Mélantois
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Mélantois
The Mélantois () is an inland area of northern France, at south-east of Lille. Between the Deûle and the Marque, it is bounded to the north by a line from Willems Willems is a patronymic surname of Dutch origin, equivalent to Williams. In 2008, it was the 6th most common surname in Belgium (18,604 peopleand in 2007 it was the 39th most common surname in the Netherlands (17,042 people People with this surnam ... to La Madeleine. It is a chalky plateau at an altitude of between , with gentle slopes (below 5 %). References Nord (French department) {{Nord-geo-stub ...
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Lille
Lille ( , ; nl, Rijsel ; pcd, Lile; vls, Rysel) is a city in the northern part of France, in French Flanders. On the river Deûle, near France's border with Belgium, it is the capital of the Hauts-de-France Regions of France, region, the Prefectures in France, prefecture of the Nord (French department), Nord Departments of France, department, and the main city of the Métropole Européenne de Lille, European Metropolis of Lille. The city of Lille proper had a population of 234,475 in 2019 within its small municipal territory of , but together with its French suburbs and exurbs the Lille metropolitan area (French part only), which extends over , had a population of 1,510,079 that same year (Jan. 2019 census), the fourth most populated in France after Paris, Lyon, and Marseille. The city of Lille and 94 suburban French municipalities have formed since 2015 the Métropole Européenne de Lille, European Metropolis of Lille, an Indirect election, indirectly elected Métropole, metr ...
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Deûle
The Deûle (; nl, Deule) is a river of northern France which is channeled for the main part of its course (from Lens to Lille). The upstream part is still partly free-flowing and is known as the Souchez. The Deûle flows into the Lys (right bank) in Deûlémont. The Souchez is formed from the union, in the village of Souchez, of two smaller brooks, called the Carency and the Saint-Nazaire. The channeled part comprises two branches: *the high gauge canal known as Canal de la Deûle which ensures the connection between the channeled Lys and the Scarpe (a tributary of the Scheldt) in Douai, *the Canal de Lens, fed by the Souchez, which connects Lens with the Canal de la Deûle at Courrières. Immediately downstream of Lens, the channel is unusually elevated compared to the neighboring banks, as a result of mining depressions. The Deûle flows through the departments of Pas-de-Calais and Nord, and the towns of Lens, Wingles, Loos, Lille, Wambrechies and Quesnoy-sur-Deûle ...
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Marque (river)
The Marque (; nl, Marke) is a long river in France. It is a right tributary of the Deûle. Its source is near the village of Mons-en-Pévèle. Its course crosses the Nord department, notably the eastern part of the agglomeration of Lille. It flows northwards through the towns of Pont-à-Marcq, Tressin, Villeneuve d'Ascq, Croix and Marcq-en-Barœul, finally flowing into the Deûle in Marquette-lez-Lille. Its lowermost section, between Wasquehal and Marquette-lez-Lille, is part of the Canal de Roubaix The Canal de Roubaix is a canal in northern France. It joins the Canal de la Deûle near Marquette-lez-Lille to the Canal de l’Espierres in Belgium at Leers, just east of the former textile manufacturing town Roubaix. It is 20 km long with .... References Rivers of France Villeneuve-d'Ascq Rivers of Nord (French department) Rivers of Hauts-de-France {{France-river-stub ...
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Willems, Nord
Willems (; nl, Willems) is a commune in the Nord department in northern France. Heraldry Population See also *Communes of the Nord department The following is a list of the 648 communes of the Nord department of the French Republic. The communes cooperate in the following intercommunalities (as of 2020):Communes of Nord (French department) French Flanders {{Nord-geo-stub ...
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La Madeleine, Nord
La Madeleine () is a commune in the Nord department in northern France. It is a suburb of the city of Lille, bordering it on its north side. Heraldry History In 1944, Pierre Marchant and Lucien Olivier, two members of the French resistance from La Madeleine, were killed near Hill 60 (Ypres) by Germans. Population Education Schools in the commune: * Public preschools (''écoles maternelles''): Anne Frank, Courbet, d'Hallendre, du Moulin - Alphonse Daudet, and Gaston LeclercqMaternelles et élémentaires
" La Madeleine, Nord. Retrieved on September 4, 2016.
* Public elementary schools: , Louise de Bettignies, Kléber, and Edmond Rostand * Private prescho ...
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Chalk
Chalk is a soft, white, porous, sedimentary carbonate rock. It is a form of limestone composed of the mineral calcite and originally formed deep under the sea by the compression of microscopic plankton that had settled to the sea floor. Chalk is common throughout Western Europe, where deposits underlie parts of France, and steep cliffs are often seen where they meet the sea in places such as the Dover cliffs on the Kent coast of the English Channel. Chalk is mined for use in industry, such as for quicklime, bricks and builder's putty, and in agriculture, for raising pH in soils with high acidity. It is also used for " blackboard chalk" for writing and drawing on various types of surfaces, although these can also be manufactured from other carbonate-based minerals, or gypsum. Description Chalk is a fine-textured, earthy type of limestone distinguished by its light color, softness, and high porosity. It is composed mostly of tiny fragments of the calcite shells or skeletons ...
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Plateau
In geology and physical geography, a plateau (; ; ), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wide ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, Plate tectonics movements and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. The Columbia Plateau in the north-western United States is an example. They may be formed by upwelling of volcanic magma or extrusion of lava. The un ...
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