Mud aprons in front of Svalbard surge moraines: Evidence of subglacial deforming layers or proglacial glaciotectonics?
Large debris-flow units commonly occur on the distal sides of subaqueous end moraines deposited by surges of Svalbard tidewater glaciers, but have rarely been described in terrestrial settings. Some researchers have argued that these kinds of debris flows reflect processes unique to the subaqueous e...
| Published in: | Geomorphology |
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| Main Authors: | , , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
2009
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| Subjects: | |
| Online Access: | https://research-portal.st-andrews.ac.uk/en/researchoutput/mud-aprons-in-front-of-svalbard-surge-moraines-evidence-of-subglacial-deforming-layers-or-proglacial-glaciotectonics(280a89af-93d9-4c7a-b373-0d35cf678945).html https://doi.org/10.1016/j.geomorph.2009.04.022 |