Published online by Cambridge University Press: 01 May 2009
For some years geologists have more or less agreed in the view that the present features of the earth, whether hill, valley, or plain (with some small exceptions, as volcanic outbursts) have been formed directly by denudation; though indirectly disturbances, whether faults upheavals or sinkings, have of course had their effect in determining the flow, so to speak, of the denuding agent.
page 447 note 1 The title given by the editor to the short abstract in the Society's Journal (Vol. xxiii. p. 265) is not quite correct.Google Scholar
page 447 note 2 Hutton's Theory of the Earth, vol. ii. p. 238.Google Scholar
page 448 note 1 The Theory of the Earth, 2 vols., 8vo.; Edin., 1795.See especially vol. 1. p.304, and vol. ii. pp 3–5, 98, 99, 138–40, 143 (quotation from the French), 157, 205, 209, 210, 236, 245, 295, 296, 401, 466–8, 498, 528, 529, 534, 535, 547.Google Scholar
page 448 note 2 Illustrations of the Huttonian Theory, 8vo.; Edin., 1802. Reprinted in vol. i. of Playfair's Works, 1822. See pp. 105–7, 110–14, 373–6 of the original edition ═pp. 117–19, 122–5, 370–2 of the later one.Google Scholar
page 448 note 3 Memoir on the Geology of Central France, 4to., Lond., 1827. Ed. 2, 8vo., 1858 pp. 37, 38, 97, 158, 159, 205–9, 213, 244;Google Scholar and Geol. Mag., Vol. III. p. 193 (1866). Scrope, Mr. touched on the subject before in his “Consideration on Volcanos,” 8vo. Lond., 1825 (pp. 96, 97, 138, 139, 214, 215).Google Scholar
page 449 note 1 Essai, . sur la constitution géognostique des Pyrenees, 8vo., Paris, 1823, p. 25.Google Scholar
page 449 note 2 Rain and Rivers, 8vo, Lond., 1857. Ed. 2 in 1866.Google Scholar
page 449 note 3 Phil. Trans., vol. 154, p. 247;CrossRefGoogle Scholar Quart. Journ. Geol. Soc., vol. xix. p. 497 (1863).Google Scholar
page 449 note 4 Quart. Journ. Geol. Soc., vol. vi. p. 94 (1850); vol. vii. pp. 121–6, 130, 134 (1851); vol. xi. pp. 118, 119 (1855); vol. xiii. pp. 63, 71 (1857).Google Scholar
page 449 note 5 Ibid. vol.xviii. p.185 (1862); Phil. Mag., vol. 28, p. 293 (1864); vol 29, p. 285. (1865);CrossRefGoogle Scholar The Physical Geology and Geography of Gt. Britain, 8vo., Lond. Ed. 2. (1865).Google Scholar
page 449 note 6 Brit. Assoc. Rept. for 1861, Trans. of Sections, p. 54;Google Scholar Quart. Journ. Geol. Soc., vol. xviii. p. 378 (1862);Google Scholar Geol. Mag., vol. iii. p. 232 (1866), vol. iv. p. 444. (1867).Google Scholar
page 449 note 7 Bull. Soc. Geol., France, 2 Ser., t. xii. p. 314 (1855).Google Scholar
page 449 note 8 I believe that: Professor Ramsay started this argument against the marine origin of escarpments.—W. W.Google Scholar
page 450 note 1 Quart. Journ. Geol. Soc., vol. xxi. p. 443 (1865).Google Scholar
page 450 note 2 Geol. Mag., Vol. III. p. 435 (1866), and Vol IV. p. 184 (1867).Google Scholar
page 450 note 3 Notes of Travel by Vacation Tourists, 1861.—The Geology and Scenery of Scotland, (1865).Google Scholar
page 450 note 4 Geol. Survey Memoir on Sheets 81 N.W. and S.W., P. 86 (1866).Google Scholar
page 450 note 5 Geol. Mag., Vol. III. pp. 344, 439, 575 (1866).Google Scholar
page 450 note 6 Quart. Journ. of Science, vol. iv. p. 33 (1867).Google Scholar
page 450 note 7 Mem. Geol. Survey, India, vol. v. p. 201 (1866)Google Scholar.—Geol. Mag., Vol. IV. pp. 3, 345 (1867).Google Scholar
page 450 note 8 Quart. Journ. Geol. Soc., vol. xvii. p. 1 (1861).Google Scholar
page 450 note 9 United states Exploring Expedition during the Years 1838–1842, vol. x., Geology, 4to., Philadelphia, 1849, pp. 384–92, 526–33, 670–7.Manual of Geology, 8vo., Philadelphia, 1863, pp. 635–42, 676.Google Scholar
page 450 note 10 Quart. Journ. Geol. Soc., vol. xx. pp. 125, 126, 128–30 (1864), where references to the author's other notes on the subject are given.Google Scholar
page 450 note 11 Notes on a Map to Illustrate Five Types of Earth-Surface, 4to., Philadelphia, 1866.Google Scholar
page 450 note 12 Geol. Survey, Canada—Rept. of Progress to 1863, 8vo.,Google Scholar Montreal, p. 889.Google Scholar
page 450 note 13 Part 3 (Geology) of Lieut. Ives' Eeport on the Colorada Eiver of the West 1861. References to other remarks on denudation by this author are given in Professor Hind's paper referred to above.
page 450 note 14 Report on the Geological Survey of the State of Wisconsin, vol. i, pp. 117–26 (1862).Google Scholar
page 450 note 15 Report on the Geology of Canterbury, New Zealand;—andGoogle Scholar Quart. Journ. Geol. Soc., vol. xxi. pp. 129, 130 (1865).Google Scholar
page 450 note 16 Quart. Journ. Geol. Soc., vol. xx. p. 463 (1864)–in abstract only. The paper has been printed in full in Trans.Google Scholar Nova Scotian Institute of Nat. Sci., Vol. I. part iv. p. 91.Google Scholar
page 450 note 17 Geol. Mag., Vol. III. p. 88 (1866).Google Scholar
page 451 note 1 It would be overburdening this paper with foot-notes were I to acknowledge the many sources whence some of the following arguments have been in great part derived; enough to refer the reader to the list of authors given before. I would gladly have quoted largely from Hutton, Playfair, Scrope, and others, but the paper would have been much lengthened thereby.
page 452 note 1 Geol. Mag. Vol. II., p. 26. (1865.)Google Scholar
page 452 note 2 1865. pp 351–5. As Sir Charles does not now hold that these needless are signs of the action of the sea (see before, p. 449), it might be thought needless here to controvert that idea. However, as it is contained in the last edition of his “Elements,” a work constantly referred to by geologists, I have let this paragraph stand.Google Scholar
page 453 note 1 Geol. Mag., Vol. III. p. 571.Google Scholar
page 453 note 2 Hutton, , “Theory of the Earth,” vol. ii. p. 367.Google Scholar
1 Professor Ramsay has noticed the great thickness of solid rock that must have been denuded in Wales (Mem. Geol. Surv. vol. i. p. 297, and plates. 4, 5, 1846; and vol. iii. p. 236, and pl. 28, 1866). I believe that the former of these was the first attempt at showing the vast amount of denudation that has taken place.Google Scholar