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dc.contributor.authorLARCANCHÉ, Marie
hal.structure.identifierInstitut de Mécanique et d'Ingénierie [I2M]
dc.contributor.authorVERDET, Cécile
hal.structure.identifierUniversité de Bordeaux [UB]
hal.structure.identifierInstitut de Mécanique et d'Ingénierie [I2M]
dc.contributor.authorSIRIEIX, Colette
hal.structure.identifierArchéologie, Terre, Histoire, Sociétés [Dijon] [ARTeHiS]
dc.contributor.authorSTEINMANN, Ronan
hal.structure.identifierARCHEORIENT - Environnements et sociétés de l'Orient ancien [Archéorient]
dc.contributor.authorCOLIN, Sylvain
hal.structure.identifierLIttoral ENvironnement et Sociétés [LIENSs]
dc.contributor.authorMATHÉ, Vivien
hal.structure.identifierCentre de Recherche en Archéologie, Archéosciences, Histoire [CReAAH]
dc.contributor.authorCHEVILLOT, Christian
dc.contributor.authorMATÉO, Sylvain
hal.structure.identifierInstitut de Mécanique et d'Ingénierie [I2M]
dc.contributor.authorHOUILLON, Nicolas
hal.structure.identifierLIttoral ENvironnement et Sociétés [LIENSs]
hal.structure.identifierIRAMAT-Centre de recherche en physique appliquée à l’archéologie [IRAMAT-CRP2A]
dc.contributor.authorHANTRAIS, Juliette
hal.structure.identifierGPR HUMAN PAST
hal.structure.identifierArchéosciences Bordeaux
hal.structure.identifierCentre National de la Recherche Scientifique [CNRS]
hal.structure.identifierUniversité Bordeaux Montaigne [UBM]
dc.contributor.authorHIRIART, Eneko
dc.date.issued2023
dc.identifier.issn1075-2196
dc.description.abstractEnAbstract This article combining geophysics and archaeology aims to provide a more comprehensive characterization of the La Ruchelle valley located in the south of the Celtic site of La Peyrouse (Saint‐Félix‐de‐Villadeix, Dordogne, France) (occupied between the 3rd century BC and the 2nd century AD) through geological prospection (core sampling, geotechnical prospection and mechanical prospection) and near‐surface geophysics (electrical resistivity tomography). On this site, other studies have been carried out since the discovery of the site, such as magnetic prospecting and a hydrogeological study. Geophysical data coupled with geological prospection were used to understand the geology of the valley: (1) The bottom of the valley is filled with colluvium with a thickness of 6 m maximum; (2) part of the colluvium filling characterize by a very low resistivity is indeed archaeological remains; (3) three very distinct geological horizons have been detected—two of these horizons are characteristic of Campanian limestone (C6d and C6e), and the last consists of colluvium with a filling between 2 and 6 m in the centre of the valley, which is particularly thick. This last very thick formation is in fact filled with archaeological and prehistoric remains.
dc.language.isoen
dc.publisherWiley
dc.title.enA Late Holocene case study from south‐west France: Combining geomorphology and geophysics to understand archaeological site morphology
dc.typeArticle de revue
dc.identifier.doi10.1002/arp.1913
dc.subject.halSciences de l'Homme et Société/Archéologie et Préhistoire
bordeaux.journalArchaeological Prospection
bordeaux.page1-16
bordeaux.peerReviewedoui
hal.identifierhal-04220598
hal.version1
hal.popularnon
hal.audienceInternationale
hal.origin.linkhttps://hal.archives-ouvertes.fr//hal-04220598v1
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