Schurre
Encyclopedia
The Schurre is a stone run
Stone run
A stone run is a conspicuous rock landform, result of the erosion of particular rock varieties caused by myriad freezing-thawing cycles taking place in periglacial conditions during the last Ice Age.The actual formation of stone runs involved no less than five processes: weathering, solifluction,...

 in the Bode Gorge
Bode Gorge
The Bode Gorge is a long, ravine that forms part of the Bode valley between Treseburg and Thale in the Harz Mountains of central Germany. The German term, Bodetal , is also used in a wider sense to refer to the valleys of the Warme and Kalte Bode rivers that feed the River Bode.At the Bode Gorge,...

 in the Lower Harz
Harz
The Harz is the highest mountain range in northern Germany and its rugged terrain extends across parts of Lower Saxony, Saxony-Anhalt and Thuringia. The name Harz derives from the Middle High German word Hardt or Hart , latinized as Hercynia. The legendary Brocken is the highest summit in the Harz...

 near Thale
Thale
Thale is a town in the Harz district in Saxony-Anhalt in central Germany.-Geography:It is situated on the river Bode, approximately 8 km west of Quedlinburg. It is the terminus of the Magdeburg–Thale railway.- History :...

 in Saxony-Anhalt
Saxony-Anhalt
Saxony-Anhalt is a landlocked state of Germany. Its capital is Magdeburg and it is surrounded by the German states of Lower Saxony, Brandenburg, Saxony, and Thuringia.Saxony-Anhalt covers an area of...

, Germany. The stone run is slowly slipping downhill, the sliding of its boulders being audible especially during periods of heavy rain.

Its name has been given to a much-frequented trail, blazed in 1864 between the Bode Gorge and the legendary Rosstrappe site. In 18 hairpin bends the Schurre wends its way up the steep stone run. The trail has been extensively developed and is cobbled in places. Several trees planted along the route, with its extreme climatic conditions, have survived. Negotiating this route uphill from the valley requires walkers to be fit due to its steep gradient and the requirement to climb around 200 metres in height.
In May 2010 there was a rockslide that led to the path being closed for several months. The path was also closed in summer 2011 due to another major rockslide.
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