[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.