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on the method used for the determination of the shear strength. When a clay is remolded, the position of the particles and the balance . of the interparticle stresses is disturbed. Quick clay landslide in Rissa, Norway, 1978. Source: Norwegian Geotechnical Institute (NGI) On 29 April 1978, a landslide wiped away an area of 330 km 2 (about the same as 47 football pitches) including 13 farms, two homes and the local community centre.

Alta: a truly remarkable video of a quick clay landslide in Norway One of the top ten landslide videos of all time was captured yesterday at Kråknes in Alta, in the north of Norway. This video shows what is almost certain to be a quick clay landslide. It occurred in the morning of Wednesday 3 June 2020; the video has been posted to Youtube. The quick clay landslide created a ravine in the village of Ask. Credits: Forbes/NTB/AFP VIA GETTY IMAGES A massive quick clay landslide struck in a Norwegian village sweeping away buildings. The landslide occurred in the village of Ask, located in the municipality of Gjerdurm on December 30, 2020. Quick clay has been the underlying cause of many deadly landslides. In Canada alone, it has been associated with more than 250 mapped landslides.

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The slide measured 2300 feet by 984 feet (700m by 300m). The collapse injured at least 10 people with one seriously injured. Do take a look – the film is amazing.

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• Rainfall. • Earthquake. Man-made triggers. The Norwegians define quick clays as those soils quick clay considers soil behavior only, ignoring In nonsensitive soils, landslide masses generally come to 18 Oct 2019 highly sensitive, low-salinity, glaciomarine quick clay at Dragvoll, Trondheim, Norway, Keywords: geochemistry landslides soil stabilisation.

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This PhD is expected to improve the current knowledge of quick-clay landslides and how they are preconditioned. Climate change will probably affect the study area in the near future, most likely increasing landslide risk, therefore, research should continue and advance to new levels. 2021-03-25 · The quick clay ground under the affected area of Ask is known to be at high-risk of landslides.

The Quick clay landslide in Rissa, Sør-Trøndelag in 1978, is the largest in volume that has hit Norway after 1900.
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Mapping of quick clay using geoelectrical imaging and CPTU

In stepwise landslides, sufficient failed material liquefies that the debris from each step flows away from the slide scarp, leaving an unsupported unstable slope that, in turn, fails and flows away.