Abstract:Solifluction sheets are large‐scale and extensive valley‐floor and valley‐side landforms developed widely in the British Isles from mass‐wasting of glacial and periglacial sediments during late‐glacial times. We describe their geographical distribution and review the processes that have led to their development. We use data from the Cheviot Hills, the one site in the British Isles where sedimentology and optically stimulated luminescence dating have been combined, to assess their age and nature of deposition. … Show more
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