ミュンクのおすすめウォーキング＆ハイキングルート

Boosの溶岩爆弾は、アイフェルにおける過去の火山活動の印象的な地質学的証拠であり、Booser Doppelmaar近くの火山露頭にあります。

蜂蜜は本当におすすめです👍🏽😊😋😋🍯

この蜂蜜は本当におすすめです👍🏽

ああ、何と言えばいいのか、ただひつじのショーン🤣😂🐑🐑🐑📸📸🥳見なければならない☝🏽

Especially pleasant when it's very hot🥵

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.

Tower closed. Danger of collapse

This view of the Booser Maar with the Booser Weiher is simply picturesque.