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A Drift-filled Valley at Thistleton on the Rutland–Lincolnshire Border

Published online by Cambridge University Press:  01 May 2009

R. J. Rice
Affiliation:
Department of Geography, The University, Leicester.

Abstract

A borehole programme by Stewarts and Lloyds Minerals, Ltd., has shown that a narrow tongue of boulder clay conceals a deep steepsided valley cut into the Lincolnshire Limestone and filled with drift. Plotting of structure contours indicates that, even where thedrift is more than 100 feet thick, there is considerable “bulging” of the Upper Lias Clay.

Type
Articles
Copyright
Copyright © Cambridge University Press 1962

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References

REFERENCES

Hollingworth, S. E., 1951. The Northampton Sand Ironstone; its stratigraphy, structure and reserves. Mem. geol. Surv. U.K.Google Scholar
Hollingworth, S. E., Taylor, J. H., and Kellaway, G.A., 1944. Large-scale superficial structures in the Northampton Ironstone field. Quart. J. geol. Soc. Lond., 100, 144.CrossRefGoogle Scholar
Kellaway, G. A., and Taylor, J. H., 1952. Early stages in the physiographic evolution of a portion of the East Midlands. Quart. J. geol. Soc. Lond., 108, 343375.CrossRefGoogle Scholar