バート・リップシュプリンゲのバイクパーク・トップ20

Currently free of trees again, challenging but beautiful!

It used to be totally beautiful, but today it is all the more a sign of the forest dying. But even after some time now for what all comes back by itself.

"The “Große Egge” ravine is a section of old road carved in the form of a ravine into the existing Cenomanian limestone at the wooded “Große Egge” pass in the southeastern Teutoburg Forest. It is located in the municipality of Horn-Bad Meinberg (Holzhausen-Externsteine district) in North Rhine-Westphalia and is located about 1.2 km west-southwest of the Externsteine and almost 2.3 km east of the Gauseköte. The path investigation did not produce any find that could be dated with certainty. Around 120 m northeast of the cultural monument rises the Wiembecke, which forms a pond at the Externsteine is pent up." https://de.wikipedia.org/wiki/Hohlweg_Gro%C3%9Fe_Egge

Silberbachtal largely impassable due to fallen trees! Possibly. You could avoid such passages on hiking trails. But it is very tedious and could end up in a dead end. Driving - even with the MTB - on the paths almost impossible.

Lake Lippe is a local recreation area where there are a variety of water sports and leisure opportunities such as sailing, surfing, pedal boating and fishing. There is a small beach at the kiosk on the north bank. There is also a barbecue area, a children's playground, sunbathing areas, a mountain bike course, a skate park and a mini golf course. Water skiing opportunities can be found in the adjacent Nesthauser See. Lake Lippe is completely surrounded by mostly asphalted paths on which cycling and running are possible all year round. If the snow conditions are suitable, the Lippesee circuit is also suitable as a cross-country ski trail. Water sports are possible on Lake Lippe. There are two sailing clubs on the lake, the Paderborn Yacht Club e.V. and the Segler-Verein Paderborn e.V., as well as a commercial sailing school. In addition to its use as a local recreation area, the lake also produces high-quality gravel, which was deposited in layers up to 20 m thick during the last ice age at the transition from the Westphalian Bay to the Paderborn plateau, especially in the area of Lake Lippe. These river deposits come mainly from the Alme and the Beke, which flow into the Lippe above the Lippesee.

Today only for hotel guests. The host is fed up. Too bad.

Keeping a long story short. Narrow trail that is easy to miss. Fun for every MTBr.

Extremely dangerous section on this descent