The Rhinluch is a fen landscape in the German state of Brandenburg, bisected by the river Rhin to which it owes its name. This wetland region lies north of Fehrbellin in the county of Ostprignitz-Ruppin. The upper Rhinluch covers an area of about . The suffix luch, from the west-Slavic "lug", meaning marshy ground, is used to describe several low-lying wet areas in the state of Brandenburg. In these areas, prior to the advent of modern drainage systems, water remained largely stagnant rather than flowing.
The Rhinluch was formed during the last ice age and its post-glacial period. About 16,000 years ago, the Eberswald urstromtal was formed by the meltwaters of the glacial ice sheet as they drained away to the sea. Later, this broad river valley dried up as the ice sheet retreated during the late ice age. In the land that makes up the present-day Rhinluch, lakes initially formed in individual places, especially where there were dead ice kettle holes. Over the course of time, these became bogs through the natural silting up process. In addition, during the post-glacial period, there was a widespread formation of swamps (Versumpfungsmooren) on the sands of the urstromtal. Not until man appeared, however, did these moors become pastures and meadows as a result of land improvement measures. The easternmost outlier of the Rhinluch is the Kremmener Luch.
The Rhinluch contains suitable habitat for the near threatened European pond turtle, whose population is stable in Brandenburg due to intensive conservation management of the Rhinluch and similar wetlands. The area is also known for its archaelogical importance, as several well-preserved Mesolithic sites have been unearthed here.
The Brandenburg poet, Theodor Fontane, described the Rhinluch thus in his Wanderungen durch die Mark Brandenburg:
References
External links
Society for the Preservation of the Upper Rhinluch (Landschaftsförderverein Oberes Rhinluch)