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IV.—Sir Henry H. Howorth and the Glaciation of Norway
Published online by Cambridge University Press: 01 May 2009
Extract
Few will deny that whatever comes from the pen of Sir Henry Howorth is always interesting and original, whether the reader agrees with it or otherwise. This is especially the case when he has a theory to build up or to overturn, and in the latter case he not only tries to knock over his antagonist, but he discharges at him volleys of brilliant verbiage with the view to his utter annihilation.
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References
page 454 note 1 Page 356.
page 455 note 1 The course of the ice movement over the same region is shown on Professor James Geikie's glacial map of Scotland, and on one of the general glaciation of the British Isles in the writer's “Physical History of the British Isles” (p. 118, pl. xiii).Google Scholar Also: Croll, , “Climate and Time,” p. 444;Google Scholar Peach, and Home, , Quart. Journ. Geol. Soc., vol. xxxvi, p. 648;Google Scholar T. F. Jamieson, ibid., vol. xxii, p. 261.
page 456 note 1 In the paper on “Another possible Cause of the Glacial Epoch,” to which the Council of the Geological Society thought proper to refuse publication, I adduced the case of this submerged plateau as being a representative of those of the eastern coast of An erica and the Antilles so ably worked out by Professor Spencer.