^{page 339 note 2} Such crystalline magnesite occurs in Ceylon, as at Randeniya, Wellawaya. It occurs also in various parts of North America (see Dana's, System of Mineralogy, 6th ed., p. 275Google Scholar) and elsewhere.

^{page 339 note 1} Woodward, , Geol. Mag., Dec. III, Vol. II, p. 352, Pl. IX, Figs. 7–s0, 1885Google Scholar; Reed, Ibid., Dec. V, Vol. IV, p. 113, Pl IV, Fig. 12, 1907.

^{page 339 note 2} Such crystalline magnesite occurs in Ceylon, as at Randeniya, Wellawaya. It occurs also in various parts of North America (see Dana's, System of Mineralogy, 6th ed., p. 275Google Scholar) and elsewhere.

^{page 340 note 1} It is convenient to use the name chondrodite in a general sense for the members of the humite series when dealing with scattered granules in these rocks, since it is not practicable to identify any given irregular small grain with safety as belonging to any particular member of the series.

^{page 340 note 2} See particularly The Geological Structure of the North-West Highlands (Memoirs of the Geological Survey of Great Britain), pp. 453–62, 1907.Google Scholar

^{page 340 note 3} Loc. cit.

^{page 340 note 4} The Tertiary Igneous Rocks of Skye (Mem. Geol. Surv.), pp. 144–51, 1904.Google Scholar

^{page 340 note 6} Q. J. G. S., vol. lxvi, p. 507, 1910.Google Scholar

^{page 341 note 1} This is a specimen of the Ceylon Mineral Survey collection at the Imperial Institute.

^{page 342 note 1} These peculiar intergrowths of dolomite in calcite appear to be identical with those described and figured by Coomaraswamy (“Crystalline Limestones of Ceylon”: Q. J. G. S., vol. lviii, p. 412, 1902Google Scholar).

^{page 343 note 1} Geology of the Haliburton and Bancroft Areas, Province of Ontario. Adams, F. D. & Barlow, A. E., Memoir No. 6, Department of Mines, Canada, p. 214, 1910.CrossRefGoogle Scholar

^{page 344 note 1} “Petrology of Chhindwára”: Rec. Geol. Surv. Ind., vol. xxxiii, pt. iii, 1906.Google Scholar