Publication Date:
1982-05-01
Description:
SummaryPalaeochannels developed in a terrace of the River Wey are described. Their morphology, relationship with the underlying Folkestone Sands, and the character of associated superficial deposits all suggest that the channels are examples of thermokarst phenomena, probably of Devensian age.
Print ISSN:
0016-7568
Electronic ISSN:
1469-5081
Topics:
Geosciences
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