^{page 310 note 1} See Molengraaff, G. A. F., “Geology of the Transvaal,” Edinburgh, 1904, p. 66.Google Scholar

^{page 311 note 1} “Report on the Geology of Cornwall, Devon, and West Somerset,” 1839, p. 204.Google Scholar

^{page 311 note 2} “The Red Sandstones, Conglomerates, and Marls of Devonshire,” pt. ii: Ann. Rept. and Trans. Plymouth Inst., 1862-1863, p. 30.Google Scholar

^{page 311 note 3} “The Igneous Constituents of the Triassio Breccias and Conglomerates of South Devon”: Quart. Journ. Geol. Soc., 1890, pp. 71, 72.Google Scholar

^{page 311 note 4} See Plate XXI, Fig. 1.

^{page 311 note 5} Pengelly describes and figures false bedding at Slapton, Start Bay, and Goodrington Sands, Torbay: Trans. Plymouth Inst., 1862–3, p. 31.

^{page 311 note 6} See Ussher, W. A. E., Geol. of Torquay: Geol. Survey Mem., 1903, pp. 110, 111.Google Scholar

^{page 312 note 1} See Plate XXI, Fig. 2, and for section of Petit Tor see W. A. E. Ussher, Geol. of Torquay, Geol. Survey Mem., 1903, p. 109; and “Coast Section from Babbacombe to Watcombe,” by Ussher, W. A. E., Proc. Geol. Assoc., vol. xvi (1900), p. 434.Google Scholar

^{page 312 note 2} Ussher, W. A. E., “On the Age and Origin of the Watcombe Clay”: Rept. and Trans. Devon Assoc. Adv. Sci., ix (1877), p. 298Google Scholar; also section in Proc. Geol. Assoc., xvi, p. 434.

^{page 313 note 1} Quart. Journ. Geol. Soc., p. 496.

^{page 313 note 2} Ussher, & Teall, , Geol. of Exeter: Geol. Survey Mem., 1902, p. 78.Google Scholar

^{page 313 note 3} Quart. Journ. Geol. Soc., 1890, p. 76.Google Scholar

^{page 313 note 4} Geol. of Torquay: Geol. Survey Mem., 1903, p. 112.Google Scholar

^{page 313 note 5} Conybeare, Rev. J. J., “On the Red Rock Marle, or Newer Red Sandstone”: Annals of Philosophy, n.s., vol. i (1821), p. 257;Google Scholar Conybeare, & Phillips, , Geol. England and Wales, pt. i (1822), p. 294;Google Scholar also Ussher, , Geol. of Torquay, 1903, p. 111, line 4.Google Scholar

^{page 314 note 1} See Ormerod, G. W., “On the Murchisonite Beds of the Estuary of the Ex, and an attempt to classify the Beds of the Trias thereby”: Quart. Journ. Geol. Soc., 1875, p. 349Google Scholar, and section from Minnicombe to Lympstone, fig. 3.

^{page 315 note 1} Very likely a minute search might discover some.

^{page 315 note 2} Pengelly, says: “The pebbles lie with their longest axes parallel to the planes of bedding” (“The Red Sandstones, etc., of Devonshire,” pt. ii: Ann. Rept. and Trans. Plymouth Inst., 1862-1863, p. 31).Google Scholar

^{page 316 note 1} “The Great Ice Age,” 3rd ed. (1894), p. 274.Google Scholar

^{page 316 note 2} Quart. Journ. Geol. Soc., 1890, p. 75Google Scholar, item 29.

^{page 317 note 1} “The Petrography of Dartmoor and its borders”: Trans. Devon. Assoc. Adv. Sci., vol. xxxiv (1902), p. 519.Google Scholar

^{page 317 note 2} Quart. Journ. Geol. Soc., 1892, p. 506.Google Scholar

^{page 317 note 3} “Morphologie der Erdoberfläche” (1894), vol. i, p. 280Google Scholar, line 18.

^{page 318 note 1} “Die Erde und das Leben” (1902), vol. ii, p. 86.Google Scholar

^{page 318 note 2} “Textbook of Geology,” 3rd ed (1893), p. 376; 4th ed (1903), p. 487.Google Scholar

^{page 318 note 3} “The Red Sandstones, Conglomerates, and Marls of Devonshire,” part ii: Ann. Rept. and Trans. Plymouth Inst., 1862-1863, p. 31.Google Scholar

^{page 318 note 4} Loc. cit., p. 29.

^{page 318 note 5} Same paper, part iii (1864–5), p. 40.

^{page 318 note 6} “On the Triassic Rocks of Somerset and Devon”: Quart. Journ. Geol. Soc., 1876, p. 392.Google Scholar

^{page 318 note 7} Loc. cit., p. 45.

^{page 318 note 8} “Elements of Geology,” 6th ed. (1865), p. 18.Google Scholar

^{page 318 note 9} “The Building of the British Isles,” 2nd ed (1892), p. 168.Google Scholar

^{page 318 note 10} Proc. Geol. Assoc., vol. xvi (1900), p. 434.Google Scholar

^{page 319 note 1} See also Irving, Rev. Dr. A., Quart. Journ. Geol. Soc., 1888, p. 157.Google Scholar

^{page 319 note 2} Pengelly, (Trans. Plymouth Inst., 1862-1863, p. 29)Google Scholar gives the dip at Ness Point as 5° to N. 129 E. mg. = E. 15½° S. true.

^{page 319 note 3} Ussher, , “Geology of Exeter”: Geol. Survey Mem., 1902, p. 59.Google Scholar Hobson, B., “Basalts and Andesites of Devonshire, etc.”: Quart. Journ. Geol. Soc., 1892, p. 500.Google Scholar