Speleothem U-series constraints on scarp retreat rates and landscape evolution: an example from the Severn valley and Cotswold Hills gull-caves, UK

Modelling landscape evolution requires quantitative estimates of erosional processes. Dating erosional landscape features such as escarpments is usually difficult because of the lack of datable deposits. Some escarpments and valley margins are associated with the formation of mass-movement caves, so...

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Bibliographic Details
Main Authors: Farrant, Andrew R., Noble, Stephen R., Barron, A.J. Mark, Self, Charles A., Grebby, Stephen
Format: Article
Published: Geological Society of London 2014
Online Access:https://eprints.nottingham.ac.uk/33867/