Abstract
ONE of the largest and most successful among recent meetings of the British Association has just been concluded in Dublin. The following return shows the number of tickets issued in the varioui classes of members:—
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References
Journ. Soc. Chem. Ind., 1906, 1019.
March 15, 1907.
Ber., 1900, i., lxxi.
Levinstein, Journ. Soc. Chem. Ind., 1903, 845.
Pror. R.S., lxxvii, p. 472, and lxxv.ii., p. 150.
NATURE, lxxv., p. 294.
Trans. Royal Dublin Soc., vol. vii., ser. ii., p. 23 et sea.
Ibid., p. 46.
"The Data of Geochemistry", by F. W. Clark, p. 20.
Ibid., p. 31.
Prof. H. A. Wilson has made a suggestive estimate of the thermal effects of radium enclosed in the central parts of the earth (NATURE, February 20, 1908).
See the account given by Schardt, Verhandl. Schhweizerischen Natrtrf. Gesellsch., 1904, lxxxvii., "Jahresversammlung", p. 204 et seq.
Schardt, loc. cit.
Trans. North of England Mining and Mec. Engineers, xxxiii., p. 25.
Proc. R.S., xli., p. 44.
Prof. C. Schmidt (Basel) has recently given reasons or the view that the Mesozoic schists of the Simplon at the period of their folding were probably from 15,000 to 20,000 metres beneath the surface ("Ec. Geol. Helvetiæ", vol. ix., No. 4. p 590). As another instance consider the compression of the Laramide range (Dawson, Bull. Geol. Soc. Am., xii., p. 87).
O.T.G.S., xlviii., p. 210.
Ibid., lviii., p. 354 et seq.
Phil. Mag., xxxv., p. 173.
Trans. R.D.S., vi., p. 208.
See Strutt, Proc. R S., lxxvii., p 482.
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FOURNIER, E. The Dublin Meeting of the British Association . Nature 78, 449–466 (1908). https://doi.org/10.1038/078449a0
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DOI: https://doi.org/10.1038/078449a0