1. Morphological and sedimentary evolution of an alluvial floodplain in an urban area: geoarchaeological approaches and applications (Tours, France)
- Author
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Xavier Rodier, Amélie Laurent-Dehecq, Jean-Jacques Macaire, Eymeric Morin, Cités, Territoires, Environnement et Sociétés (CITERES), Centre National de la Recherche Scientifique (CNRS)-Université de Tours (UT), GéoHydrosystèmes COntinentaux (GéHCO EA6293), Université de Tours (UT), This work was supported by the French Etablissement Public Loire (EPL) and the European Regional Development Fund (ERDF) as part of the 'Plan Loire Grandeur Nature 2007-2013' programme., Projet ' Relations entre la dynamique de la Loire et du Cher et l'espace urbanisé tourangeau ', Centre National de la Recherche Scientifique (CNRS)-Université de Tours, and Université de Tours
- Subjects
River Loire ,010506 paleontology ,Archeology ,[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory ,Context (language use) ,Present day ,010502 geochemistry & geophysics ,01 natural sciences ,Urban archaeology ,Geostatistics ,[SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology ,Stratigraphy (archaeology) ,0105 earth and related environmental sciences ,geography ,geography.geographical_feature_category ,Bedrock ,City of Tours ,Geomorphology ,[SHS.GEO]Humanities and Social Sciences/Geography ,15. Life on land ,Archaeology ,Alluvial plain ,River Cher ,Sedimentary rock ,Alluvium ,Physical geography ,Geology ,Chronology - Abstract
International audience; Urban zones on alluvial plains offer considerable geoarchaeological potential for understanding river dynamics over large time spans and their relationship with land use, because of the extensive subsoil data that is available. In the alluvial plain of Tours, lying between the Loire and the Cher, multidisciplinary studies of the relationships between societies and environment have been conducted as part of an archaeological research programme launched in the 1960s. A sedimentary database containing data for 1309 surveys has been compiled and assembled in a geographic information system to produce geostatistical models of valley bottom geomorphology. The stratigraphy and chronology of alluvial filling have also been studied with information and C14 and OSL dating obtained during archaeological operations. Taken together, the results offer a new interpretation of the morphological evolution of the alluvial plain of Tours from the Weichselian to the present day, by providing new information that either validates or invalidates previous hypotheses: bedrock incision prior to the end of the Weichselian Upper Pleniglacial, coarse sedimentation during the Lateglacial, relative morphological stability up to the late Holocene. The morphological context of the first human settlements, which are not concentrated on the low alluvial reliefs, and the role of urbanization conditions on the present morphology of the valley floor are also presented. This applied study shows the relevance of combining different methodological approaches.
- Published
- 2014
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