マイエンコブレンツの湖・トップ20

During the summer months, suitable photo spots are scarce, as the lake is only visible from the bike path through the trees. But there are these little hotspots.

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.

Lake Laach in the eastern Volcanic Eifel, near Maria Laach Abbey in the municipality of Glees, is the largest lake in Rhineland-Palatinate. It formed in the caldera of the Laach volcano after its last eruption, which was initially dated to 10,930 BC. Following radiocarbon dating of buried tree trunks carried out in 2021, the date of this eruption was corrected to 11,056 BC; doubts about the accuracy of the new dating have not yet been confirmed. The outgassing observed as mofettes in the southeastern part of the lake is a sign of ongoing volcanism. Source: Wikipedia

and a swim 😜

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

Simply beautiful here at the lake

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.