The Flims rockslide happened about 10,000 years ago (8000 BC) in eastern Switzerland. It is the biggest known landslide incident in the Alps, and the biggest worldwide whose effects are still visible, moving some 12 km3 (2.9 cu mi) of rock, about 300 times that of the historic Swiss Goldau landslide. The town of Flims can be found at the line where the slip surface disappears under the debris. North of Flims the rock face of Flimserstein stands 350 metres (1,148 ft) high whereas more westerly the slide surface is clearly visible. South of Flims is a huge hilly debris area that has been forest ever since, as this area is not suitable for farming, firstly for its shape and, even more for its lack of water. The river Rhine crosses this debris in a gorge called Ruinaulta. The Rhine still runs
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| - Flimser Bergsturz (de)
- Flims rockslide (en)
- 플림스 암반산사태 (ko)
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| - The Flims rockslide happened about 10,000 years ago (8000 BC) in eastern Switzerland. It is the biggest known landslide incident in the Alps, and the biggest worldwide whose effects are still visible, moving some 12 km3 (2.9 cu mi) of rock, about 300 times that of the historic Swiss Goldau landslide. The town of Flims can be found at the line where the slip surface disappears under the debris. North of Flims the rock face of Flimserstein stands 350 metres (1,148 ft) high whereas more westerly the slide surface is clearly visible. South of Flims is a huge hilly debris area that has been forest ever since, as this area is not suitable for farming, firstly for its shape and, even more for its lack of water. The river Rhine crosses this debris in a gorge called Ruinaulta. The Rhine still runs (en)
- Der Flimser Bergsturz fand vor 9480 bis 9430 Jahren (kalibriert) statt. Er ist mit einem Volumen zwischen 9 km³ und 12 km³ das grösste alpine Bergsturzereignis (rund 300 mal grösser als der Bergsturz von Goldau und rund 1200 mal grösser als der Bergsturz von Elm) und weltweit einer der grössten derzeit bekannten Bergstürze überhaupt. (Zum Vergleich: Das Wasservolumen des Vierwaldstättersees beträgt 11,9 km³) Auf dem Übergang der Gleitfläche im Norden zur Schuttmasse im Süden liegt der Ferienort Flims. Nördlich von Flims ragen Felswände bis 350 Meter hoch und im Süden liegt eine dicht bewaldete, unübersichtliche Hügellandschaft mit Seen und einer wilden Schlucht, der Ruinaulta. Der Bergsturz ist für Reisende durch Wald verborgen; weil der Schuttkegel landwirtschaftlich uninteressant ist, bl (de)
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| - Der Flimser Bergsturz fand vor 9480 bis 9430 Jahren (kalibriert) statt. Er ist mit einem Volumen zwischen 9 km³ und 12 km³ das grösste alpine Bergsturzereignis (rund 300 mal grösser als der Bergsturz von Goldau und rund 1200 mal grösser als der Bergsturz von Elm) und weltweit einer der grössten derzeit bekannten Bergstürze überhaupt. (Zum Vergleich: Das Wasservolumen des Vierwaldstättersees beträgt 11,9 km³) Auf dem Übergang der Gleitfläche im Norden zur Schuttmasse im Süden liegt der Ferienort Flims. Nördlich von Flims ragen Felswände bis 350 Meter hoch und im Süden liegt eine dicht bewaldete, unübersichtliche Hügellandschaft mit Seen und einer wilden Schlucht, der Ruinaulta. Der Bergsturz ist für Reisende durch Wald verborgen; weil der Schuttkegel landwirtschaftlich uninteressant ist, blieb er ein ausgedehntes Waldgebiet. Der Wald ist für das Vorderrheintal Namensgeber: Das romanische Surselva bedeutet „ob dem Wald“. (de)
- The Flims rockslide happened about 10,000 years ago (8000 BC) in eastern Switzerland. It is the biggest known landslide incident in the Alps, and the biggest worldwide whose effects are still visible, moving some 12 km3 (2.9 cu mi) of rock, about 300 times that of the historic Swiss Goldau landslide. The town of Flims can be found at the line where the slip surface disappears under the debris. North of Flims the rock face of Flimserstein stands 350 metres (1,148 ft) high whereas more westerly the slide surface is clearly visible. South of Flims is a huge hilly debris area that has been forest ever since, as this area is not suitable for farming, firstly for its shape and, even more for its lack of water. The river Rhine crosses this debris in a gorge called Ruinaulta. The Rhine still runs in debris, which shows that it has not yet reached its level as before the incident. The highest hill in the debris area is almost 200 metres (656 ft) higher than Flims at the end of the sliding surface. (en)
- 플림스 암반 산사태(Flims rockslide)는 스위스 동부에서 약 10,000년 전(기원전 8000년) 발생했다. 그것은 알프스 산맥에서 알려진 가장 큰 산사태이며, 그 영향이 여전히 가시적인 세계 최대 규모로, 역사적인 스위스 골다우 산사태의 약 300배에 달하는 약 12k㎥의 암석을 움직였다. 플림스의 마을은 산사태로 드러난 표면이 파편 아래에서 사라지는 라인강에서 찾을 수 있다. 플림스 북쪽 플림저슈타인의 암벽은 높이가 350m인 반면 더 서쪽으로 갈수록 미끄럼 표면이 뚜렷하게 보인다. 플림스의 남쪽은 숲이었던 거대한 구릉지 잔해 지역이다. 그 이후로 이 지역은 농사를 짓기에 적합하지 않기 때문에 첫째, 그 모양과 물 부족 때문에 더욱 그렇다. 라인강은 루이놀타라고 불리는 협곡에서 이 잔해물을 건넌다. 라인강은 여전히 잔해 속에서 흘러내리고 있어 아직 사고 전과 같은 수준에 도달하지 못했다는 것을 알 수 있다. 잔해 지역에서 가장 높은 언덕은 산사태 표면의 끝에서 플림스보다 거의 200m 높다. (ko)
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