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III.—On Accumulation and Denudation, and their Influence in Causing Oscillation of the Earth’s Crust

Published online by Cambridge University Press:  01 May 2009

Extract

The Carboniferous Limestone of the north-west of England was formed in a bay separated from another marine area farther south by a narrow isthmus and promontory never submerged, extending, as Professor Jukes pointed out, in “a band of country running east and west across England from Leicestershire, through Warwickshire, South Staffordshire, North Shropshire into Montgomeryshire,” and to the mountainous district of North Wales.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1883

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References

page 348 note 1 Oebbeke, Beiträge zur Petrographie der Philipinen und der Palan-Inseln, Neues Jahrbueh, I. Beilage Band, p. 451.

page 348 note 2 That portion of this isthmus, situated between Coalbrookdale and the Clee Hills, was sixteen miles wide at the termination of the deposition of the Carboniferous Limestone, and was reduced to twelve miles during that of the Millstone Grit.

page 348 note 3 Memoirs of the Geological Survey, The South Staffordshire Coal-field; by J. Beete Jukes, F.R.S., p. xii. See also Jukes's Manual of Geology, second edition, p. 518.

page 348 note 4 Professor J. Phillips recognized that “they were confined to valleys in the slate formation, and never follow that rock to its escarpments on high ground.”—Geology of Yorkshire, part ii., p. 13.

page 348 note 5 Mem. Geol. Survey, Geology of Kendal, etc., W. T. Aveline, F.G.S., p. 14; [Prof.] T. McK. Hughes, F.S.A., p. 15; of Kirkby Lonsdale [Prof.] Hughes, p. 16. On the Carboniferous Conglomerates of the Basin of the Eden, by J. G. Goodchild, Quart. Journ. Geol. Soc. vol. xxx. p. 396.

page 349 note 1 The Double Delta of the Whang-Ho, by Samuel Mossman, Geographical Magazine, vol. v. p. 92.

page 349 note 2 Geological Survey, Vertical Sections, No. 23.

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page 349 note 4 Morton op. cit., p. 81.

page 349 note 5 Morton, op. cit. pp. 39 and 75.

page 350 note 1 Mem. Geol. Survey, North Derbyshire, p. 18.

page 350 note 2 Geology of Yorkshire, by John Phillips, F.R.S., part ii. p. 176.

page 350 note 3 Geological Survey, Vertical Sections, No. 23.

page 350 note 4 Under the local definition of Cefn-y-Fedw Sandstone, op. cit. p. 51.

page 350 note 5 Fig. 37, Comparative Sections of thethe Millstone Grit and Yoredale Rocks, Mem. Geol. Survey, North Derbyshire, p. 139.

page 351 note 1 Geological Survey, Vertical Sections, No. 23.

page 351 note 2 The Coalfields of Great Britain, by Edward Hull, F.G.S., second edition, p. 96.

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