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- W2024661431 abstract "The established denudation chronology for south Derbyshire is questioned in the light of recent field and borehole evidence. It is argued that existing surfaces of faint relief are unlikely to be the direct result of early Pleistocene planation since they frequently occur on variable thicknesses of glacial drift. Furthermore, the subjacent bedrock floor is often irregular, bearing little or no relationship to the surface morphology. It is suggested that the level surface forms were produced in response to late-Pleistocene (Devensian) periglacial activity, and that their progressive declination towards the modern valley floors is merely indicative of the contemporary topography at the time of their formation. These views also imply that the previously held concept of a pre-glacial landscape that remained little changed until the present day is no longer tenable." @default.
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- W2024661431 date "1985-01-01" @default.
- W2024661431 modified "2023-09-27" @default.
- W2024661431 title "A re-appraisal of the denudation chronology of south Derbyshire, England" @default.
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- W2024661431 doi "https://doi.org/10.1016/s0016-7878(85)80015-8" @default.
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