[en] The main characteristics of Reims' natural environment make it a plains city, lacking any major waterway, situated in a marginal position, between two sectors of low-lying plateaus. To the west, the territories formed by the Brie, the Soissonais and the Laonnois, are composed of Cenozoic (Tertiary) layers cut into by numerous deep valleys. These valleys provide the plateaus with significantly diversified environments, between the crops on the loess layers, forests generally along the clay covered interfluves, wetland meadows at the foot of the valleys, as well as multiple slopes with suitable exposure for vine cultivation. The Ile-de-France's cuesta bounds these tertiary plateaus and dominates the much flatter chalky Champagne to the east, the Cretaceous (Mesozoic) chalk layers of which compose a much shallower topographical layout. These flatter landscapes facilitate the passage of overland throughways, but the poor soils, without irrigation or modification, remain useful only for pastoralism. The city is located within the breakthrough funnel of the Vesle, a small river native to the Champagne chalklands. This area, punctuated by mounds and foothills situated between two very different natural regions, provides Reims with a varied set of agricultural resources and diversified potential in terms of geomaterials. In addition to the geological and agricultural riches of the Reims plain, this article also details the hydrological framework of the city of Reims, whose historic center is located on the right bank of a small river, the Vesle, bordered by marshy and low-energy areas, in a relatively open environment. The historic heart of the city is located on the right bank of the river, atop an alluvial terrace that protects it from flooding, is responsible the flatness of the terrain and provides it with good access to groundwater (chalk vadose zone). The Vesle, which is about ten meters lower than the ancient city, is in fact a low-energy river, fed by aquifer drainage, with no significant runoff. Its primary bed is occupied by a vast marshy area rich in alkaline peat bogs, which borders the southern portion of the urban zone. The lack of surface runoff and the vulnerability to urban pollution pose a threat to the drinking water supply and wastewater disposal (low dilution) for an urban locality of this size.

[fr] Les principales caractéristiques du cadre naturel de Reims en font une ville de plaine, dépourvue de cours d'eau majeur, dans une situation de marge entre deux secteurs de bas plateaux. À l'ouest, les territoires formés par la Brie, le Soissonais et le Laonnois, sont composés de couches du Cénozoïque (Tertiaire) entaillées par différentes vallées bien incisées. À l'est s'étend la Champagne crayeuse, bien plus plane, dont les couches de craie du Crétacé (Mésozoïque) forment des reliefs peu marqués, qui facilitent le passage des voies de communication terrestres. Cette situation de contact entre deux régions naturelles bien différentes confère à Reims des ressources agricoles variées et des potentialités diversifiées en géomatériaux. Outre les richesses géologiques et agricoles de la plaine rémoise, cet article détaille par ailleurs le cadre hydrologique de la ville de Reims, dont le cœur historique est localisé en rive droite d'un petit cours d'eau, la Vesle, bordé de zones marécageuses et à faible énergie, dans un environnement relativement ouvert.