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Plant remains from the Corton Beds at Lowestoft, Suffolk

Published online by Cambridge University Press:  01 May 2009

R. G. West  and
D. Gay Wilson
R. G. West
Affiliation:
Department of Botany, University of Cambridge.
D. Gay Wilson
Affiliation:
Department of Botany, University of Cambridge.
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Summary

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.

Type
Articles
Information
Geological Magazine , Volume 105 , Issue 2 , April 1968 , pp. 116 - 123
Copyright
Copyright © Cambridge University Press 1968

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References

REFERENCES

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