The Geology of the Country Between Derby, Burton-On-Trent, Ashby-de-La-Zouch and Loughborough; (Explanation of Sheet 141) download torrent
The Geology of the Country Between Derby, Burton-On-Trent, Ashby-de-La-Zouch and Loughborough; (Explanation of Sheet 141) download torrent

The Geology of the Country Between Derby, Burton-On-Trent, Ashby-de-La-Zouch and Loughborough; (Explanation of Sheet 141). Charles Fox-Strangways

The Geology of the Country Between Derby, Burton-On-Trent, Ashby-de-La-Zouch and Loughborough; (Explanation of Sheet 141)
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Author: Charles Fox-Strangways
Number of Pages: 26 pages
Published Date: 21 May 2012
Publisher: Rarebooksclub.com
Publication Country: United States
Language: English
ISBN: 9781236349859
File Name: The.Geology.of.the.Country.Between.Derby,.Burton-On-Trent,.Ashby-de-La-Zouch.and.Loughborough;.(Explanation.of.Sheet.141).pdf
Download Link: The Geology of the Country Between Derby, Burton-On-Trent, Ashby-de-La-Zouch and Loughborough; (Explanation of Sheet 141)
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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. 1905 Excerpt: ... Geol, Soc, vol. lix., p. 311. t See Appendix p. 54. The great beauty of the scenery about Bretby Park and Repton Shrubs is mainly owing to the outcrop of these rocks. Lower Keuper Sandstone And Marls. The Lower Keuper Sandstone and Marls vary in thickness from about one hundred to nearly fifty feet, being thickest in the south and thinning northwards. They are composed of beds of pink and wnite sandstone with bands of marl. The sandstones occasionally, as about Burton, are fairly massive. At the base they contain beds of breccia which are well seen at Castle Donington and other places, but become most marked on the flanks of the Charnwood Hills, about Thringston and Grace Dieu. Sometimes the beds contain a considerable amount of bitumen; this was well shown in cutting the road at Bearwood Hill, Burton, where the hollows containing this mineral were about two inches in diameter. This bituminous bed appears to occupy a definite horizon which can be traced in the neighbourhood of Winshill and Bladon. The upper part of these beds is much more marly, and it is difficult to fix a division between them and the overlying Keuper Marl. At Weston Cliff, opposite Donington Park, footprints of Labyrinthodon have been found in these sandstones. In the south-west corner of the map the Lower Keuper Sandstone covers a considerable area, and in the neighbourhood of Caldwell the branch line to Netherseal Colliery cuts through these beds exposing several sections in massive sandstones with marly bands having a general dip of about 5 to the south-west. North of this the outcrop forms a narrow strip above the Bunter Pebble Beds as far as Brizlincote Hall, where it turns down the valley to the west towards Stapenhill; and, extending along the side of the Trent, forms the lower ...

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