On the 9th January 1965, from the southwestern slope of Johnson ridge, 150 km west of Vancouver, approximately 15 km from Hope along the BC Highway 3, a 44 million m3 rock slide fell in two separate events, between 4 am and 7 am (VON SACKEN, 1991); the movement assumed the behavior of a rock avalanche. The sliding mass fell down, filling the Outram Lake, destroying and burying several km of the BC highway 3, sweeping away and killing four people, which were unfortunately never found. As a result of the slide, the valley floor was raised of about 70 m with respect to the original topography. Hope Slide represents the major historical rock avalanche in Canada. This work summarizes the results of a geological, structural and geomorphological s...
Since the occurrence of the Frank Slide in 1903, studies have identified potentially unstable volume...
This is the author accepted manuscript. The final version is available from Geological Society of Am...
It is being increasingly realized that there exists an interrelationship between seismicity and rock...
On the 9th January 1965, from the southwestern slope of Johnson ridge, 150 km west of Vancouver, app...
The 1965 Hope Slide is one of the largest rock avalanche to have occurred in recent historic time. A...
Factors governing rock slope stability include lithology, geological structures, hydrogeological con...
Abstract We present he well-documented case of a 2- 106 m 3 rockslide that was recorded by seismogra...
The displacement of a large slow-moving landslide is accompanied by slope damage, such as fractures,...
Debris sliding is one of the most important processes acting to transport sediment within mountainou...
Three highly mobile landslides, all of which have occurred in this millennium, have been documented,...
The Cascade Bay landslide is a large postglacial bedrock failure on the east side of Harrison Lake i...
The Barrier is a steep, 250 m-high escarpment of dacite in Garibaldi Provincial Park, British Columb...
Many large, deep-seated landslides have occurred along the Peace River Valley and its steep-sided tr...
The purpose of this study is to understand the environment for failure of the Perpetual Landslide. T...
Mount Meager is a glacier-clad volcanic complex in British Columbia, Canada. It is known for its lan...
Since the occurrence of the Frank Slide in 1903, studies have identified potentially unstable volume...
This is the author accepted manuscript. The final version is available from Geological Society of Am...
It is being increasingly realized that there exists an interrelationship between seismicity and rock...
On the 9th January 1965, from the southwestern slope of Johnson ridge, 150 km west of Vancouver, app...
The 1965 Hope Slide is one of the largest rock avalanche to have occurred in recent historic time. A...
Factors governing rock slope stability include lithology, geological structures, hydrogeological con...
Abstract We present he well-documented case of a 2- 106 m 3 rockslide that was recorded by seismogra...
The displacement of a large slow-moving landslide is accompanied by slope damage, such as fractures,...
Debris sliding is one of the most important processes acting to transport sediment within mountainou...
Three highly mobile landslides, all of which have occurred in this millennium, have been documented,...
The Cascade Bay landslide is a large postglacial bedrock failure on the east side of Harrison Lake i...
The Barrier is a steep, 250 m-high escarpment of dacite in Garibaldi Provincial Park, British Columb...
Many large, deep-seated landslides have occurred along the Peace River Valley and its steep-sided tr...
The purpose of this study is to understand the environment for failure of the Perpetual Landslide. T...
Mount Meager is a glacier-clad volcanic complex in British Columbia, Canada. It is known for its lan...
Since the occurrence of the Frank Slide in 1903, studies have identified potentially unstable volume...
This is the author accepted manuscript. The final version is available from Geological Society of Am...
It is being increasingly realized that there exists an interrelationship between seismicity and rock...