Belgium , country of northwestern Europe. It is one of the smallest and most densely populated European countries, and it has been, since its independence in , a representative democracy headed by a hereditary constitutional monarch. Initially, Belgium had a unitary form of government. Culturally, Belgium is a heterogeneous country straddling the border between the Romance and Germanic language families of western Europe. Just north of the boundary between Walloon Brabant Brabant Walloon and Flemish Vlaams Brabant lies the officially bilingual but majority French-speaking Brussels-Capital Region, with approximately one-tenth of the total population. See also Fleming and Walloon.
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The Ardennes region is part of the Hercynian orogenic belt of mountain ranges, which reaches from western Ireland into Germany and was formed roughly to million years ago, during the Paleozoic Era. The Ardennes is a plateau cut deeply by the Meuse River and its tributaries.
Its higher points contain peat bogs and have poor drainage; these uplands are unsuitable as cropland. A large depression, known east of the Meuse River as the Famenne and west of it as the Fagne, separates the Ardennes from the geologically and topographically complex foothills to the north.
The principal feature of the area is the Condroz, a plateau more than 1, feet metres in elevation comprising a succession of valleys hollowed out of the limestone between sandstone crests. Its northern boundary is the Sambre-Meuse valleywhich traverses Belgium from south-southwest to northeast.
About half of it remains wooded; in the south lies a small region of iron ore deposits. The area is dissected by the Dender, Senne, Dijle, and other rivers that enter the Schelde Escaut River ; it is bounded to the east by the Herve Plateau.
The Brussels region lies within the Central Plateaus. Bordering the North Sea from France to the Schelde is the low-lying plain of Flanders, which has two main sections. Maritime Flanders, extending inland for about 5 to 10 miles 8 to 16 kmis a region of newly formed and reclaimed land polders protected by a line of dunes and dikes and having largely clay soils.
Interior Flanders comprises most of East and West Flanders and has sand-silt or sand soils. At an elevation of about 80 to feet 25 to 90 metresit is drained by the Leie, Schelde, and Dender rivers flowing northeastward to the Schelde estuary.