TY - JOUR PY - 2008// TI - Large-scale moraine deformation at the Athabasca Glacier, Jasper National Park, Alberta, Canada JO - Landslides A1 - Hugenholtz, Chris A1 - Moorman, Brian A1 - Barlow, John A1 - Wainstein, Pablo SP - 251 EP - 260 VL - 5 IS - 3 N2 - In this paper the development of a large-scale gravitational deformation involving the eastern lateral moraine of the Athabasca Glacier in Jasper National Park, Alberta, Canada, is described. Interpretation and analysis of sequential aerial photographs indicates that a 540-m-wide segment of the eastern lateral moraine began to deform in the early 1950s; however, significant movement only began in the late 1960s. Since then, the moraine has undergone progressive gravitational deformation leading to a network of fractures, bulging, and the development of a large gap in the moraine crest. Geographic information system analysis of topographic changes between 1967 and 2006 indicates that the displaced volume of the moraine is approximately 9.0 × 10 5 m 3 . In the last 39 years, the moraine crest has displaced 55 m (1.4 m yr −1 ) down towards the glacier. The development of slope instability is linked to a combination of debuttressing from recent glacier recession, deformation of the moraine, as well as the movement of a large, mobile, debris-mantled slope impinging the upslope margin of the lateral moraine. This case study illustrates the importance of glacial conditioning and local geomorphological factors in creating conditions for large-scale moraine instability in recently deglacierized alpine basins.

LA - SN - 1612-510X UR - http://dx.doi.org/10.1007/s10346-008-0116-5 ID - ref1 ER -