Hope landslide
The landslide of Hope (Engl. Hope Slide ) occurred on January 9, 1965 in Hope , 135 kilometers east of Vancouver , the largest city in British Columbia , in the extreme southwest of Canada. Hope had been promoted to town shortly before.
The landslide was the largest to date in Canadian history and - although in an almost uninhabited area - cost the lives of four people, two of the victims were never found. It tore off a steep slope (> 45 °) just below a ridge in the Cascade Mountains and poured into a side valley of the Coquihalla River , which flows into the Fraser River about 10 km further at Hope . Local surveys showed that 46 million cubic meters of rock and rubble fell down a slideway that was inclined by about 20 ° under the steep slope and was left in a huge heap 70 meters high and three kilometers long. According to a rule of thumb from Albert Heim , the mass falling on the slideway must have had a speed of over 200 km / h.
The debris avalanche filled a lake (Outram Lake) near the Nicolum River completely and shifted the course of the river. It also rolled over a few miles from Highway 3 (a branch of the newly opened Trans-Canada Highway ) that had to be closed for weeks. However, short-term closures are often necessary in winter and because of minor landslides.
It is not possible to clearly determine whether a small earthquake triggered the landslide. It could also indicate a previous landslide . The rock of the mountainside is old, metamorphic basalt , but with layers of clay minerals and some fault lines. Most geologists assume that the clay was saturated with water from previous weather conditions.
literature
- 46-million-cubic-meter Pemberton avalanche second only to Hope Slide
- http://web.viu.ca/earle/geol390/hope-slide.doc
- English article
Individual evidence
- ↑ corresponds to a rock volume of 50 × 50 × 185 meters
- ↑ lock z. B. in February 2008: Coquihalla remains closed, in: Hope Standard, February 14, 2008 ( Memento from March 31, 2008 in the Internet Archive )