Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/117170
Citations
Scopus Web of Science® Altmetric
?
?
Full metadata record
DC FieldValueLanguage
dc.contributor.authorGuerrero, J.en
dc.contributor.authorGutiérrez, F.en
dc.contributor.authorGarcía-Ruiz, J.en
dc.contributor.authorCarbonel, D.en
dc.contributor.authorLucha, P.en
dc.contributor.authorArnold, L.en
dc.date.issued2018en
dc.identifier.citationLandslides, 2018; 15(10):1975-1989en
dc.identifier.issn1612-510Xen
dc.identifier.issn1612-5118en
dc.identifier.urihttp://hdl.handle.net/2440/117170-
dc.description.abstractThe production of a cartographic landslide inventory in the glaciated headwaters of the upper Gállego River, Axial Zone of the Spanish Pyrenees, revealed several paleolakes. These relict lake basins are related to the blockage of drainages by postglacial earthflows and slides, mainly developed on Paleozoic slates. The paleolakes are recorded either by non-dissected infilled basins or by hanging and incised lacustrine terraces that persisted for thousands of years. The development of lakes upstream of landslides, was favored, despite their erodibility, by high-displacement rates and the occurrence of paired landslides on both sides of the valley. Radiocarbon and single-grain optically stimulated luminescence (OSL) ages obtained on the lake sediments range between 41.5 ± 3.9 ka and 15.1 ± 0.3 ka. These chronologies indicate prolonged landslide activity long after the early deglaciation in the upper Gállego River Valley. The landslide-lake dating results support the interpretation that the regional maximum ice extent (MIE) in the Pyrenees occurred during the marine isotope stage 4 (MIS 4), long before the global Last Glacial Maximum (LGM).en
dc.description.statementofresponsibilityJ. Guerrero, F. Gutiérrez, J.M. García-Ruiz, D. Carbonel, P. Lucha, L.J. Arnolden
dc.language.isoenen
dc.publisherSpringeren
dc.rights© Springer-Verlag GmbH Germany part of Springer Nature 2018en
dc.subjectEarthflows; landslide dating; last glacial maximum; maximum ice extent; deglaciationen
dc.titleLandslide-dam paleolakes in the Central Pyrenees, Upper Gállego River Valley, NE Spain: timing and relationship with deglaciationen
dc.typeJournal articleen
dc.identifier.rmid0030090558en
dc.identifier.doi10.1007/s10346-018-1018-9en
dc.identifier.pubid424781-
pubs.library.collectionIPAS publicationsen
pubs.library.teamDS14en
pubs.verification-statusVerifieden
pubs.publication-statusPublisheden
dc.identifier.orcidArnold, L. [0000-0001-9603-3824]en
Appears in Collections:IPAS publications

Files in This Item:
There are no files associated with this item.


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.