브뤼크탈 최고의 워킹 & 하이킹 경로

클로스터탈과 카루셀 사이의 옛 가파른 구간은 트랙이 더 거칠고 무자비했던 옛 뉘르부르크링 시절을 떠올리게 합니다. 모터스포츠 신화의 한 조각입니다! 🏎️🔥 오늘날 이 구간은 수년에 걸쳐 여러 차례 재건축되고 현대화되었기 때문에 원래의 형태로 더 이상 주행할 수 없습니다. 특히 안전상의 이유로 말입니다. 🔧🛑

Wippermann 구간은 기술적으로 흥미로울 뿐만 아니라, "Grüne Hölle"를 가까이서 경험하고 싶은 관객과 관광객들에게 인기 있는 장소입니다. 🌳👀

Great area for e-bike riding was fun

Two Silver Arrows The legendary one and mine 😁

Especially pleasant when it's very hot🥵

The Klostertal curve is the branch off to the steep section.

The steep section, with gradients of up to 27%, was originally built for vehicle testing. Today, it is no longer used.

The Boos Double Maar consists of two silted-up maars, which today appear as shallow depressions in the terrain. They are located within the municipality of Boos. The two maars formed between 10,150 and 14,160 years ago and belong to the Quaternary volcanic field of the Volcanic Eifel. The two maars form large, circular basins surrounded by tuff embankments. They lie on a west-southwest-east-northeast trend, thus following the Variscan strike of the subsurface. The west-southwest maar has a diameter of approximately 700 m and a depth of between 30 and 60 m; the east-northeast maar is between 650 and 700 m and a depth of between 50 and 87 m. Both depressions are very humid, so there are still areas that have a permanent water surface. The waters were formerly used as fish ponds, but later silted up and served as meadows and fields. Today, there is once again a fish pond in the west-southwestern part of the maar, the Booser Weiher. In the vicinity of the maars, there are tuff pits where the volcanic tuff formed during the eruption of the maars was mined. Very beautiful nature.