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Published online by Cambridge University Press: 01 May 2009
The Limestone of the foreshore at Dwlban Point is magnificently glaciated, the ice-worn surfaces being preserved for a distance of some yards from the Boulder-clay. The striæ where undeflected run N.N.E.-S.S.W., which is in agreement with the general direction of the glaciation on that part of the coast.
1 For this photograph and that illustrating the preceding paper, as well as for the lantern slides and other photographs of these phenomena, used at the British Association, I am indebted to Mr. J. Trevor Owen, M.A., Headmaster of the County School, Carnarvon.