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Tournaisis. The Tournaisis, or Tournai (Flemish: Doornik ), a territory in the Low Countries in present-day Belgium, is one of Europe's oldest town centres. [1] Located in the Wallonia region of Belgium on the Scheldt River (French: L'Escaut ), northwest of Mons, Tournai residents are primarily French-speaking.
Tournai, known as Tornacum, was a place of minor importance in Roman times, a stopping place where the Roman road from Cologne on the Rhine to Boulogne on the coast crossed the river Scheldt. It was fortified under Emperor Maximiam in the 3rd century AD, [6] when the Roman limes was withdrawn to the string of outposts along the road.
Picardy Wallonia. Picardy Wallonia ( French: Wallonie-Picarde; Picard: Walonnie picarte) or Western Hainaut ( French: Hainaut-Occidental; Picard: Hénau occhidintal) is the North-West part of the province of Hainaut in Wallonia, where the Picard language is used.
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Saint-Martin Abbey, Tournai. Coordinates: 50°36′11″N 3°23′13″E. Preserved side of medieval pledge corridor. Side of the abbot's palace, now city hall. The Saint-Martin Abbey (French: abbaye Saint-Martin) in the historic center of Tournai, in the Wallonia region of Belgium is a former Benedictine abbey, dating back to the 7th century.
The Battle of Tournay or Battle of Tournai or Battle of Pont-à-Chin (22 May 1794) saw Republican French forces led by Jean-Charles Pichegru attack Coalition forces under Emperor Francis II and Prince Josias of Saxe-Coburg-Saalfeld. After a bitter all-day struggle, Coalition troops recaptured a few key positions including Pont-à-Chin, forcing ...
Tournai remained in English hands, with William Blount, 4th Baron Mountjoy as Governor. The fortifications and a new citadel were reconstructed between August 1515 and January 1518, costing around £40,000. Work ceased because Henry VIII planned to restore the town to France. Tournai was returned by treaty on 4 October 1518.
The Tournaisian was named after the Belgian city of Tournai. It was introduced in scientific literature by Belgian geologist André Hubert Dumont in 1832. Like many Devonian and lower Carboniferous stages, the Tournaisian is a unit from West European regional stratigraphy that is now used in the official international time scale.