Géoarchéologie alluviale du site antique de Molesme en plaine alluviale de Laigne (Bourgogne). Réunion des Sciences de la Terre (RST), Dijon.

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Formation processes and sedimentary filling history of closed depressions on the plateau lorrain, north-eastern Paris Basin (France).

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Le quartier bas (BK 04)

Rhine flood deposits recorded in the Gallo-Roman site of Oedenburg (Haut-Rhin, France).

13 pages; International audience; From the first to the fourth century AD, the Gallo-Roman town of Oedenburg developed in the alluvial landscape of the southern Upper Rhine Graben. Throughout this period, the landscape mosaic, composed of palaeochannels, stable palaeoislands and river terraces, continued to evolve. A district of this town, situated on a lateral Rhine channel system, was archaeologically excavated. Largescale excavation and cross-section analysis provide evidence of changing fluvial conditions during the period under study. At about AD 20 or earlier, this lateral part of the floodplain, affected by very fine sedimentation, was occupied by moribund marshy palaeochannels. When…

Temps archéologique, temps géologique : des biais d’enregistrement sédimentaire identifiés sur des sites antiques en domaine alluvial (Molesme (21), Biesheim (68)).

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Rhine’s floods during roman antiquity. Geoarchaeology of the Oedenburg Gallo-Roman site (France).

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Photographies aériennes obliques, ordres de grandeur et paysages

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Le tsunami du 26 décembre 2004

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Géoarchéologie des systèmes fluviaux : les exemples de Molesme et Biesheim.

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Mise en évidence de crues antiques sur le site gallo-romain d’Oedenburg.

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Analyse géo-archéologique de la stratigraphie néolithique de la redoute du camp de Chassey

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Milieux humides et aménagements anthropiques dans la plaine alluviale du Rhin : le site romain d’Oedenburg (Haut-Rhin).

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Saint-Gibrien, Marne, "Derrière les Grands Clos", rapport de fouille archéologique préventive

Le paysage antique

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Roman Rhine settlement dynamics evidenced by coin distribution in a fluvial environment (Oedenburg, Upper Rhine, France).

International audience; On the basis of archaeological and alluvial records, this paper presents the first spatial analysis of artefacts in relation to the evolution of the Rhine River, at the Gallo-Roman site of Oedenburg, during the first four centuries AD. The dataset consisted of several thousand Roman artefacts found by pedestrian prospecting over the last twenty years, over half of which were coins. This dataset was used together with high-resolution topography and geomagnetic mapping, to reconstruct settlement evolution, both on the terrace and in the floodplain. A comprehensive monetary chart has been compiled for the Oedenburg site, which highlights four major phases of settlement.…

Evolution de l’environnement et de l’exploitation minière en Morvan. Palynologie, géochimie et prospections (intervention 557, chantier 303).

Human settlement dynamics and alluvial dynamics of the Rhine River during the Holocene: Geoarchaeology of the site of Oedenburg (Haut-Rhin, France).

The relationship between alluvial dynamics and control parameters such as climate are well known and understood at plurimillennial and pluriannual time-scales. But it is not really the case at multicentennial and multidecennal time-scales compatible with human society settlement time-scales. In a present and near future context, when human settlement may be affected by strong climatic variation, alluvial dynamics understanding is however a major centre of attention to the development of efficient models. To approach this scale-related question, a segment of the Upper Rhine River presenting both anastomosed and braided was investigated. This area also gives us the opportunity to study settle…

Oedenburg. Une agglomération d’époque romaine sur le Rhin supérieur : fouilles françaises, allemandes et suisses à Biesheim-Kunheim (Haut-Rhin)

Die römische Fundstelle Oedenburg (Biesheim-Kunheim, Haut-Rhin, France) wird seit 1998 von einem international Team ausgegraben (Ecole pratique des hautes études, Paris, Universität Freiburg im Breisgau, Deutschland, Universität Basel, Schweiz). Gegenüber dem keltischen Oppidum von Breisach, nahe am heutigen Rhein gelegen, war die Siedlung in einer deutlich anderen Landschaft angelegt worden, die damals von verschiedenen Flussarmen durchzogen war. Nach dem bisherigen Stand der Erforschung scheint der Ort zu Beginn der tiberischen Zeit von einem Militärlager besetzt gewesen zu sein, das zum Kommandobereich von Vindonissa im Nordteil des Territoriums der Rauriker gehörte. Zur gleichen Zeit en…

Impact alluvial du Rhin sur l’occupation du site gallo-romain d’Oedenburg d’après la répartition spatiale des monnaies.

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