Book contents
- Landslides
- Landslides
- Copyright page
- Contents
- Contributors
- Preface
- 1 Landslide hazard and risk
- 2 Landslides in the Earth system
- 3 Earthquake ground motion and patterns of seismically induced landsliding
- 4 Landslides at stratovolcanoes initiated by volcanic unrest
- 5 Mobility of long-runout rock avalanches
- 6 Rapid rock-slope failures
- 7 Risk assessments for debris flows
- 8 Landslides in quick clay
- 9 Controls on the distribution of major types of submarine landslides
- 10 Tsunami hazard assessment related to slope failures in coastal waters
- 11 Physical impacts of climate change on landslide occurrence and related adaptation
- 12 Landslides and geologic environments
- 13 Numerical modeling of rock-slope instability
- 14 Remote sensing techniques and landslides
- 15 Engineering geomorphology of landslides
- 16 Developments in landslide runout prediction
- 17 Models of the triggering of landslides during earthquakes
- 18 Slow rock-slope deformation
- 19 Landslide monitoring:
- 20 Groundwater in slopes
- 21 Soil slope stabilization
- 22 Rockfall characterization and modeling
- 23 The 2006 Eiger rockslide, European Alps
- 24 Randa:
- 25 Characterization and management of rockslide hazard at Turtle Mountain, Alberta, Canada
- 26 The Åknes rockslide, Norway
- 27 A seismometric approach for back-analyzing an unusual rockfall in the Apennines of Italy
- 28 Downie Slide, British Columbia, Canada
- 29 The 1963 Vaiont landslide, Italy
- 30 Hong Kong landslides
- 31 Landslides induced by the Wenchuan earthquake
- 32 Landslides on other planets
- Index
25 - Characterization and management of rockslide hazard at Turtle Mountain, Alberta, Canada
Published online by Cambridge University Press: 05 May 2013
- Landslides
- Landslides
- Copyright page
- Contents
- Contributors
- Preface
- 1 Landslide hazard and risk
- 2 Landslides in the Earth system
- 3 Earthquake ground motion and patterns of seismically induced landsliding
- 4 Landslides at stratovolcanoes initiated by volcanic unrest
- 5 Mobility of long-runout rock avalanches
- 6 Rapid rock-slope failures
- 7 Risk assessments for debris flows
- 8 Landslides in quick clay
- 9 Controls on the distribution of major types of submarine landslides
- 10 Tsunami hazard assessment related to slope failures in coastal waters
- 11 Physical impacts of climate change on landslide occurrence and related adaptation
- 12 Landslides and geologic environments
- 13 Numerical modeling of rock-slope instability
- 14 Remote sensing techniques and landslides
- 15 Engineering geomorphology of landslides
- 16 Developments in landslide runout prediction
- 17 Models of the triggering of landslides during earthquakes
- 18 Slow rock-slope deformation
- 19 Landslide monitoring:
- 20 Groundwater in slopes
- 21 Soil slope stabilization
- 22 Rockfall characterization and modeling
- 23 The 2006 Eiger rockslide, European Alps
- 24 Randa:
- 25 Characterization and management of rockslide hazard at Turtle Mountain, Alberta, Canada
- 26 The Åknes rockslide, Norway
- 27 A seismometric approach for back-analyzing an unusual rockfall in the Apennines of Italy
- 28 Downie Slide, British Columbia, Canada
- 29 The 1963 Vaiont landslide, Italy
- 30 Hong Kong landslides
- 31 Landslides induced by the Wenchuan earthquake
- 32 Landslides on other planets
- Index
Summary
In 1903, more than 30 million m3 of rock fell from the east slopes of Turtle Mountain in Alberta, Canada, causing a rock avalanche that killed about 70 people in the town of Frank. The Alberta Government, in response to continuing instabilities at the crest of the mountain, established a sophisticated field laboratory where state-of-the-art monitoring techniques have been installed and tested as part of an early-warning system. In this chapter, we provide an overview of the causes, trigger, and extreme mobility of the landslide. We then present new data relevant to the characterization and detection of the present-day instabilities on Turtle Mountain. Fourteen potential instabilities have been identified through field mapping and remote sensing. Lastly, we provide a detailed review of the different in-situ and remote monitoring systems that have been installed on the mountain. The implications of the new data for the future stability of Turtle Mountain and related landslide runout, and for monitoring strategies and risk management, are discussed.
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- Information
- LandslidesTypes, Mechanisms and Modeling, pp. 310 - 322Publisher: Cambridge University PressPrint publication year: 2012
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