The Flint Flakings of the Weybourne Crag

^{page 309 note 1} Warren, S. H., Proc. Geol. Assoc., vol. xxxiv, 1923, p. 173.

^{page 309 note 2} Haward, F. N., Proc. Prehift. Soc. East Anglia, vol. iii, 1919, p. 139.

^{page 309 note 3} It will be gathered that I take the Crag flakings which are found together as an associated group of common origin, just as one takes the flakings from Chelles, Milton Street, or Le Moustier. Some authorities select a few of the Crag flakes with chipped edges while rejecting the rostro-carinates, with most of their associates. This appears to me equivalent to selecting a few of the scrapers from Grimes Graves for acceptance, while rejecting the axes, cores, etc., from which (broadly speaking) the flakes were struck off. Let it be granted that nature has made nineteen of the flakings, then she can equally make the twentieth, which is a little more attractive.

^{page 310 note 1} For the frictional group characters, vide Proc. Geol. Assoc., vol. xxxiv, 1923, pp. 156–60, etc.

^{page 311 note 1} For a fuller explanation, vide Journ. R. Anthrop. Inst., vol. xliv, 1914, p. 412; Proc. Geol. Assoc., vol. xxxiv, 1923, p. 39, and p. 153.

^{page 311 note 2} Haward, F. N., Proc. Prehist. Soc. E. Anglia, vol. i, 1912, p. 189, etc.; vol. iii, 1919, p. 137; also S. H. Warren, as under 1.

^{page 311 note 3} For a fuller explanation of a “ complete ” or “ incomplete ” group of flakings, vide Proc. Geol. Assoc., vol. xxxiv, 1923, p. 171.