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Staufen, Germany
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Staufen im Breisgau is a German town in the Breisgau-Hochschwarzwald district of Baden-Württemberg. It has a population of approximately 7700. Additional information may be found (in German) on the Staufen im Breisgau article in the German language Wikipedia. Geography
Staufen lies at the foot of the Black Forest at the exit from the Münstertal.

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Encyclopedia
Staufen im Breisgau is a German town in the Breisgau-Hochschwarzwald district of Baden-Württemberg. It has a population of approximately 7700. Additional information may be found (in German) on the Staufen im Breisgau article in the German language Wikipedia.
General The city of Staufen im Breisgau lies in the Land district of Breisgau-Hochschwarzwald (Breisgau-Upper Black Forest) in the German State of Baden-Württemberg. The City of Staufen has approximately 7700 inhabitants and forms, together with the community of Münstertal, a community administrative unit.
Geography
Staufen lies at the foot of the Black Forest at the exit from the Münstertal. The Black Forest valley of Neumagen goes here directly over into the Rhine plain. The piedmont of the Black Forest is less distinct. North of the valley exit, the steeply rising Schlossberg dominates; to the southwest begins the hilly landscape of the Markgräflerland. Staufen lies on the border between two natural and economic areas: the Rhine plain up to the piedmont with its cultivation of grain, winegrapes and vegetables; and the Black Forest, with its cattle and forestries, and, in an earlier time, mining.
Geothermal drilling controversy Since 2008, the center of the city has been reported to have been rising some 12 cm so far, after initially sinking a few millimeters. This has been causing considerable damage to buildings in the city center, including the historical town hall. One hypothesis for the cause of this geological change is a drilling operation conducted in the fall of 2007 to provide geothermal heating to the city hall. The drilling perforated a gypsum layer and caused high-pressure groundwater to come into contact with the gypsum, which then began to expand. Currently no end to the rising process is in sight.
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