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Published online by Cambridge University Press: 01 May 2009
For some time I have had under observation the sections of drift exposed in the cuttings of the Seacombe branch of the Wirral Railway, and hope to describe them on some future occasion when the sections are nearer completion.
However, Mr. Mellard Keade has forestalled me in the description of one part of the sections, and professes to have foundinthem evidence of “ an ancient glacial shore.” What does he produce in favour of the statement?
1 See Proc. Roy. Dublin Soc. vol. vii. (1892), p. 518.Google Scholar
2 Geol. Mag. Feb. 1894.