Cambios históricos de los cauces de los ríos Tajo y Jarama en Aranjuez

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dc.contributor.authorPinilla, L.
dc.contributor.authorPérez González, Alfredo
dc.contributor.authorBenito, Gerardo
dc.date.accessioned2017-03-20T11:39:30Z
dc.date.available2017-03-20T11:39:30Z
dc.date.issued1995
dc.description.abstractChanges in channel morphology between 1775 and 7 988, at the confluence of Jarama and Tajo rivers near Aranjuez, have been studied. In contrast to the relative stability of the Tajo river upstream of the confluence with the Jarama river, there is a great inestability at the two other reaches until 7 945. Since then, a relative channel stabilitatlon, mainly due to a reduction of flood frequency and peak dlschargues after dam regulation, has been observeden_US
dc.identifier.urihttp://hdl.handle.net/10272/13462
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherHistorical channel changesen_US
dc.subject.otherFluvial morphological variationsen_US
dc.subject.otherJarama and Tajo riversen_US
dc.titleCambios históricos de los cauces de los ríos Tajo y Jarama en Aranjuezen_US
dc.titleHistorical channel changes of the Jarama and Tajo rivers at Aranjuezeng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 18, (1995)