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The structure of mountain ranges has always been difficult to understand. They often show that peculiarly complicated disturbances of strata have occurred in the process of their formation. Mountain ranges in many stages of dissection are to be seen in various parts of the world; but the better knowledge which their study has furnished us with has not, at the moment, always assisted us in the better understanding of the problem of mountain building.
page 111 note 1 Mountains, their Origin, Growth, and Decay, 1913, p. 66.Google Scholar
page 111 note 2 Ibid., p. 130.
page 112 note 1 Ibid., p. 173.
page 113 note 1 Deeley, R. M., “Trail and Underplight”: Geol. Mag., Dec. VI, Vol. III, pp. 2–5, 1916.CrossRefGoogle Scholar
page 113 note 2 “The Structure of the Himalayas”: Geol. Survey of India, vol. xlii, pt. ii, p. 122.Google Scholar
page 114 note 1 Glaciers of the Alps, 1860, p. 9.Google Scholar
page 118 note 1 Presidential Address, Brit. Ass. Rep., 1910, p. 54Google Scholar.
