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The Source of Some Erratics from North-Eastern Northamptonshire and adjacent parts of Huntingdonshire1

Published online by Cambridge University Press:  01 May 2009

P. A. Sabine
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Abstract

A collection of erratics from the Boulder Clay and associated remanie drift of the Nene Valley includes distinctive sedimentary, igneous, pyroclastic, and metamorphic rocks. Localities are suggested from which these may have originated and it is concluded that the Upper Chalky Boulder Clay was brought by ice moving from a direction west of north.

Type
Articles
Information
Geological Magazine , Volume 86 , Issue 4 , August 1949 , pp. 255 - 260
Copyright
Copyright © Cambridge University Press 1949

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Footnotes

1

Communicated with the permission of the Director of the Geological Survey and Museum.

References

Baden-Powell, D. F. W., 1948A. Long Distance Correlation of Boulder Clays. Nature, 161, 4086, 287.CrossRefGoogle Scholar
Baden-Powell, D. F. W. 1948B. The Chalky Boulder Clays of Norfolk and Suffolk. Geol. Mag., lxxxv, 279.CrossRefGoogle Scholar
Eastwood, T., and others, 1928. The Geology of the Whitehaven and Workington District. Mem. Geol. Surv., p. 38.Google Scholar
Harmer, F. W., 1928. The Distribution of Erratics and Drift. Proc. Yorks. Geol. Soc., xxi, 102.Google Scholar
Hollingworth, S. E., and Taylor, J. H., 1946. An Outline of the Geology of the Kettering District. Proc. Geol. Assoc., lvii, 230.Google Scholar
Kennedy, W. Q., and Read, H. H., 1936. The Differentiated Dyke of Newmains, Dumfriesshire and its Contact and Contamination Phenomena. Quart. Journ. Geol. Soc., xcii, 116.CrossRefGoogle Scholar
Macgregor, Malcolm., 1937. The Western Part of the Criffell-Dalbeattie Igneous Complex. Quart. Journ. Geol. Soc., xciii, 457.CrossRefGoogle Scholar
Matley, C. A., 1914. Note on the Source of Pebbles of the Bunter Pebble Beds of the English Midlands. Geol. Mag., li, 211.CrossRefGoogle Scholar
Phemister, J., 1936. Summ. Prog. Geol. Surv. Gt. Brit., pt. i, 83.Google Scholar
Richardson, L., and others, 1946. The Geology of the Country around Witney. Mem. Geol. Surv., p. 109.Google Scholar