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The geography of France consists of a terrain that is mostly flat plains or gently rolling hills in the north and the west and mountainous in the south (including the Massif Central and the Pyrenees) and the east (the country's highest points being in the Alps). Metropolitan France has a total size of 551,695 km 2 (213,011 sq mi) (Europe only).
Pages in category "Plains of France" The following 6 pages are in this category, out of 6 total. This list may not reflect recent changes. B. Beauce, France; Bresse; C.
Historically, the plains have been the site of numerous battles and invasions, as they offer relatively easy access to neighboring countries and provide an open space for armies to maneuver. They also play a major role in the European Union as a key region for trade and industry. The EU's Common Agricultural Policy, which regulates agricultural ...
Plains of France (6 P) G. Plains of Georgia (country) (3 P) Plains of Germany (2 C, 5 P) ... Plains of the United States (1 C, 15 P) V. Plains of Venezuela (3 P)
North European Plain coloured in green. Topography of the North European Plain.. The North European Plain (German: Norddeutsches Tiefland – North German Plain; Mitteleuropäische Tiefebene; Polish: Nizina Środkowoeuropejska – Central European Plain; Danish: Nordeuropæiske Lavland and Dutch: Noord-Europese Laagvlakte; French: Plaine d'Europe du Nord) is a geomorphological region in Europe ...
France, [X] officially the French Republic, [XI] is a country located primarily in Western Europe. Its overseas regions and territories include French Guiana in South America, Saint Pierre and Miquelon in the North Atlantic, the French West Indies, and many islands in Oceania and the Indian Ocean, giving it one of the largest discontiguous exclusive economic zones in the world.
The region usually regarded as the Paris Basin is rather smaller than the area formed by the geological structure. The former occupies the centre of the northern half of the country, excluding Eastern France. The latter extends from the hills just south of Calais to Poitiers and from Caen to the brink of the middle Rhine Valley, east of ...
The Massif Central is an old massif, formed during the Variscan orogeny, consisting mostly of granitic and metamorphic rocks.It was powerfully raised and made to look geologically younger in the eastern section by the uplift of the Alps during the Paleogene period and in the southern section by the uplift of the Pyrenees.
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