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- W4248070022 abstract "The object of the present brief notice is to bring before the Society, while the works are in progress, a feature of intraglacial structure disclosed by the sewerage works at Norwich, in order that, since the case appears to us to be peculiar among the perplexing features presented by the glacial beds as far as yet known, the opportunity may be afforded, to any who may suspect that some mistake has been made, of investigating the accuracy of our representation before the means of doing so are removed. For this reason we have ventured to bring the subject forward now, instead of reserving it for description with the general glacial structure of the east of England, which we hope at some future time to lay before the Society. All the valleys of Suffolk, and of Central and Eastern Norfolk, are excavated out of the glacial beds, and possess no connexion whatever with any preglacial condition of the surface. They appear, however, to have had their configuration and direction determined in several places by a denudation of the glacial beds themselves, which was effected during the progress of their deposit. Of this the case before us affords one instance. The accompanying section shows the structure of the valley of the Yare, near the places of its inosculation with that of the Tese and that of the Wensum. The sewer-works, up to the present time, have been carried on by shafts, sunk in the bottom of the valley, where the surface is" @default.
- W4248070022 created "2022-05-12" @default.
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- W4248070022 date "1869-02-01" @default.
- W4248070022 modified "2023-10-16" @default.
- W4248070022 title "On a peculiar Instance of Intraglacial Erosion near Norwich" @default.
- W4248070022 doi "https://doi.org/10.1144/gsl.jgs.1869.025.01-02.78" @default.
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