Algunas pautas del comportamiento hidrogeológico de rocas duras afectadas por glaciarismo y periglaciarismo en Sierra Nevada (España)

dc.contributor.authorCastillo, A.
dc.contributor.authorFedeli, B.
dc.date.accessioned2014-11-06T12:48:33Z
dc.date.available2014-11-06T12:48:33Z
dc.date.issued2002
dc.description.abstractWe discuss the hydrogeologic behaviour of metamorphic schist materials affected by quaternary glacial and periglacial processes. The field study was carried out in the upper part of Sierra Nevada (Spain), in the basins of the Monachil and Dilar rivers, at altitudes of 1500 to 3400 m a.s.l. The results obtained reveal that the flow is mainly at the subsurface and takes place through glaciary and periglaciary deposits and alteration bands. The drainage network is sparse and influenced by rising springs, mainly located on the lower edges of the above mentioned permeable materials. The depletion coefficients were very high, appropriate to a high transmissivity flow of about 1,5 a 8 x 10 2 days'1en_US
dc.identifier.urihttp://hdl.handle.net/10272/9131
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.otherSierra Nevadaen_US
dc.subject.otherHards rocksen_US
dc.subject.otherSubsurface flowen_US
dc.subject.otherGlacial and periglacial processesen_US
dc.titleAlgunas pautas del comportamiento hidrogeológico de rocas duras afectadas por glaciarismo y periglaciarismo en Sierra Nevada (España)en_US
dc.titleHydrogeologic behaviour of hard rocks affected by glaciarism and periglaciarism in Sierra Nevada (Spain)eng
dc.typejournal articleen_US
dspace.entity.typePublication

Files

Original bundle

Now showing 1 - 1 of 1
Loading...
Thumbnail Image
Name:
Algunas.pdf
Size:
906.01 KB
Format:
Adobe Portable Document Format