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Essay on New Spain," volume i., page 62. Santa Cruz and Barbadoes, Prof. Hovey, "Silliman's Journal", volume xxxv., page 74. St. Domingo, Courrojolles, "Journ de Phys." tom. liv., page 106. Bahamas, "United Service Journal", No. lxxi., pages 218 and 224. Jamaica, De la Beche, "Geol. Man." page 142. Cuba, Taylor in "Lond. and Edin. Mag." volume xi., page 17. Dr.
Schröter's final result in 1811 was 23h. 21m. 7·977s. Monat. Not., vol. lvii., p. 402; Astr. Phys. Roy. Astr. Nach., No. 2,021; Am. Spettr. Ital., Dicembre, 1882; Am. Ass., 1873, p. 407. Nach., No. 2,809; f. Nach., No. 3,097; Phil. Trans., vol. clxxxvi., A., p. 469; Proc. Roy. Geol. Soc., vol. iii. Mag., vol. xxviii. Wien, Bd. lxiv.; quoted by Poynting. Cf. The Moon, by T. Gwyn Elger, p. 20.
Richardson's paper on Scottish earthquakes, Trans. Edin. Geol. Soc., vol. vi. p. 194 . Volcanic phenomena are the outward manifestations of forces deep-seated beneath the crust of the globe; and in seeking for the causes of such phenomena we must be guided by observation of their nature and mode of action.
Americ.: Birds, pp. 343 and 359; Major W. Ross King, 'The Sportsman in Canada, 1866, p. 156; Mr. Haymond, in Prof. Cox's 'Geol. Survey of Indiana, p. 227; Audubon, 'American Ornitholog. Biograph. vol. i. p. 216. On the Kalij-pheasant, Jerdon, 'Birds of India, vol. iii. p. 533. On the Weavers, Livingstone's 'Expedition to the Zambesi, 1865, p. 425.
Geol. Soc., vol. xxvii. p. 279; also, "History of Volcanic Action in British Isles," Trans. Roy. Soc. Edin. ; Judd, "On the Ancient Volcanoes of the Highlands," etc., Quart. Journ. Geol. Soc., vol. xxx. p. 233; and Volcanoes, p. 139. Brit. Assoc. Rep. for 1850, p. 70. Judd, Quart. Jour. Geol. Soc., vol. xxx. p. 242. History of Volcanic Action, etc., loc. cit. p. 153, et seq.
"This apparently is true not only of the segments of thrust surface beneath eastern Flattop, Yellow, and Chief Mountain, but also of the more deeply buried portions which appear to dip with the Algonkian strata into the syncline. While observation is not complete, it may be assumed on a basis of fact that thrust surfaces and bedding are nearly parallel over extensive areas." Geol.
It will be preferable to turn to the positive facts of palaeontology, and to inquire what they tell us. Journ. Geol.
Rain and river action, supplemented by that of glaciers, have also had a share in eroding channels and wearing down the upper surface of the ground, with the result we at present behold in the wild and broken scenery of the Inner Hebrides and adjoining coast. Geikie, loc. cit., p. 178; also Quart. Jour. Geol. Soc., vol. xxvii. p. 303.
The evidence on which such conclusions are based is of two kinds, negative and positive. Journ. Geol. It will be preferable to turn to the positive facts of paleontology, and to inquire what they tell us.
W. J. Hoffman, at that time connected with the Hayden Survey, published descriptions of the so-called Montezuma well and of a large cliff ruin on Beaver creek, the latter accompanied by an illustration. The descriptions are slight and do not touch the region herein discussed. Rep. U.S. Geol. The first publication of importance to the present inquiry is a short paper by Dr.
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