[143] Journal du Nord, St. Petersburg, 1807.
[144] Fleming, Ed. New Phil. Journ., No. xii. p. 285.
Bishop Heber informs us (Narr. of a Journey through the Upper Provinces of India, vol. ii. p. 166-219), that in the lower range of the Himalaya mountains, in the northeastern borders of the Delhi territory, between lat. 29° and 30°, he saw an Indian elephant of a small size, covered with shaggy hair. But this variety must be exceedingly rare; for Mr. Royle (late superintendent of the East India Company's Botanic Garden at Saharunpore) has assured me, that being in India when Heber's Journal appeared, and having never seen or heard of such elephants, he made the strictest inquiries respecting the fact, and was never able to obtain any evidence in corroboration. Mr. Royle resided at Saharunpore, lat. 30° N., upon the extreme northern limits of the range of the elephant. Mr. Everest also declares that he has been equally unsuccessful in finding any one aware of the existence of such a variety or breed of the animal, though one solitary individual was mentioned to him as having been seen at Delhi, with a good deal of long hair upon it. The greatest elevation, says Mr. E., at which the wild elephant is found in the mountains to the north of Bengal, is at a place called Nahun, about 4000 feet above the level of the sea, and in the 31st degree of N. lat., where the mean yearly temperature may be about 64° Fahrenheit, and the difference between winter and summer very great, equal to about 36° F., the month of January averaging 45°, and June, the hottest month, 81° F. (Everest on climate of Foss. Eleph., Journ. of Asiat. Soc., No. 25, p. 21.)
[145] See Dr. Buckland's description of these bones, Appen. to Beechy's Voy.
[146] Darwin, Journal of Travels in S. America, &c., 1832-36, in voyage of H. M. S. Beagle, p. 98. 2d Ed. London, 1845, p. 86.
[147] Darwin, Journal of Travels in S. America, &c., p. 99, 2d Ed. p. 85.
[148] Burchell, cited by Darwin, ibid. p. 101. 2d Ed. p. 87.
[149] Since the above passage was first printed in a former edition, June, 1835, it has been shown by the observations of Sir R. Murchison, M. de Verneuil, and Count Keyserling, and more recently by M. Middendorf (see above, p. [81]), that the Lowland of Siberia has actually been extended, since the existing species of shells inhabited the northern seas.
[150] Humboldt, Fragmens Asiatiques, tom. ii. p. 393.
[151] Reboul. Geol. de la Période Quaternaire, who cites Observ. sur la Sibérie, Bibl. Univ., Juillet, 1832.