ブランクのおすすめランニングルート

ターベカー・ムーアは、最後の氷河期以降に融雪の溝の中に形成された、より大きな泥炭地の残骸です。周囲の泥炭地は19世紀と20世紀に排水され、ほぼ完全に牧草地になりました。ターベカー・ムーアは、1951年から1990年まで、鉱物の基盤まで部分的に工業的に採掘されました。泥炭の採掘は、高層湿原の植生を完全に破壊しました。

湿原は静かで自然のままの場所です。 静かに滞在することができますし、そうするべきです。

The field edge path south of the lake offers occasional views of the lake and a particularly beautiful bathing area, although this is in the shade of two linden trees.

The small, often dried-up stream without a name continues along the Treene.

Here at the bathing area with shallow sandy entry, there is an idyllic bench under a huge double lime tree.

The Muggesfelder Moor borders the Tarbeker Moor to the west. Both moors were used for peat extraction. Cranes now live in both rewetted moors, some of them all year round.

The moor is wonderful, but the view from this point is not very impressive: You have a limited all-round view and in the evening the sun is not in a good position.

Here, as you walk around the Muggesfelder See, you can finally get close to the lake and catch a beautiful view towards Muggesfeld. The path continues between the lake and the meadow until you reach a small forest...