マイエンコブレンツの湖・トップ20

The Luisenplatz Hut is picturesquely situated above Mayen, nestled in the city forest and the gentle hills of the Eifel region. It is considered one of the most beautiful viewpoints in the area and invites hikers to rest and enjoy the breathtaking panoramic views. On the popular "Förstersteig" (Forester's Trail) hiking route, this spot is described as a highlight of the tour – offering a "stunning panoramic view over Mayen, the Maifeld region, and all the way to the Rhine." Just a few steps from the hut is a trigonometric survey point, which underscores the unique topographical location of the site. This prominent point was once used for geodetic measurements.

The Eiterbachweiher pond is located near Kürrenberg (a district of Mayen) in the Vorderwald or Vorderer Stadtwald of Mayen, nestled in the so-called Eiterbach valley.

Mofettes at Lake Laach demonstrate: The Laacher See volcano, Europe's youngest, didn't go extinct 13,000 years ago; it's just dormant. That's what volcanologists say. And indeed, on the eastern shore of the lake, it's bubbling like a glass of mineral water. Mass amounts of CO2 bubbles rise here, and there's a faint smell of sulfur. Source: https://www.meineeifel.de/mofetten-am-laacher-see/

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.

and a swim 😜

😯😮It's very interesting to see the mofettes - gas bubbles from inside the lake🫧🫧🫧🫧. 🌋Welcome to the active volcanic Eifel 🌋.

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.