santa Marta, and crosses the departament of the Cesar, the Guatapurí River is also born in the Sierra Nevada of Santa Marta, it ends in the right bank of the Cesar River, down watters Valledupar City. Geologically both are framed by the Sierra Nevada of Santa Marta's igneous-metamorphic complex. The Cesar and Guatapurí Rivers present different and contrasting hydro-sedimentologic characters. The Cesar River shows a high sinuosity, a presence of sedimentation bars, the gradient are gentle; a high relatonship of suspenden silts/load channel, high rate of lateral migration, and intense erosive phenomena and deposit on bars of silits. We can classify as braided, and from the point of view of the development state, it con be considered as a young system characteristic of mountainous regions. El río Cesar nace en el flanco suroriental de la Sierra Nevada de Santa Marta y recorre el departamento del Cesar, el Guatapurí nace en la Sierra Nevada de Santa Marta y desemboca en la margen derecha del río Cesar, aguas abajo de Valledupar, geológicamente, ambos se enmarcan en el complejo ígneo-metamórfico de la Sierra Nevada de Santa Marta. Los ríos Cesar y Guatapurí presentan caracteres hidrosedimentológicos diferentes y contrastantes, el primero muestra alta sinuosidad, presencia de barras de sedimentación, pendientes suaves, una alta relación de carga suspendida/carga de lecho, alta rata de migración lateral y cambios de curso, el segundo muestra baja sinuosidad, cambios estaciónales del cauce por acreción lateral, fenómenos erosivos intensos y depositación sobre barras de sedimentos, este se puede clasificar como trenzado y desde el punto de vista del estado de desarrollo se puede considerar como un sistema juvenil propio de regiones montañosas.application/pdfspaspaUniversidad Pedagógica y Tecnológica de Colombia - UPTChttps://revistas.uptc.edu.co/index.php/ingenieria_sogamoso/article/view/880/879Derechos de autor 2008 Ingeniería Investigación y Desarrollohttp://purl.org/coar/access_right/c_abf245http://purl.org/coar/access_right/c_abf2Ingeniería Investigación y Desarrollo; Vol. 7 No. 2: julio-diciembre de 2008; 13-18Ingeniería Investigación y Desarrollo; Vol. 7 Núm. 2: julio-diciembre de 2008; 13-182422-43241900-771Xhydro-sedimentologysedimentation barlateral migrationaccretion depositspoint barsbraidedbanksuperficial glidehidrosedimentologíameandriformebarra de sedimentaciónmigración lateraldepósitos acrecionalesbarras de puntastaludescurrimiento superficialThe hydro-sediments characterization and the erosive processes of the rivers Cesar and Guatapurí, medium courseCaracterización hidrosedimentológica y procesos erosivos de los ríos Cesar y Guatapurí parte mediainfo:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6744http://purl.org/coar/resource_type/c_2df8fbb1http://purl.org/coar/version/c_970fb48d4fbd8a328http://purl.org/coar/version/c_970fb48d4fbd8a85Ortega-Montero, CalixtoRojas-Martínez, Elías001/12155oai:repositorio.uptc.edu.co:001/121552025-07-18 11:25:54.201metadata.onlyhttps://repositorio.uptc.edu.coRepositorio Institucional UPTCrepositorio.uptc@uptc.edu.co |
| dc.title.en-US.fl_str_mv |
The hydro-sediments characterization and the erosive processes of the rivers Cesar and Guatapurí, medium course |
| dc.title.es-ES.fl_str_mv |
Caracterización hidrosedimentológica y procesos erosivos de los ríos Cesar y Guatapurí parte media |
| title |
The hydro-sediments characterization and the erosive processes of the rivers Cesar and Guatapurí, medium course |
| spellingShingle |
The hydro-sediments characterization and the erosive processes of the rivers Cesar and Guatapurí, medium course hydro-sedimentology sedimentation bar lateral migration accretion deposits point bars braided bank superficial glide hidrosedimentología meandriforme barra de sedimentación migración lateral depósitos acrecionales barras de puntas talud escurrimiento superficial |
| title_short |
The hydro-sediments characterization and the erosive processes of the rivers Cesar and Guatapurí, medium course |
| title_full |
The hydro-sediments characterization and the erosive processes of the rivers Cesar and Guatapurí, medium course |
