Casa de piedra dam: effects of clear water on the river Colorado hydrography

The construction of Casa de Piedra (Stone House) dam, in the final stretch of Colorado river high valley, radically modified down waters the hydrologic river course, especially regarding sediment transport, the majority of which settles in the lake. Consequently, waters the dam distributes, contain...

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Autor principal: Cazenave, Hector Walter
Formato: Artículo revista
Lenguaje:Español
Publicado: Facultad de Humanidades Universidad Nacional del Comahue 2017
Materias:
Dam
Acceso en línea:http://revele.uncoma.edu.ar/index.php/geografia/article/view/1761
Aporte de:
id I22-R128-article-1761
record_format ojs
institution Universidad Nacional del Comahue
institution_str I-22
repository_str R-128
container_title_str Repositorio de Revistas Electrónicas REVELE (UNComahue)
language Español
format Artículo revista
topic Colorado river
Dam
Erosion
Meanders
Sediments
Río Colorado
Represa
Sedimentos
Erosión
Meandros
spellingShingle Colorado river
Dam
Erosion
Meanders
Sediments
Río Colorado
Represa
Sedimentos
Erosión
Meandros
Cazenave, Hector Walter
Casa de piedra dam: effects of clear water on the river Colorado hydrography
topic_facet Colorado river
Dam
Erosion
Meanders
Sediments
Río Colorado
Represa
Sedimentos
Erosión
Meandros
author Cazenave, Hector Walter
author_facet Cazenave, Hector Walter
author_sort Cazenave, Hector Walter
title Casa de piedra dam: effects of clear water on the river Colorado hydrography
title_short Casa de piedra dam: effects of clear water on the river Colorado hydrography
title_full Casa de piedra dam: effects of clear water on the river Colorado hydrography
title_fullStr Casa de piedra dam: effects of clear water on the river Colorado hydrography
title_full_unstemmed Casa de piedra dam: effects of clear water on the river Colorado hydrography
title_sort casa de piedra dam: effects of clear water on the river colorado hydrography
description The construction of Casa de Piedra (Stone House) dam, in the final stretch of Colorado river high valley, radically modified down waters the hydrologic river course, especially regarding sediment transport, the majority of which settles in the lake. Consequently, waters the dam distributes, contain a remarkable erosive capacity, and accelerate down waters hydrographic processes, increasing river "meandering" and bringing about what is known as the ―clear waters phenomenon causing adverse effects on watering zones.With the purpose of checking the fact in a quantitative way, cartographies from a certain stretch were taken, being this stretch considered a witness one in periodsaround 25 years, assessing meanders appearance and disappearance, and comparingthese quantities with the variation -in the same sense-, that took place since Casa dePiedra dam start up. The quantities were significant considering the relatively shorttime gone by. The fact was checked in a new aero - photographic flight, according towhich, in a shorter lapse, meanders number increased again in the witness stretch.
publisher Facultad de Humanidades Universidad Nacional del Comahue
publishDate 2017
url http://revele.uncoma.edu.ar/index.php/geografia/article/view/1761
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