[423] Webster, Geol. Trans. vol. ii. p. 192, 1st series.

[424] Mantell, Geology of Sussex, p. 293.

[425] See Palmer on Shingle Beaches, Phil. Trans. 1834, p. 568.

[426] Groins are formed of piles and wooden planks, or of fagots staked down and are used either to break the force of the waves, or to retain the beach.

[427] Redman as cited, p. 315.

[428] Rob. A. C. Austen on the Valley of the English Channel, Quart. Journ. G. S. vol. vi. p. 72.

[429] See Palmer on Motion of Shingle Beaches, Phil. Trans. 1834, p. 568; and Col. Sir W. Reid, Papers of Royal Engineers, 1838, vol ii. p. 128.

[430] De la Beche, Geolog. Manual, p. 82.

[431] According to the measurement of Carpenter of Lyme.

[432] Rev. W. D. Conybeare, letter dated Axminster, Dec. 31, 1839.