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Published online by Cambridge University Press: 01 May 2009
page 482 note 1 See Geol. Magazine for 10 and 11 1867, Vol. IV.Google Scholar
page 483 note 1 Both ends of these passes have since been deepened by streams, in many places to a very great extent; for atmospheric denudation is more active in some parts of the Cotteswold district than in any part of South Britain with which I am acquainted.