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John F. W. Herschel in his Discourse on Natural Philosophy, published in 1830. In preceding works the gradual diminution of the earth's central heat was almost the only cause assigned for the acknowledged diminution of the superficial temperature of our planet. [166] We are indebted to Baron Alex. von Humboldt for having first collected together the scattered data on which he founded an approximation to a true theory of the distribution of heat over the globe. Many of these data were derived from the author's own observations, and many from the works of M. Pierre Prevost, of Genera, on the radiation of heat, and from other writers.--See Humboldt on Isothermal Lines, Mamoires d'Arcueil, tom. iii. translated in the Edin. Phil. Journ. vol. iii. July, 1820. The map of Isothermal Lines, recently published by Humboldt and Dove (1848), supplies a large body of well-established data for such investigations, of which Mr. Hopkins has most ably availed himself in an essay "On the Causes which may have produced Changes in the earth's Superficial Temperature."--Q. Journ. Geol. Soc. 1852, p. 56. [167] Sir J. Richardson's Appendix to Sir G. Bach's Journal, 1843-1845, p. 478. [168] Malte-Brun, Phys. Geol. book xvii. [169] On Isothermal Lines, &c. [170] Rennell on Currents, p. 96. London, 1832. [171] Ibid. p. 153. [172] Ibid. p. 25. [173] Scoresby's Arctic Regions, vol. i. p. 208.--Dr. Latta's Observations on the Glaciers of Spitzbergen, &c. Edin. New Phil. Journ. vol. iii. p. 97. [174] Rennell on Currents, p. 95. [175] Humboldt on Isothermal Lines. [176] Journ. of Travels in S. America, &c. p. 272. [177] Darwin's travels in S. America, p. 271. [178] Mr. Hopkins raises the question whether, in South Georgia, the descent of glaciers to the margin of the sea might not have been mistaken by Capt. Cook for the descent of the snow-line to the sea level. Quart. Journ. Geol. Soc. p. 85, 1852. The great navigator is generally very accurate, and there seem to be no observations of more recent date either to confirm or invalidate his statements. [179] After all these modern discoveries, the area still unexplored, within the antarctic circle, is more than double
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