A Manual of Elementary Geology / or, The Ancient Changes of the Earth and its Inhabitants as Illustrated by Geological Monuments

by Sir Charles Lyell

[233-D] Fitton, ibid.

[233-E] Buckland and De la Beche, Geol. Trans., Second Series, vol. iv. p. 16. Mr. Forbes has ascertained that the subjacent rock is a freshwater limestone, and not a portion of the Portland oolite, as was previously imagined.

[234-A] E. Forbes, ibid.

[235-A] See Principles of Geol., 8th ed. pp. 260-268.

[235-B] Ibid. p. 443.

[237-A] Fitton, Geol. of Hastings, p. 58.; who cites Lander's Travels.

[237-B] See above, p. 85.; and Second Visit to the U. S. vol. ii. chap. xxxiv.

[237-C] See the Author's Anniv. Address, Geol. Soc. 1850, Quart. Geol. Journ. vol. vi. p. 52.

[241-A] An account of these cliffs was read by the author to the British Assoc. at Glasgow, Sept. 1840.

[241-B] Seine-Inferieure, p. 142. and pl. 6. fig. 1.