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Published online by Cambridge University Press: 01 May 2009
The fluctuations which take place from time to time in the lengths of glaciers are extremely interesting to the glaciologist; for there are good reasons for believing that the meteorological conditions which give rise to the lesser oscillations of glaciers are generally of the same character as those which produced the great secular changes of climate which occurred in past ages.
page 337 note 1 Hess, Hans, Die Gletscher, 1904, p. 210.Google Scholar
page 338 note 1 Die Gletscher, 1904, p. 84.Google Scholar
page 338 note 2 Heat considered as a mode of motion, chap. vi.Google Scholar
page 339 note 1 Peterman's Mitteilungen, i, pp. 57–60, 1911, and Pet. Mitt. Ergangungsheft, No. 173, Gotha, 1912.Google Scholar
page 340 note 1 The Alps in the Ice Age, p. 1141 et seq.Google Scholar
page 341 note 1 The Quaternary Ice Age, p. 146.Google Scholar