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The Urbacher Bergrutsch is a remarkable natural monument and geotope located north of Urbach in Baden-Württemberg, Germany. Situated at an elevation of approximately 340 meters on the edge of the Welzheim Forest, this site is renowned for a dramatic landslide that occurred in 2001. It is entirely encompassed by the scenic Schornbach-, Wieslauf-, Urbach- and Bärenbachtal landscape protection area, offering a unique blend of geological history and natural beauty.
Visitors are consistently captivated by the sheer scale of the landslide,…
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Naturpark Schwäbisch-Fränkischer Wald
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2월 3, 2021
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8월 19, 2018
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2월 3, 2018
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256
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4.36km
01:20
160m
160m
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86
등산객
6.44km
01:59
250m
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66
등산객
6.34km
01:50
160m
160m
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정보
고도 340 m
The main trail is the "Bergrutsch-Rundweg" (Landslide Circular Trail). It's approximately 3 kilometers long and is generally considered to be of intermediate difficulty, suitable for hikers and walkers. The path winds through traditional orchards and directly past the landslide site, offering a comprehensive experience.
Yes, parking is available near the trailhead. However, it's advisable to arrive early, especially on weekends or during peak seasons, as parking spaces can fill up quickly.
While the area is primarily accessed by car, you can reach Urbach by public transport. From there, the Urbacher Bergrutsch is located north of the town, above the Urbach outdoor swimming pool. It's recommended to check local bus schedules from Urbach to see if there are stops closer to the Kirchsteig area.
Yes, the "Bergrutsch-Rundweg" is considered family-friendly. The 3-kilometer loop is manageable for children, and the seven information boards along the path provide engaging educational content about the geology, history, and ecology, making it an interesting outing for all ages.
Generally, dogs are welcome on the trails at Urbacher Bergrutsch. However, as it is a nature reserve and geotop, it's important to keep dogs on a leash to protect the local flora and fauna, especially given the unique ecosystem created by the landslide.
While the area is generally accessible, the "Bergrutsch-Rundweg" involves varied terrain, including paths through orchards and potentially uneven sections with gentle ascents and descents. It may not be fully accessible for all wheelchairs or strollers, especially those not designed for off-road use.
While the site is beautiful year-round, spring and autumn offer particularly vibrant scenery. For winter hiking, be prepared for potentially muddy or icy conditions, and check local weather forecasts. To avoid crowds, visiting on weekdays or early in the morning on weekends is recommended, especially during warmer months.
The Urbacher Bergrutsch itself is a natural monument without on-site commercial facilities. However, you can find cafes and restaurants in the nearby municipality of Urbach, which is a short distance away.
The landslide dramatically exposed different geological layers. You can observe the claystones of the Steigerwald Formation, which formed the sliding surface, and the prominent escarpment created by the sandstones of the Hassberge Formation (part of the Middle Keuper). The imposing, arc-shaped cliff face is the most striking geological feature.
The varied topography created by the landslide, including rock faces, scree slopes, and open soil areas, has fostered new habitats. This has led to a diverse range of flora and fauna, including light and warmth-loving plants, various insect species, and rare birds like the Common Redstart. The surrounding traditional high-stemmed orchards also contribute significantly to the area's ecological richness.
The Urbacher Bergrutsch is entirely encompassed by the scenic Schornbach-, Wieslauf-, Urbach- and Bärenbachtal landscape protection area, offering further opportunities for nature exploration. The Bärenbachtal, in particular, is known for its natural beauty and hiking possibilities.
The most significant historical event is the massive landslide that occurred on April 7, 2001, when approximately 70,000 cubic meters of rock and earth slid down the hillside. This event, triggered by heavy rainfall, dramatically reshaped the landscape and led to its designation as a nature reserve and geotop. A similar large landslide also occurred in 1926.