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III.—The Suffolk Boxstones and their probable Age
Published online by Cambridge University Press: 01 May 2009
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.
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