| Title | Analyse des déplacements du glissement de Gascons, Gaspésie, par couplage d'observations aéroportées et terrestres |
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| Author | Lord, P -E; Locat, J; Cloutier, C; Couture, R; Charbonneau, F; Singhroy, V; Pedrazzini, A |
| Source | Geo2010, proceedings of the 63rd Annual Canadian Geotechnical Conference and the 6th Canadian Permafrost Conference; 2010 p. 56-64 |
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| Year | 2010 |
| Alt Series | Earth Sciences Sector, Contribution Series 20100062 |
| Meeting | 63rd Canadian Geotechnical Conference and the 6th Canadian Permafrost Conference; Calgary; CA; September 12-16, 2010 |
| Document | book |
| Lang. | English |
| Media | paper |
| Related | This publication is contained in Evaluating the major
controls on permafrost distribution in Ivvavik National Park based on process-based modelling |
| Province | Quebec |
| NTS | 22A/02NW |
| Area | Gaspé Peninsula; Gascons; Baie des Chaleurs; Port-Daniel-Gascons |
| Lat/Long WENS | -65.0000 -64.7500 48.2500 48.0833 |
| Subjects | engineering geology; surficial geology/geomorphology; slope stability; slope stability analyses; slope failures; slope deposits; landslide deposits; landslides; remote sensing; LiDAR |
| Illustrations | location maps; images |
| Released | 2010 01 01 |
| Abstract | In Gaspesie peninsula, an unstable rock slope has been identified near Port-Daniel-Gascons. This unstable slope stands approximately from sea level up to 100m above the Baie des Chaleurs. Sixty-three
meter above mean sea level, a railway runs across the landslide. In 2009, a complete automated monitoring network has been installed. This system has been developed to monitor parameters that could lead to failure or to acceleration of the current
deformation rates. In order to link these deformations to the landslide morphology, an airborne LiDAR survey has been conducted to define the reference elevation model. |
| GEOSCAN ID | 285472 |
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