마지막 업데이트: 3월 26, 2026
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마옌-코블렌츠 주변 인기 장소
Moselle 사이클로 탐방로 — Vosges에서 Rhine까지 18 구간
트리어에서 코블렌츠까지 — 모셀크로스
모젤스타이그 트레일 - 맑은 모젤 계곡의 24 구간
라인슈타이크 트레일의 21개 구간 - 라인 강을 따라
라인 성 트레일 – 순수한 라인 낭만주의의 13단계
Dream Trails in the Rhine-Mosel-Eifel Region – Small Trails, Great Nature
Stunningly beautiful – hiking on the RheinBurgenWeg
Traumpfade – dreamy, varied hiking trails in Rhein-Mosel-Eifel-Land
Moselsteig Partner Trails – nature, culture and views
Mosel Cycle Path – in 10 stages from Perl to Koblenz
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.
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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/
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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
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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
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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.
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