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Textural distinction of Main Glaciation and Scottish Readvance tills in the Cumberland lowland

Published online by Cambridge University Press:  01 May 2009

David Huddart
David Huddart
Affiliation:
Department of Geology, The University, Newcastle-upon-Tyne
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Summary

The sand/matrix ratio technique is described and has been shown to provide a rapid method of correlating till units in the Cumberland lowland which belong to separate glacial phases. Basal tills have a relatively constant sand/silt-matrix ratio compared with flowage tills in the same locality.

Type
Articles
Information
Geological Magazine , Volume 108 , Issue 4 , July 1971 , pp. 317 - 324
Copyright
Copyright © Cambridge University Press 1971

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References

Shepps, V. C. 1953. Correlation of tills of North Eastern Ohio by size analysis. J. sedim. Petrol. 23, 34–48.CrossRefGoogle Scholar
Sitler, R. F. 1968. Glacial till in orientated thin section. 23rd. Int. Geol. Congr. 8, 283–95.Google Scholar
Trotter, F. M. 1929. Glaciation of the Eastern Edenside, the Alston Block and the Carlisle Plain. Q. Jl geol. Soc. Lond. 88, 549–607.CrossRefGoogle Scholar