Abstract
I examine prehistoric and historic quick clay landslide scars in two valleys in northwestern British Columbia, and test the evidence against Bjerrum’s and Levebvre’s landscape evolution models. Streams in the Terrace-Kitimat valley are still incising deep glaciomarine sediments and appear to be in the early and intermediate stages of valley formation, thus large landslides are still occurring and more are expected. In contrast, streams in the Nass Valley are incised into bedrock, in the late stages of valley formation. Early evidence suggests most of the landslides are old, and more large landslides are not expected to be triggered by bank erosion. Rapid incision in the Nass valley may have overwhelmed climatic influences, however in the Terrace-Kitimat valley identified wetter climate regimes seem to correspond to higher earth flow activity. Here, a future warmer and wetter climate, as predicted by most global circulation models, will likely lead to increased landsliding.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
References
Bjerrum L, Løken T, Heiberg S, Foster R (1969) A field study of factors responsible for quick clay slides. In: Proceedings of 7th ICSMFE, vol 2, Mexico, pp 531–540
Bovis MJ, Jones P (1992) Holocene history of earthflow mass movements in south-central British Columbia: the influence of hydroclimatic changes. Can J Earth Sci 29:1746–1755
Church M, MJ Miles (1987) Meteorological antecedents to debris flow in southwestern British Columbia; some case studies. Geol Soc Am Rev Eng Geol 7:63–79
Clague JJ (1984) Quaternary geology and geomorphology, Smithers-Terrace-Prince Rupert area, British Columbia. Geological Survey of Canada, Memoir 413, 71 pp
Clague JJ, Mathewes RW (1996) Neoglaciation, glacier-dammed lakes, and vegetation change in northwestern British Columbia, Canada. Arctic Alpine Res 28:10–24
Evans SG (1989) Rain-induced landslides in the Canadian Cordillera, July 1988. Geosci Can 16:193–200
Farley AL (1979) Atlas of British Columbia, people, environment and resource use. University of British Columbia Press, Vancouver, 136 p
Geertsema M (1998) Flowslides in waterlain muds of northwestern British Columbia, Canada. In: Moore DP, Hungr O (eds) Proceedings of 8th IAEG Congress, vol III, Vancouver, pp 1913–1921
Geertsema M, Schwab JW (1996) A photographic overview and record of the Mink Creek Earthflow, Terrace, British Columbia. B.C. Min. For., Victoria, B.C. Res. Rep. 08
Geertsema M, Schwab JW (1997) Retrogressive flowslides in the Terrace-Kitimat, British Columbia area: from early post-deglaciation to present – and implications for future slides. In: Proceedings of the 11th Vancouver Geotechnical Society Symposium (pp. 115–133). Vancouver BC
Geertsema M, Cruden DK, Schwab JW (2006) A large, rapid landslide in sensitive glaciomarine sediments at Mink Creek, northwestern British Columbia, Canada. Eng Geol 83:36–63
Hogan DL, Schwab JW (1991) Meteorological conditions associated with hillslope failures on the Queen Charlotte Islands. Land management report 73, BC Ministry of forests, 36 pp
Jakob M, Weatherly H (2003) A hydroclimatic threshold for landslide initiation on the North Shore Mountains of Vancouver, British Columbia. Geomorphology 54:137–156
Lafleur J, Lefebvre G (1980) Groundwater regime associated with slope stability in Champlain clay deposits. Can Geotech J 17:44–53
Lebuis JJ, Robert M, Rissmann P (1983) Regional mapping of landslide hazard in Quebec. In: Bergren B, Lindgren J (eds) Symposium on slopes on soft clays, Swedish Geotechnical Institute report No. 17, Linkoping, pp 205–262
Lefebvre G (1986) Slope instability and valley formation in Canadian soft clay deposits. Can Geotech J 23:261–270
Lefebvre G (1996) Soft sensitive clays. In: Turner AK, Shuster RL (eds) Special report 247: landslides investigation and mitigation. TRB, National Research Council, Washington, DC, pp 607–619
McCuaig SJ (1997) Quaternary geology of the Nass River region, British Columbia. Current research 1997-A. Geological Survey of Canada, Ottawa, ON, Canada, pp 183–189.
McNeely R (2005) Geological Survey of Canada radiocarbon dates XXXIV; Geological Survey of Canada current research, Ottawa, ON, Canada, 113 p
Pielou EC (1991) After the ice age: the return of life to glaciated North America. The University of Chicago Press, Chicago and London
Potvin EC, Pellerin F, Demers D, Robitaille D, La Rochelle P, Chagnon J-Y (2002) Revue et investigation complementaire du site du glissement de Saint-Jean-Vianney. In: Proceedings of an Earth Odyssey 2001, Canadian Geotechnical Society, Laval, PQ, Canada, pp 792–800
Schwab JW (1983) Mass wasting: October–November 1978 storm, Rennell Sound, Queen Charlotte Islands, British Columbia. Research Note 91. BC Ministry of Forests, Victoria, BC, Canada, p 23
Tavenas F, Chagnon J-Y, La Rochelle P (1971) The Saint-Jean-Vianney landslide: observations and eyewitnesses accounts. Can Geotech J 8:463–478
Viberg L (1983) Experiences of mapping and classification of stability conditions. In: Bergren B, Lindgren J (eds) Symposium on slopes on soft clays, Swedish Geotechnical Institute Report No. 17, Linkoping, pp 455–461
Author information
Authors and Affiliations
Corresponding author
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2013 Springer-Verlag Berlin Heidelberg
About this chapter
Cite this chapter
Geertsema, M. (2013). Quick Clay Landslides, Landscape Evolution, and Climate Change: A Perspective from British Columbia. In: Margottini, C., Canuti, P., Sassa, K. (eds) Landslide Science and Practice. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-31337-0_15
Download citation
DOI: https://doi.org/10.1007/978-3-642-31337-0_15
Published:
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-31336-3
Online ISBN: 978-3-642-31337-0
eBook Packages: Earth and Environmental ScienceEarth and Environmental Science (R0)