| title_fullStr |
The hydro-sediments characterization and the erosive processes of the rivers Cesar and Guatapurí, medium course |
| title_full_unstemmed |
The hydro-sediments characterization and the erosive processes of the rivers Cesar and Guatapurí, medium course |
| title_sort |
The hydro-sediments characterization and the erosive processes of the rivers Cesar and Guatapurí, medium course |
| dc.subject.en-US.fl_str_mv |
hydro-sedimentology sedimentation bar lateral migration accretion deposits point bars braided bank superficial glide |
| topic |
hydro-sedimentology sedimentation bar lateral migration accretion deposits point bars braided bank superficial glide hidrosedimentología meandriforme barra de sedimentación migración lateral depósitos acrecionales barras de puntas talud escurrimiento superficial |
| dc.subject.es-ES.fl_str_mv |
hidrosedimentología meandriforme barra de sedimentación migración lateral depósitos acrecionales barras de puntas talud escurrimiento superficial |
| description |
The Cesar River originates in the South East edge of the Sierra Nevada of Santa Marta, and crosses the departament of the Cesar, the Guatapurí River is also born in the Sierra Nevada of Santa Marta, it ends in the right bank of the Cesar River, down watters Valledupar City. Geologically both are framed by the Sierra Nevada of Santa Marta's igneous-metamorphic complex. The Cesar and Guatapurí Rivers present different and contrasting hydro-sedimentologic characters. The Cesar River shows a high sinuosity, a presence of sedimentation bars, the gradient are gentle; a high relatonship of suspenden silts/load channel, high rate of lateral migration, and intense erosive phenomena and deposit on bars of silits. We can classify as braided, and from the point of view of the development state, it con be considered as a young system characteristic of mountainous regions. |
| publishDate |
2017 |
| dc.date.accessioned.none.fl_str_mv |
2024-07-05T18:47:37Z |
| dc.date.available.none.fl_str_mv |
2024-07-05T18:47:37Z |
| dc.date.none.fl_str_mv |
2017-02-08 |
| dc.type.none.fl_str_mv |
info:eu-repo/semantics/article |
| dc.type.coar.fl_str_mv |
http://purl.org/coar/resource_type/c_2df8fbb1 |
| dc.type.coarversion.fl_str_mv |
http://purl.org/coar/version/c_970fb48d4fbd8a85 |
| dc.type.coar.spa.fl_str_mv |
http://purl.org/coar/resource_type/c_6744 |
| dc.type.coarversion.spa.fl_str_mv |
http://purl.org/coar/version/c_970fb48d4fbd8a328 |
| format |
http://purl.org/coar/resource_type/c_6744 |
| dc.identifier.none.fl_str_mv |
https://revistas.uptc.edu.co/index.php/ingenieria_sogamoso/article/view/880 |
| dc.identifier.uri.none.fl_str_mv |
https://repositorio.uptc.edu.co/handle/001/12155 |
| url |
https://revistas.uptc.edu.co/index.php/ingenieria_sogamoso/article/view/880 https://repositorio.uptc.edu.co/handle/001/12155 |
| dc.language.none.fl_str_mv |
spa |
| dc.language.iso.none.fl_str_mv |
spa |
| language |
spa |
| dc.relation.none.fl_str_mv |
https://revistas.uptc.edu.co/index.php/ingenieria_sogamoso/article/view/880/879 |
| dc.rights.es-ES.fl_str_mv |
Derechos de autor 2008 Ingeniería Investigación y Desarrollo |
| dc.rights.coar.fl_str_mv |
http://purl.org/coar/access_right/c_abf2 |
| dc.rights.coar.spa.fl_str_mv |
http://purl.org/coar/access_right/c_abf245 |
| rights_invalid_str_mv |
Derechos de autor 2008 Ingeniería Investigación y Desarrollo http://purl.org/coar/access_right/c_abf245 http://purl.org/coar/access_right/c_abf2 |
| dc.format.none.fl_str_mv |
application/pdf |
| dc.publisher.es-ES.fl_str_mv |
Universidad Pedagógica y Tecnológica de Colombia - UPTC |
| dc.source.en-US.fl_str_mv |
Ingeniería Investigación y Desarrollo; Vol. 7 No. 2: julio-diciembre de 2008; 13-18 |
| dc.source.es-ES.fl_str_mv |
Ingeniería Investigación y Desarrollo; Vol. 7 Núm. 2: julio-diciembre de 2008; 13-18 |
| dc.source.none.fl_str_mv |
2422-4324 1900-771X |
| institution |
Universidad Pedagógica y Tecnológica de Colombia |
| repository.name.fl_str_mv |
Repositorio Institucional UPTC |
| repository.mail.fl_str_mv |
repositorio.uptc@uptc.edu.co |
| _version_ |
1839633882416152576 |