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TitleInSAR monitoring of a retrogressive thaw flow at Thunder River, lower Mackenzie
 
AuthorSinghroy, V; Murnaghan, K; Couture, R
SourceGeo2010, proceedings of the 63rd Annual Canadian Geotechnical Conference and the 6th Canadian Permafrost Conference; 2010 p. 1317-1322
Image
Year2010
Alt SeriesEarth Sciences Sector, Contribution Series 20100181
Meeting63rd Canadian Geotechnical Conference and the 6th Canadian Permafrost Conference; Calgary; CA; September 12-16, 2010
Documentbook
Lang.English
Mediapaper
RelatedThis publication is contained in Evaluating the major controls on permafrost distribution in Ivvavik National Park based on process-based modelling
ProvinceNorthwest Territories
NTS106O/05; 106O/06; 106O/07; 106O/10; 106O/11; 106O/12
AreaThunder River; Mackenzie Valley
Lat/Long WENS-132.0000 -130.5000 67.7500 67.2500
Subjectsengineering geology; surficial geology/geomorphology; geophysics; slope stability; slope stability analyses; slope failures; slope deposits; landslide deposits; landslides; remote sensing; permafrost; freezing ground; ground ice; RADARSAT; InSAR; Mackenzie Valley Pipeline Corridor
Illustrationslocation maps; images; photographs
ProgramSecure Canadian Energy Supply
AbstractIn this study we analysed 55 RADARSAT 1 InSAR images acquired from August 2006-July 2010 to monitor deformation of permafrost slopes along the Mackenzie Valley Pipeline Corridor. Results from two corner reflectors installed near a landslide show a 10 and 20 cm motion from 2006-2010. Our InSAR measurement also shows that the lower steeper slope is moving faster than upper slope. This differential motion may be due to a combination of thaw depth, slope angle and ground moisture.
GEOSCAN ID286251

 
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