The Newer Pliocene Period in England
- 1 February 1882
- journal article
- Published by Geological Society of London in Quarterly Journal of the Geological Society
- Vol. 38 (1-4) , 667-745
- https://doi.org/10.1144/gsl.jgs.1882.038.01-04.53
Abstract
In the previous part of this Memoir, after describing the conditions under which the beds of the Red and Fluvio-marine Crag accumulated, and their overspread during a depression by the Chillesford Clay, I traced the progress of events from this time to the recession of the ice of the Major Glaciation, in the following order, viz.:— The elevation and denudation of much of this Crag and Clay over all but their north-western, or most estuarine, extremity, and the formation at Kessingland, in North-east Suffolk, of a freshwater bed on one of the islands which came into existence by such elevation and denudation.Keywords
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