Please use this identifier to cite or link to this item: https://hdl.handle.net/10216/52669
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dc.creatorH. Esteves
dc.creatorI. Fernandes
dc.creatorC. Vasconcelos
dc.date.accessioned2019-02-02T02:40:07Z-
dc.date.available2019-02-02T02:40:07Z-
dc.date.issued2010
dc.identifier.othersigarra:48283
dc.identifier.urihttps://repositorio-aberto.up.pt/handle/10216/52669-
dc.description.abstractThe Minho's river-side is characterized for abundant joints mainly in granitic lithologies.Small spots of metassediments and sedimentary formations exist, fluvial terraces and alluviums. Thefluvial phenomena, associated to the tectonic and the lithology, are responsible for the Geodiversity.Thus, the Geologic Heritage congregates rock outcrops, faults and other discontinuities, sedimentarydeposits, fishing artefacts which influence the river dynamics, sedimentation, meanders and structures oferosion. The Geoconservation is basic for the sustainable and convenient use of this patrimony
dc.language.isopor
dc.rightsopenAccess
dc.rights.urihttps://creativecommons.org/licenses/by-nc/4.0/
dc.subjectCiências da terra e ciências do ambiente
dc.subjectEarth and related Environmental sciences
dc.titleA margem do rio Minho entre Melgaço e Monção: alguns aspectos do património geológico
dc.typeArtigo em Revista Científica Nacional
dc.contributor.uportoFaculdade de Ciências
dc.subject.fosCiências exactas e naturais::Ciências da terra e ciências do ambiente
dc.subject.fosNatural sciences::Earth and related Environmental sciences
Appears in Collections:FCUP - Artigo em Revista Científica Nacional

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