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The Luxembourg Sandstone (French: Grès de Luxembourg) is a geologic formation in Luxembourg. It exists along the eastern margin of the Paris Basin. Sandstone units continuous with the Luxembourg Sandstone also occur in France. It is Early Jurassic in age. It predominantly outcrops in a belt extending through south-central Luxembourg.
Lower Jurassic sandstone of the Grès de Luxembourg Formation near Waldhof. The geology of Luxembourg is divided into two geologic regions: Rheinisches Schiefergeblige in the north, extending into the Ardennes region in Belgium, and the Oesling (also known as Islek) Zone to the north of Ettelbruck.
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• Grand Duchy of Luxembourg: 1815– Dutch rule: 1815–30 • Reign of Guillaume I: 1815-40 • Belgian Revolution: 1830–31: Personal union: 1839–90 • Treaty of London: 1839 • Reign of Guillaume II: 1840–49 • Reign of Guillaume III: 1849-90 • Luxembourg Crisis: 1867: Full independence: 1890-
City of Luxembourg: its Old Quarters and Fortifications: Luxembourg City: 1994 699; iv (cultural) The city developed around a fortress built in the 10th century on an almost inaccessible rock. Due to its strategic location, it passed among great European powers several times, with the fortifications being constantly upgraded.
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