Bosberg

Vieux-Condé (French pronunciation: [vjø kɔ̃de]; Dutch: Oudkonde) is a commune in the Nord department in northern France. The village stands on a canalised section of the river Scheldt, adjacent to the northwest of Condé-sur-l'Escaut. It is part of the agglomeration (unité urbaine) of Valenciennes.

The Nord-Pas-de-Calais Mining Basin is a mining basin in Northern France that stretches across the Nord and Pas-de-Calais departments. The region is famous for its long history of coal extraction and its testimony to a significant period in the history of industrialisation in Europe, and as a result it was inscribed on the UNESCO World Heritage List in 2012. This area has been shaped by three centuries of coal extraction from the late 17th century through the 20th century, and demonstrates the evolution of coal mining techniques and worker conditions during that time.

Odomez is a commune in the Nord department in northern France.

Fresnes-sur-Escaut (French pronunciation: [fʁɛn syʁ ɛsko], literally Fresnes on Escaut) is a commune in the Nord department in northern France.

The siege of Condé (8 April – 12 July 1793) saw a force made up of Habsburg Austrians and French Royalists commanded by Duke Ferdinand Frederick Augustus of Württemberg lay siege to a Republican French garrison led by Jean Nestor de Chancel. After a blockade lasting about three months the French surrendered the fortress. The operation took place during the War of the First Coalition, part of a larger conflict known as the French Revolutionary Wars. Condé-sur-l'Escaut, France is located near the Belgium border about 14 kilometres (9 mi) northeast of Valenciennes. The Austrian victory at Neerwinden in mid-March drove the French occupation army from the Austrian Netherlands. The subsequent defection of Charles François Dumouriez shook the morale of the French soldiers and caused the politicians to suspect most generals of treason. Austria and her Coalition allies moved against the line of fortresses protecting the northeastern border of France, investing first Condé and Valenciennes soon afterward. Meanwhile, the motley French armies, composed of regulars and raw recruits and led by generals fearful of the guillotine, struggled to defend their nation.

Condé-sur-l'Escaut (French pronunciation: [kɔ̃de syʁ lɛsko], literally Condé on the Escaut; Picard: Condé-su-l'Escaut) is a commune of the Nord department in northern France. It lies on the border with Belgium. The population as of 1999 was 10,527. Residents of the area are known as Condéens or Condéennes. The Mayor of Condé-sur-l'Escaut is Gregory Lelong (2015).

Escautpont (French pronunciation: [ekopɔ̃]; West Flemish: Schledebrug) is a commune in the Nord department in northern France.

The Canal de Pommerœul à Condé is a canal in northern France and southwestern Belgium. It leads from Pommerœul in Belgium to Condé-sur-l'Escaut in France. It is not in service. It is 5 km long and had 3 locks.

The Haine (French: Haine, French pronunciation: [ɛn] ; Dutch: Hene; German: Henne; Picard: Héne; Walloon: Hinne) is a river in southern Belgium (Hainaut) and northern France (Nord), right tributary of the river Scheldt. The Haine gave its name to the County of Hainaut, and the present province of Hainaut. Its source is in Anderlues, Belgium. As the western end of the sillon industriel, Wallonia's industrial backbone, it flows through the heavily industrialized Borinage region, notably the towns La Louvière, Mons and Saint-Ghislain. A few kilometres after crossing the border to France, the Haine flows into the Scheldt in Condé-sur-l'Escaut. Its length within Belgium is 72 km (45 mi) and the Belgian part of its drainage basin is 802 km2 (310 sq mi).

Hergnies (French pronunciation: [ɛʁɲi]) is a commune in the Nord department of northern France.

The Sainte-Barbe Clays Formation is a geological formation in Belgium. It is found in localised areas of the northern margin of the Mons Basin, alongside the equivalently aged Hautrage and Baudour Clay Formations. It is Upper Barremian-Lower Aptian in age. It predominantly consists of laminated clay, with some lignite. It is well known for the "Iguanodon sinkhole" locality near Bernissart where many specimens of Iguanodon bernissartensis were described by Louis Dollo in the late 19th century.