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VI.—On a New Section of Pre-Glacial White Clay and Sand near Mold

Published online by Cambridge University Press:  01 May 2009

D. Mackintosh
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Extract

Mr George Maw, in the Geological Magazine, Vol. IV. pp. 24 and 299, has described a number of sections in Flintshire and Denbighshire in which white clay or sand occurs under Boulder-clay. A newly-exposed section near Colomendey Hall, about three miles from Mold, is very important on account of the complete series of glacial drifts by which the white clay is overlain. I lately examined it in company with Mr. Manning, of the Chester Natural Science Society.

Type
Research Article
Information
Geological Magazine , Volume 1 , Issue 2 , February 1874 , pp. 67 - 68
Copyright
Copyright © Cambridge University Press 1874

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References

page 67 note 1 Nearly all that can be seen of the blue clay fills up a hollow in the white clay. But a bore-hole at some distance from the pit reveals its existence in the same position relatively to the other deposits.

page 68 note 1 See Geol. Mag. Vol. VII. 10. and 12. 1870, and Vol. IX. 01, 1872.Google Scholar