FIELD MONITORING OF LANDSLIDE DEFORMATION USING LOW ALTITUDE PHOTOGRAMMETRY
The Ottawa/Gatineau region has significant deposits of sensitive glacial marine clay. As these deposits have risen due to isostatic rebound, these materials have been incised by various watercourses, carving river valleys throughout the region. The slopes of these river banks are susceptible to retr...
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| Language: | en en |
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2012
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| Online Access: | http://hdl.handle.net/1974/6993 |