Show Summary Details

Quick Reference

1 An interstadial that occurred 65 000–60 000 years BP, during the Devensian glaciation.

2 Sections of alluvial sands and organic muds containing tree remains from the Chelford Interstadial, overlaid and underlaid by till, that are exposed in sand pits between Chelford and Congleton, in Cheshire, England.

Subjects: Earth Sciences and Geography — Ecology and Conservation.

Reference entries

Users without a subscription are not able to see the full content. Please, subscribe or login to access all content.