Mountain Biking Highlight
The Cösitzer Teich was created around 1936 by the sinking of a mine area within the Fuhneaue. Fuhne determined the hydrological regime of the pond.
Strong nutrient inputs led to strong eutrophication phenomena in the water, which is only about 1 m deep (nutrient overload combined with excessive plant growth).
(Source: State administration office - lvwa.sachsen-anhalt.de/das-lvwa/landwirtschaft-umwelt/naturschutz-landschaftspflege-bildung-fuer-nachhaltige-entwicklung/naturschutzgebiete-in-sachsen-anhalt/coesitzer-teich)
December 23, 2019
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