Transactions of the Federated Institution of Mining Engineers Volume 11
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Transactions of the Federated Institution of Mining Engineers Volume 11

Transactions of the Federated Institution of Mining Engineers Volume 11


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This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1896 Excerpt: ...245. At Shireoaks colliery, the Permian rocks are 196 feet; at Best wood, where they are overlain by the Bunter, only 120 feet thick; at Clifton they have disappeared altogether. From the map and section accompanying Mr. Coke's paper, he (Mr. de Ranee) had plotted the accompanying longitudinal section (Fig. 3, Plate XIX.), adopting the scales there used, which clearly showed that the tilting of the Coal-measures tpok place before the Permians were deposited; that both formations were extensively denuded before the Triassic rocks were deposited; and that this denudation increased southwards at a very rapid rate, and so that the surface of the Coal-measures dips rapidly south, or in an opposite direction to the dip of the measures themselves, the intervening vertical space being filled in with Triassic rocks of an increased thickness. It would appear probable that this disposition of comparative levels is entirely due to a series of faults throwing down the strata southwards, and it is clearly established that these faults are of newer date than the Triassic formation, and, consequently, Prof. Hull is probably correct as to the Permians thinning out against the uprise of old Palaeozoic rocks. Mr. J. Bagnold Smith (Newstead) wrote that Mr. Coke's information and deductions seem to be very correct and of great interest. If the approximate line of outcrop be correct, it gives a knowledge of it from north of Eckington of the Brimington anticlinal to south of Nottingham. When read in conjunction with Prof. Riicker and Thorpe's Bakerian lecture of 181)0 it presents features of great interest in connexion with the magnetic ridge-lines, which show folds in the primary igneous rocks, and these folds are nearly related to the contour of various coal-basins and the lie ...


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Product Details
  • ISBN-13: 9781231912553
  • Publisher: Rarebooksclub.com
  • Publisher Imprint: Rarebooksclub.com
  • Height: 246 mm
  • No of Pages: 344
  • Spine Width: 18 mm
  • Width: 189 mm
  • ISBN-10: 1231912553
  • Publisher Date: 01 May 2012
  • Binding: Paperback
  • Language: English
  • Returnable: N
  • Weight: 617 gr


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