2013
DOI: 10.1007/s10750-013-1490-0
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Channel response to multiple damming in a meandering river, middle and lower Aragón River (Spain)

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Cited by 46 publications
(36 citation statements)
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References 51 publications
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“…Most likely, the Prahova River is an example of a passive meandering [54,55] (sensu), characterized by fine-grained alluvia and low evidence of active erosion/deposition forms. Similar channel narrowing were recorded for the Tisza River (Hungary, [56]), the Ebro River (Spain, [57,58], the Hernád River (Hungary, [51]) and the Aragon River (Spain, [59]). Over time, the Tisza and Ebro rivers metamorphosed into passive meandering, each with a relative lateral stability after 1950 in relation to human pressures (e.g., artificial bank stabilization works, revetments, and increase in reforestation).…”
Section: Interpretation Of Morphological Quality Of the Lower Prahovasupporting
confidence: 76%
“…Most likely, the Prahova River is an example of a passive meandering [54,55] (sensu), characterized by fine-grained alluvia and low evidence of active erosion/deposition forms. Similar channel narrowing were recorded for the Tisza River (Hungary, [56]), the Ebro River (Spain, [57,58], the Hernád River (Hungary, [51]) and the Aragon River (Spain, [59]). Over time, the Tisza and Ebro rivers metamorphosed into passive meandering, each with a relative lateral stability after 1950 in relation to human pressures (e.g., artificial bank stabilization works, revetments, and increase in reforestation).…”
Section: Interpretation Of Morphological Quality Of the Lower Prahovasupporting
confidence: 76%
“…Channel migration and the width of the active channel were found to be reduced, and in the short-circuited reaches the river bed incised. Ibisate et al (2013) conclude that these physical changes could in turn have important effects for river communities and ecosystem functioning. Belletti et al (2012) analyse the braiding pattern of multiple reaches in the Rhône basin and measure several variables describing the physical characters of channel habitats.…”
mentioning
confidence: 89%
“…Ibisate et al (2013) report the long-term hydromorphological changes induced by a reservoir as well as by a chain of small hydropower plants at the middle and lower reaches of the Aragón River in Spain. Channel migration and the width of the active channel were found to be reduced, and in the short-circuited reaches the river bed incised.…”
mentioning
confidence: 99%
“…Desde el ámbito de la geología destacan los trabajos sobre ríos en roca (Ortega y Garzón, 2009;Ortega y Durán, 2010;Ortega et al, 2014), las paleocrecidas (Benito y Thorndycraft, 2005), así como los análisis y cartografías geomorfológicas aplicadas a la gestión de riesgos desde organismos como el IGME (Díez Herrero et al, 2008Lastra et al, 2008), el INDUROT (Sánchez Martínez y Lastra, 2011) y la universidad (Uribelarrea, 2008). Por último, el grupo que desarrolla su investigación en Aragón, País Vasco y Galicia está trabajando en clasificación fluvial, diagnóstico hidromorfológico y aplicaciones a la restauración fluvial y a la gestión de riesgos (Ollero, 2010;Ollero et al, 2011Ollero et al, , 2014Ibisate et al, 2013;Ibisate, 2014;Horacio, 2012Horacio, , 2014.…”
Section: Iii3 La Geomorfología Fluvial En El Siglo XXIunclassified