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Research in the Meurthe and Moselle valleys downstream from the Vosges Massif has resulted in the definition of the terrace system, and in the recognition of the climatic influence on its formation. Eight alluvial terraces were recognized at less than 100m relative height. An absolute chronology was established for the youngest alluvial terraces, based on infrared optically stimulated luminescence...
By comparing the topographic contour map, the Bajocian limestone structural contour map and alluvial terraces in the Toul and Nancy area, it is possible to reconstitute the changes in the drainage pattern and the Moselle and Meuse cuestas (cotes de Moselle et de Meuse) retreat that have taken place since the late Tertiary. The highest reworked alluvial deposits of the palaeo-rivers ('Haute-Moselle'...
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