ゲレンベルクの湖・トップ20

beautiful small reservoir, ideal for a short walk

especially when the sun rays penetrate through the treetops a great sight

The history of the Volcanic Eifel can be explored at the Booser Doppelmaar. The Booser Doppelmaar consists of two silted-up maars, which today appear as flat hollows in the terrain. The two maars were formed between 10,150 and 14,160 years ago. Viewed from above, the two maars are circular basins. The west-southwest maar has a diameter of around 700 m and is between 30 and 60 m deep, the east-northeast maar is between 650 and 700 m large and has a depth of 50 to 87 m. The two hollows are very wet, so there are still places that have a permanent water surface. The water areas were previously used as fish ponds, but later silted up and served as meadows and fields. Today there is again a fish pond in the west-southwestern maar, the Booser Weiher, see also https://de.wikipedia.org/wiki/Booser_Doppelmaar

The Booser Doppelmaartour is an Eifel dream trail. It is important that you look in vain for water here, because the two maars are so-called dry maars.

Here you can spend your holidays on the farm. http://website.meisenthaler-muehle.de

From a wooden bridge there is a wonderful view of the swampy foothills of the rainwater-filled Booser Maar, which is located in the Hohe Acht mountain region and approx. 8 km south of the Hohe Acht. The maar lies in a circular tuff basin, whose tuff walls are covered with swampy meadows and the edge of the bank is overgrown with reeds. Galloways graze in the dry, higher meadows.

A circular route leads around the small reservoir. For children there are climbing frames and other play facilities.

At this point you come across the swampy, swampy foothills of the Booster Maare.