Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5916
DC FieldValueLanguage
dc.contributor.authorallD'Ecclesiis, G.en
dc.contributor.authorallPolemio, M.; CNR-IRPIen
dc.date.accessioned2010-02-18T19:24:43Zen
dc.date.available2010-02-18T19:24:43Zen
dc.date.issued1994en
dc.identifier.urihttp://hdl.handle.net/2122/5916en
dc.description.abstractThe Niella spring is located on north Mount Sirino slope. The spring aquifer is characterized by the presence of localized fissures in carbonatic rock. The spring is the highest of the aquifer end is placed at half slope. Flinty limestone outcrops along the whole slope; the spring area is characterized by debris outcrops. Spring water comes out in these conditions for described tectonic influence on aquifer permeability. Geological-structural conditions end the effects on groundwater flow are described.en
dc.description.sponsorshipGNDCI-CNRen
dc.language.isoEnglishen
dc.publisher.namePitagora Editriceen
dc.relation.ispartofQuaderni di Geologia Applicataen
dc.relation.ispartofseries2/2en
dc.subjectspringen
dc.subjectgroundwater resourcesen
dc.titleOutflow conditions of Niella Sprong of Lagonegroen
dc.title.alternativeCondizioni di emergenza della sorgente Niella di Lagonegroen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber343-350en
dc.subject.INGV03. Hydrosphere::03.02. Hydrology::03.02.03. Groundwater processesen
dc.description.journalTypeN/A or not JCRen
dc.description.fulltextopenen
dc.contributor.authorD'Ecclesiis, G.en
dc.contributor.authorPolemio, M.en
dc.contributor.departmentCNR-IRPIen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptUniversità della Basilicata-
crisitem.author.deptCNR-IRPI-
crisitem.classification.parent03. Hydrosphere-
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