Plant remains from the Corton Beds at Lowestoft, Suffolk
- 1 April 1968
- journal article
- research article
- Published by Cambridge University Press (CUP) in Geological Magazine
- Vol. 105 (2), 116-123
- https://doi.org/10.1017/s0016756800052481
Abstract
A flora found in a clay lens in the Corton Beds at Lowestoft indicates a late- or full-glacial type of environment during an interval in the deposition of the Corton Beds. The interval may be related to drainage changes associated with the retreat of the North Sea Drift ice and advance of the Lowestoft Till ice.Keywords
This publication has 1 reference indexed in Scilit:
- Field meeting in the Lowestoft DistrictProceedings of the Geologists' Association, 1950