호네라스‬에서 가장 멋진 ‪20‬개의 천연기념물

고도 미터 연습에 좋은 투어와 거래

The park is part of popular hiking trails such as the Bergheidenweg and is maintained by the "Wacholderwacht Osteifel" initiative. Visitors can expect easy-to-walk paths, expansive views as far as the Hohe Acht, and an immersive nature experience – especially charming during the heather bloom.

Impressive views of Schuld and the Eifel mountains. Anyone who climbs here and continues along the Ahrsteig trail toward Schuld should be sure-footed.

Demanding passage - surefootedness required!

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.

Beautiful descending path, worth every inch to explore

The Legend the legend, in which the devil built the castle here, high in the sky, in defiance of God, based on this observation of the rocks, which had already been made in the past by people with a natural acumen. (...) This time, as always, it did not work out well for the devil: his half-finished castle was shattered by one blow of the hand of God, and the rock really gives the impression of a Cyclopean castle ruin.

The largest contiguous quartzite block in Europe, Teufelsley, is located four kilometres from Dümpelfeld.