Late Quaternary Environmental Change in North-west Europe: Excavations at Holywell Coombe, South-east England

Holywell Coombe, an embayment in the chalk scarp overlooking Folkestone, Kent, was designated a geological Site of Special Scientific Interest in 1985 because it contains richly fossiliferous Late Quaternary sediments providing a unique archive of the last 13,000 years.
The construction of the Channel Tunnel across the Holywell Coombe SSSI brought about a major rescue excavation, funded by ...