Failure behaviour of bedrock and overburden landslides of the Peace River Valley near Fort St. John, British Columbia
A reach of Peace River between Fort St. John and Hudson’s Hope flows in a steepsided valley cut by meltwater and Holocene river flow through Cretaceous shale and sandstone covered by clay‐rich glaciolacustrine deposits. Numerous landslides occur on the banks, initiating in both the bedrock and overb...
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| Language: | English |
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University of British Columbia
2012
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| Online Access: | http://hdl.handle.net/2429/42928 |