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A landslide in which the sliding surface is located within the soil mantle or weathered bedrock (typically to a depth from few decimeters to some meters) is called a shallow landslide. Debris slides and debris flows are usually shallow. Shallow landslides can often happen in areas that have slopes with high permeable soils on top of low ...
A large landslide entered Sullorsuaq Strait, generating a megatsunami which struck Alluttoq Island, where it had a run-up height of 45 to 70 metres (148 to 230 ft). [15] ~2800 BCE Zion Canyon, Utah, US: 0.286 km 3: Landslide created the currently level floor of Zion Canyon inside Zion National Park. [21] ~1920 BCE Jishi Gorge, Qinghai Province ...
The Tuve landslide was a large landslide in Tuve, Gothenburg, Sweden on 30 November 1977. Some 67 houses were destroyed, killing 9, injuring about 60 and making around 600 people homeless. [1] The slide began at 16.05 and lasted 5–6 minutes. [1] The slide affected 270 000 square meters (27 hectares). [2]
This Swedish photograph is in the public domain in Sweden because one of the following applies: The photograph does not reach the Swedish threshold of originality (common for snapshots and journalistic photos) and was created before 1 January 1974 (SFS 1960:729, § 49a).
The 300-by-700-metre (980 ft × 2,300 ft) quick clay landslide wrecked several houses and killed 10 people. [15] [14] On 23 September 2023, near the town of Stenungsund, Sweden, an area of c. 15 hectares (37 acres) was affected by a quick clay landslide, which among other things damaged the E6 motorway between Gothenburg and Oslo. [16]
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The difference between these two concepts is subtle but important. The landslide causes are the reasons that a landslide occurred in that location and at that time and may be considered to be factors that made the slope vulnerable to failure, that predispose the slope to becoming unstable. The trigger is the single event that finally initiated ...
The area surrounding Stenungsund is prone to quick clay landslides, with several large landslides occurring in the area in the past. [7] Göran Sällfors [], Professor Emeritus of Geology and Geotechnics at Chalmers University of Technology, identified a similarity to a landslide that occurred in 2006 approximately 50 kilometres north in Småröd [], with the cause being "large amounts of ...