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Published online by Cambridge University Press: 01 May 2009
In a letter to this Magazine of May, 1895, headed “The Indentation of the Bunter Pebbles,” Mr. W. S. Gresley criticizes the summing-up of my views, given in the ‘Annals of British Geology’ (1892, p. 52), that “The indentation of the pebbles he considers to be the result of contact-solution, the water being retained at these spots by capillary attraction.” It would have been more satisfactory if Mr. Gresley could have read my original paper before penning his letter, as he would then not have assumed that I “adduce no evidence in support of the chemical theory.”
page 341 note 1 The Trias of Cannock Chase, Proc. Liverpool Geol. Soc., Session 1891–2.
page 343 note 1 Quartz-rock, Holyhead, is given by Mallet as 1641·6 tons per square foot across laminations, and 900 tons parallel to laminations.—Manual of Rocks, Tables, etc., D. K. Clark, p. 631.