Darwin, C. R. to Fitton, W. H.
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[Excerpt copied from a letter CD wrote to WHF.]
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CD's gratefulness to William Buckland for his guidance on the glaciated terrain of N. Wales. "I am also convinced that the valleys of Glen Roy … have been occupied by arms of the Sea, & very likely, (for on that point I cannot of course doubt Agassiz & Buckland) by glaciers also."
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Transcription
[Capel Curig, N Wales]
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Yesterday (and the previous days) I had some most interesting work in examining the
marks left by extinct glaciers— I assure you no
extinct volcano could hardly leave more evident traces of its activity and vast powers.
I found one with the lateral moraine quite perfect, which D
C. Darwin
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- f1 632.f1
The text of the extract is published in E. C. Agassiz 1885, 1: 342–3, where the recipient is mistakenly identified as ‘Dr Tritten’. A copy was enclosed in a letter to Louis Agassiz from William Buckland, dated 22 July 1842. According to Buckland, it ‘was communicated to me by Dr. [Fitton], during the late meeting [of the British Association] at Manchester, in time to be quoted by me versus Murchison, when he was proclaiming the exclusive agency of floating icebergs in drifting erratic blocks and making scratched and polished surfaces’ (E. C. Agassiz 1885, 1: 342). - +
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CD explored glacial sites in North Wales 18–28 June 1842 (‘Journal’; Correspondence vol. 2, Appendix II). Notes made during the trip are in DAR 27.1, together with a draft of his article on ‘Notes on the effects produced by the ancient glaciers of Caernarvonshire’ (Collected papers 1: 163–71). - +
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Buckland 1841. - +
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CD refers to his geological tour with Adam Sedgwick in August 1831. - +
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See ‘On the distribution of the erratic boulders and on the contemporaneous unstratified deposits of South America’ (Collected papers 1: 145–63). - +
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See ‘Observations on the parallel roads of Glen Roy’ (Collected papers 1: 87–137).