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III.—The Suffolk Boxstones and their probable Age

Published online by Cambridge University Press:  01 May 2009

Alfred Bell
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Extract

The detrital matter underlying the Suffolk and N.W. Essex Crags forms an incongruous mass of disrupted local rocks and fossils, supplemented by a few transported boulders of igneous and sedimentary rocks of different ages and mostly small. To these have to be added organic remains of many classes in various conditions of preservation.

Type
Original Articles
Information
Geological Magazine , Volume 5 , Issue 1 , January 1918 , pp. 15 - 21
Copyright
Copyright © Cambridge University Press 1918

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References

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