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In the Geological Magazine of last year I described a system of Miniature Faulting observed by me in a fine bed of banded silty clay at Nevin, Carnarvonshire. This year I have had the good fortune to observe Faulting in Drift on a much larger scale in the neighbourhood of St. Bees, Cumberland, which is highly instructive and explanatory of several features of Normal Faulting which the other illustration did not touch.
1 “A Miniature Illustration of Normal Faulting,” Geol Mag. Nov. 1891, p. 487.Google Scholar