The Upper Rhine Plain, also called the Rhine Rift Valley or Upper Rhine Graben, is a major rift about 350 kilometers long and 50 kilometers wide on average, running from Basel in the south to Frankfurt and Wiesbaden in the north, with its southern section straddling the France-Germany border. It forms part of the European Cenozoic Rift System across Central Europe, having formed during the Oligocene in response to the rise of the Alps to the south, and it remains active today as a downfaulted trough through which the Rhine flows. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/
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Wikidata P31 (Q193071) mapped to discipline Geomorphology via earth5 extended reviewed judgment map; source citation is this entity's own cited Wikidata item.
Source Wikidata: Upper Rhine Graben
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Source Wikidata: Upper Rhine Graben
Also in Geography Atlas: where this subject is found.
Source Wikidata: Upper Rhine Graben
Also in Geography Atlas: where this subject is found.
Source Wikidata: Upper Rhine Graben
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Upper Rhine Plain (Wikipedia)
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The Upper Rhine Plain, Rhine Rift Valley or Upper Rhine Graben (German: Oberrheinische Tiefebene, Oberrheinisches Tiefland or Oberrheingraben, French: Vallée du Rhin) is a major rift, about 350-kilometre-long (220 mi) and on average 50-kilometre-wide (31 mi), between Basel in the south and the cities of...
Caused By: Rifting, Lead paragraph
The Upper Rhine Plain, Rhine Rift Valley or Upper Rhine Graben (German: Oberrheinische Tiefebene, Oberrheinisches Tiefland or Oberrheingraben, French: Vallée du Rhin) is a major rift, about 350-kilometre-long (220 mi) and on average 50-kilometre-wide (31 mi), between Basel in the south and the citie
View the SourceWikidata: Upper Rhine Graben
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