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오데라스

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마지막 업데이트: 9월 29, 2026

11

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#1.

Alflen에서 출발하는 울메너 마르 – 그루베 베르크크로네 광산 터널 순환 코스

37.5km

01:47

460m

460m

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보통 도로 자전거 타기. 좋은 체력 필요. 지면 대부분이 잘 포장되어 있고 라이딩하기 쉬움.

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어려운 도로 자전거 타기. 우수한 체력 필요. 투어 중 라이딩하기 어려운 비포장 구간이 있을 수 있음.

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보통 도로 자전거 타기. 좋은 체력 필요. 투어 중 라이딩하기 어려운 비포장 구간이 있을 수 있음.

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Manja
7월 16, 2026, View of Jungferweiher

전망대까지 올라가는 것은 보람이 없습니다. 모든 것이 우거져 있습니다. 실제로 아무것도 보이지 않습니다. 아마 봄과 가을에는 잎이 아직 나무에 없을 때일 것입니다. 그때는 무언가를 볼 수도 있지만 그렇지 않으면 보람이 없습니다.

번역: Google•

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이렇게 폐차된 불리가 있다니, 정말 슬픈 광경이네요..

번역: Google•

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From 13:00 o'clock many people are out and about when the sun ☀️ shines

번역: Google•

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The Ulmen Maar lies 420 meters above sea level today, covers an area of 5.5 hectares, and is 36 meters deep. The bubbles at the maar's edge demonstrate that volcanism is still active. They bear witness to a turbulent past—but rest assured, there's no eruption in sight! A wall of various rocks and ash, up to 20 meters thick, surrounds the cone. For those interested, these testimonies to this explosive past are beautifully displayed in St. Matthias Church. This unique wall, with its different colored layers and rounded inclusions, is worth seeing for more than just geologists. The slopes of the maar basin are covered with a beautiful forest, which can be explored on a circular walk. A detour to the medieval castle ruins, from which the Crusaders once launched their campaigns, is recommended. The view from the crater rim over the maar and the Eifel beyond will take your breath away. Whether after a sweaty hike or a long drive, the blue of the Ulmer Eifel lake is all too tempting in summer. However, bathing in the maar is prohibited because it is designated as a nature and water protection area.

번역: Google•

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"Old Station" Schalkenmehren Passenger service between Daun and Wittlich was discontinued on November 1, 1981. Schalkenmehren. Approaching the Old Station in Schalkenmehren on the former railway line, today's Maare-Mosel cycle path, and seeing the station building, it's hard to believe that it was opened as a fourth-class railway station exactly 100 years ago. But how did it all begin 100 years ago? Surveying for the Daun-Wittlich railway line began as early as 1897. General preparatory work for the single-track line began in 1907. But it would take some time before the Daun-Schalkenmehren-Gillenfeld section opened on December 1, 1909, with the line running over the 28-meter-high Daun viaduct and through the 560-meter-long Schalkenmehren railway tunnel, "Großes Schlitzohr" (Great Sly Fox). The extension from Gillenfeld to Manderscheid to Pantenburg was completed on May 1, 1910, and the extension from Manderscheid-Pantenburg to Wittlich, signifying the completion of the entire line, was completed on July 1, 1910. The completion of the Daun-Wittlich railway line brought rapid development to the village of Schalkenmehren. In the first year of the line's existence (1910), 18,968 tickets were sold in Schalkenmehren, followed by 25,057 in 1913, 27,969 in 1919, and even 30,279 in 1922. In addition, Schalkenmehren station was designed for general cargo traffic and the receipt and dispatch of wagonloads. Text / Source: www.volksfreund.de/ https://www.volksfreund.de/region/vulkaneifel/ein-schmuckstueck-fuer-nostalgiker_aid-5712448

번역: Google•

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Paul
5월 12, 2025, Maarsattel

Weinfelder Maar - Impressive Evidence of Explosive Geological History The Weinfelder Maar – also known as Totenmaar – is one of the three so-called Daun Maars. It is located about 2 kilometers from our district town of Daun, near the municipality of Schalkenmehren, between the Gemünden and Schalkenmehren Maars. It has a diameter of approximately 525 meters and a depth of 51 meters, making it the deepest of the three Daun Maars. It is the youngest and, at 487 meters above sea level, the highest of the three closely adjacent maars, which formed between 20,000 and 30,000 years ago. Text / Source: Natur- und Geopark Vulkaneifel GmbH, Mainzer Str. 25, Daun https://www.geopark-vulkaneifel.de/eifel/landschaft/maare-und-kraterseen/weinfelder-maar.html

번역: Google•

12

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Paul
5월 12, 2025, Maarsattel

Weinfelder Maar The Weinfelder Maar, formed by volcanic activity around 20,000 to 30,000 years ago, is the highest of the three Daun Maars at 487 meters above sea level. The lake is 51 meters deep and has a diameter of 396 to 429 meters. An almost melancholic atmosphere surrounds the maar. Many legends surround the tranquil Eifel eye. A castle is said to have once stood on the site of the crater, where a count lived with his wife and only child. After returning home from a hunt, the castle had sunk as punishment for the woman's nastiness, and he found only a lake where a cradle miraculously floated his child safely to the shore. If you look at the dark surface of the water long enough, it is said that you can make out the outline of the castle. The German landscape painter Fritz von Wille was so fascinated by the Weinfelder Maar that he repeatedly immortalized it in his paintings. Among his favorite motifs was the small chapel on the north bank, dedicated to Saint Martin. It was once the parish church of the village of Weinfeld, which was ravaged by the plague in the 16th century. Anyone who rings the bells inside by pulling the ropes can make a wish. To this day, the associated cemetery is maintained and used by the local community of Schalkenmehren. This is also where its second name, Totenmaar, comes from. Donkeys and goats have been introduced to the Weinfelder Maar to regulate vegetation. The maar's unique flora and fauna are protected. Swimming and other water sports are prohibited in the Weinfelder Maar, but a nearly two-kilometer-long path makes it a wonderful place to explore on foot. Parking: Guests can park along the L64 either in the parking lot at the Weinfelder Maar or on the Maarsattel between the Weinfelder Maar and the Schalkenmehrener Maar. Text / Source: GesundLand Vulkaneifel GmbH, Leopoldstr. 9 A, 54550 Daun https://www.eifel.info/a-weinfelder-maar

번역: Google•

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The Daun Maars - 10,000-Year-Old Volcanic Lakes The Daun Maars were formed around 10,000 years ago from volcanic steam explosions. Hot lava rises from the Earth's interior and encounters water, which suddenly evaporates. This blasts away entire mountain peaks. What remains is a deep crater that fills with water over the years and a wall of boulders surrounding the lake. The Daun Maars include the Gemünden Maar, the Weinfelder Maar, and the Schalkenmehrener Doppelmaar. One crater of the Schalkenmehrener Maar has silted up over the millennia. The area is a nature reserve and a refuge for waterfowl and rare dragonfly species. Text / Source: deutschland-outdoor.der https://deutschland-outdoor.de/eifel/dauner-maare

번역: Google•

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