질렌펠트 최고의 MTB 라이딩 경로

자전거 타기 아주 좋은 곳

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.

Beautiful circular path in the shade suitable for wheelchairs/strollers

Recorded while driving in a great tunnel

The historic market square in Wittlich is a small gem of art history. Opposite the Old Town Hall stands today's Hotel Well. The magnificent Renaissance building was formerly known as "Zum Wolf." Next to it is a simple 18th-century Baroque building, the former Neuerburg House. The Baroque building on the long side was built as a post office in 1753 by the Fier family. Text / Source: Mosellandtouristik GmbH, Kordelweg 1, 54470 Bernkastel-Kues https://www.visitmosel.de/stadt-kultur/poi/historischer-marktplatz-wittlich

Main inspection of the Pleiner Viaduct on the Maare-Mosel Cycle Route Plein Viaduct, length 98 meters, height above valley 31 meters Unkenstein Tunnel, length 140 meters Grünewald Tunnel, length 124 meters The Pleiner Viaduct consists of a five-span arch bridge. The structure is located on the Hasborn - Wittlich section of the Maare-Mosel Cycle Route. The viaduct, first built in 1910, demolished in 1945, and rebuilt in 1953, is approximately 98 meters long, approximately 31 meters high, and 4.65 meters wide between the railings. It was built on site using reinforced concrete, and the piers, abutments, and side elevations were clad in sandstone. However, the structural concrete is exposed in the arch undersides. After the railway line was closed by Deutsche Bahn in 1984, the tracks were dismantled in 1989. Before the structure was reopened as part of the Maare-Mosel cycle path in 1998, it was completely renovated. Text / Source: Rogmann Ingenieure GmbH, Einöder Straße 6, 66424 Homburg https://www.rogmann-ingenieure.de/referenzen/pleiner-viadukt-plein.html#:~:text=The%201910%20first%20built%2C%20in%201945%20blasted%20and,Width%20between%20the%20railings%20of%204%2C65%20m%20on.

Pleiner Tunnel - Hasborn–Wittlich Directly after the former Plein train station, approximately 5 km beyond Hasborn, the cycle path leads through the 585-meter-long Pleiner Tunnel. It then continues downhill through deciduous and mixed forests to Wittlich. From the rather rugged Volcanic Eifel, the cycle path descends into the Wittlich Valley. The route passes vineyards and leads into the town of Wittlich. Text / Source: wikipedia.org/wiki/Maare-Mosel https://de.wikipedia.org/wiki/Maare-Mosel-Radweg#:~:text=Direkt%20nach%20dem%20ehemaligen%20Bahnhof%20von%20Plein%2C%20ca.,f%C3%BChrt%20der%20Radweg%20hinab%20in%20das%20Wittlicher%20Tal.

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