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...

Full description

Bibliographic Details
Main Authors: Ortega-Montero, Calixto, Rojas-Martínez, Elías
Format: Online
Language:spa
Published: Universidad Pedagógica y Tecnológica de Colombia - UPTC 2017
Subjects:
Online Access:https://revistas.uptc.edu.co/index.php/ingenieria_sogamoso/article/view/880
_version_ 1801706676783415296
author Ortega-Montero, Calixto
Rojas-Martínez, Elías
author_facet Ortega-Montero, Calixto
Rojas-Martínez, Elías
author_sort Ortega-Montero, Calixto
collection OJS
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.   
format Online
id oai:oai.revistas.uptc.edu.co:article-880
institution Revista Ingeniería, Investigación y Desarrollo
language spa
publishDate 2017
publisher Universidad Pedagógica y Tecnológica de Colombia - UPTC
record_format ojs
spelling oai:oai.revistas.uptc.edu.co:article-8802017-09-08T01:16:54Z The hydro-sediments characterization and the erosive processes of the rivers Cesar and Guatapurí, medium course Caracterización hidrosedimentológica y procesos erosivos de los ríos Cesar y Guatapurí parte media Ortega-Montero, Calixto Rojas-Martínez, Elías 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 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.    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. Universidad Pedagógica y Tecnológica de Colombia - UPTC 2017-02-08 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion application/pdf https://revistas.uptc.edu.co/index.php/ingenieria_sogamoso/article/view/880 Ingeniería Investigación y Desarrollo; Vol. 7 No. 2: julio-diciembre de 2008; 13-18 Ingeniería Investigación y Desarrollo; Vol. 7 Núm. 2: julio-diciembre de 2008; 13-18 2422-4324 1900-771X spa https://revistas.uptc.edu.co/index.php/ingenieria_sogamoso/article/view/880/879 Derechos de autor 2008 Ingeniería Investigación y Desarrollo
spellingShingle 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
Ortega-Montero, Calixto
Rojas-Martínez, Elías
The hydro-sediments characterization and the erosive processes of the rivers Cesar and Guatapurí, medium course
title The hydro-sediments characterization and the erosive processes of the rivers Cesar and Guatapurí, medium course
title_alt Caracterización hidrosedimentológica y procesos erosivos de los ríos Cesar y Guatapurí parte media
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_short The hydro-sediments characterization and the erosive processes of the rivers Cesar and Guatapurí, medium course
title_sort hydro sediments characterization and the erosive processes of the rivers cesar and guatapuri medium course
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
topic_facet 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
url https://revistas.uptc.edu.co/index.php/ingenieria_sogamoso/article/view/880
work_keys_str_mv AT ortegamonterocalixto thehydrosedimentscharacterizationandtheerosiveprocessesoftheriverscesarandguatapurimediumcourse
AT rojasmartinezelias thehydrosedimentscharacterizationandtheerosiveprocessesoftheriverscesarandguatapurimediumcourse
AT ortegamonterocalixto caracterizacionhidrosedimentologicayprocesoserosivosdelosrioscesaryguatapuripartemedia
AT rojasmartinezelias caracterizacionhidrosedimentologicayprocesoserosivosdelosrioscesaryguatapuripartemedia
AT ortegamonterocalixto hydrosedimentscharacterizationandtheerosiveprocessesoftheriverscesarandguatapurimediumcourse
AT rojasmartinezelias hydrosedimentscharacterizationandtheerosiveprocessesoftheriverscesarandguatapurimediumcourse