Geomorphology of the huge Hinlopen-Yermak landslide on the northern Svalbard margin

Submarine landslide scars, including the huge Hinlopen–Yermak slide-scar north of Svalbard (Fig. 1) (Vanneste et al. 2006; Winkelmann et al. 2006), are relatively common geomorphological features on glaciated continental margins. However, landslide characteristics, for example scar area, run-out and...

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Bibliographic Details
Published in:Geological Society, London, Memoirs
Main Authors: Hogan, K. A., Vanneste, M., Dowdeswell, J. A., Mienert, J.
Other Authors: Dowdeswell, J.A., Canals, M., Jakobsson, M., Todd, B.J., Dowdeswell, E.K., Hogan, K.A.
Format: Book Part
Language:unknown
Published: Geological Society of London 2016
Subjects:
Svalbard
glacier
Svalbard margin
Online Access:http://nora.nerc.ac.uk/id/eprint/515712/
https://doi.org/10.1144/M46.123
Description
Summary:Submarine landslide scars, including the huge Hinlopen–Yermak slide-scar north of Svalbard (Fig. 1) (Vanneste et al. 2006; Winkelmann et al. 2006), are relatively common geomorphological features on glaciated continental margins. However, landslide characteristics, for example scar area, run-out and displaced volume, vary significantly (Hogan et al. 2013). A key pre-condition for failure is rapid deposition of mainly diamictic glacier-derived sediment on the slope during full-glacials, alternating with fine-grained interglacial deposition. This layered architecture, and the varying geotechnical properties of the debris, facilitate downslope mass-movements with a variety of possible triggers

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