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TitleInSAR monitoring of the Frank Slide
 
AuthorSinghroy, V; Couture, R; Molch, K
SourceLandslide risk management: proceedings of the International Conference on Landslide Risk Management; by Hungr, O (ed.); Fell, R (ed.); Couture, R (ed.); Eberhardt, E (ed.); 2005 p. 611-614
Year2005
Alt SeriesEarth Sciences Sector, Contribution Series 2004370
PublisherA.A. Balkema Publishers (Leiden, The Netherlands)
PublisherTaylor & Francis Group (London, UK)
MeetingInternational Conference on Landslide Risk Management; Vancouver, BC; CA; May 31 - June 3, 2005
Documentbook
Lang.English
Mediapaper
ProvinceAlberta
NTS82G/09
AreaFrank; Canadian Rockies
Lat/Long WENS-114.5000 -114.0000 49.7500 49.5000
Subjectsstructural geology; engineering geology; landslides; slope failures; slope stability; remote sensing; satellite imagery; radar imagery; deformation; meteorology; planning; Frank Slide; Data processing
Illustrationstables; 3-D diagrams
ProgramNatural Hazards and Emergency Response
AbstractIn this study, we used interferometrically derived images, from several radar satellites (RADARSAT, ERS and ENVISAT), to monitor current post slide motion at the Frank Slide, a 30x 106m3slide-rock avalanche, in the Canadian Rockies. The images cover the period from July 1993 to June 2004. Our results show that the Frank slide is still active and the deformation process is localized and are related to seasonal and local weather conditions. This information is useful in assisting to locate in-situ field monitoring at specific locations, and to plan mitigation strategies. The combination of satellite differential InSAR techniques, covering large areas, and site-specific GPS monitors can produce an integrated monitoring system of active slopes.
GEOSCAN ID220192

 
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