Climate and Terrain Characteristics Linked to Mud Ejection Occurrence in the Canadian High Arctic
Pressurised slurries of fine‐grained sediment expelled from the base of the active layer have been observed in recent years in the High Arctic. Such mud ejections, however, are poorly understood in terms of how exactly climate and landscape factors determine when and where they occur. Mud ejections...
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Veröffentlicht in: | Permafrost and periglacial processes 2016-04, Vol.27 (2), p.204-218 |
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