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I.—The Danbury Gravels

Published online by Cambridge University Press:  01 May 2009

J. W. Gregory
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Extract

Danbury stands on a gravel-capped plateau in Mid-Essex, five miles east of Chelmsford. The gravel is part of a once largersheet and contains a variety of rocks foreign to the district. It was therefore naturally at first regarded as a glacial gravel. This view was adopted by S. V. Wood, jun. (e.g. 1867, p. 12; 1870, p. 61), by the Rev. O. Fisher (1868, p. 98), on the Geological Survey Map (Sheet 1, N.E., 1871), and by Mr. Whitaker (1889, p. 279). Sir Joseph Prestwich regarded the Danbury gravels (1890, p. 135) as Bagshot pebble-beds invaded by some glacial agent, and the late H. B. Woodward (1903, p. 15) described them as the wreck in Glacial times of an older gravel.

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Type
Original Articles
Information
Geological Magazine , Volume 2 , Issue 12 , December 1915 , pp. 529 - 538
Copyright
Copyright © Cambridge University Press 1915

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References

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