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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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Adams Synchronological Chart or Map of History, originally published as Chronological Chart of Ancient, Modern and Biblical History is a wallchart which graphically depicts a Biblical genealogy alongside a timeline composed of historic sources from the history of humanity from 4004 BC to modern times.
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The three partitions of Luxembourg reduced Luxembourg's area substantially, to the advantage of the three surrounding countries. There were three Partitions of Luxembourg between 1659 and 1839. Together, the three partitions reduced the territory of the Duchy of Luxembourg from 10,700 km 2 (4,100 sq mi) to the present-day area of 2,586 km 2 ...
This is a timeline of Luxembourgish history.Each article deals with events in Luxembourg in a given year.. 1800s: 1800 - 1801 - 1802 - 1803 - 1804 - 1805 - 1806 ...
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.