シャルケンメーレナーマールのおすすめランニングルート

「鳥は歌い、花は咲き, 森も野原も再び緑に。 ああ、それなら行こう、さまよおう この場所からあの場所へ 広大な緑の世界を！」 (Hoffmann von Fallersleben)

シャルケンメーレンとそのマールを望む非常に美しい景色

What a great tunnel, over 500m Video on Instagram "biketime1979"

A well-maintained cycle path runs around the maar, and beautiful views are guaranteed.

A very well-maintained tunnel. A highlight for the kids.

Very good surface, pleasantly shady in summer

"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

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 meets 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 Schalkenmehren 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