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Published online by Cambridge University Press: 01 May 2009
My knowledge and observation of facts are neither of them sufficient to enable me to determine the mode of deposit of these blocks in their present sites; probably they may have been glacially trnasported, at the same time with the gravel, to the places where they are now found; or, possibly, they, or some of them, may have been swept away from their original localities in the Tertiary formation, by a flood, or floods, general or partial.
page 297 note 1 These three stones have been placed in the conrt-yard of the Hartley Institute, at Southampton, where, by the kindness of the Principal of that Institution, they may now be seen.
page 298 note 1 The Physical Geology and Geography of Great Britain, by Professor A. C. Ramsay, F.B.S. London, Stanford, Charing Cross.