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File:The Quarterly journal of the Geological Society of London (1918) (14596443020).jpg

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Identifier: quarterlyjourna741918geol (find matches)
Title: The Quarterly journal of the Geological Society of London
Year: 1845 (1840s)
Authors: Geological Society of London
Subjects: Geology
Publisher: London (etc.)
Contributing Library: Smithsonian Institution Libraries
Digitizing Sponsor: Biodiversity Heritage Library

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rpe of sediment, on the one side, and the Welsharea, where the corresponding rocks are of an argillaceous character,on the other. 1 One-inch (Old Series) Sheet 56; also Sheets 50, 61, & 55. 2 Q. J. G. S. vol. lxii (1906) p. 195. 3 Silurian System vol. i (1839) pp. 195 et seqq.; Siluria 4th ed. (1867)pp. 123 et seqq. Q. J. G. S. No. 295. s 222 MR. E. D. STAMP ON THE HIGHEST (vol. lxxiv, This paper is concerned, then, with a small portion of the largearea of highest Silurian rocks of the Welsh Borderland, and thedistrict was selected as near as possible to the typical Ludlowarea, consistent with being on the western side of the great fault.The district, indicated on the sketch-map (fig. 1), comprising the Fig. 1.— Geological sketch-map of the Welsh Borderland.
Text Appearing After Image:
_! Pre-Wenlock Wenlock Ludlow with Aymestry Limestone Old RedSandstone Scale:-SMiles=1 Inch or 1:506,8802 4 6 8 10 12 14 16 (I=Ludlow district, investigated by Miss G. L. Elles &Miss I. L. Slater. II = Bucknell district.) greater part of the basin of the River Redlake (a tributary ofthe Teme), has been mapped on the 6-inch scale. The ground isshown on the 6-inch Ordnance Survey maps, quarter-sheetsShropshire 69 S.W., 69 S.E., 76 N.W., 76 N.E., 76 S.W., 76 S.E..77 N.W., and 77 S.W. part 3) stlurian rocks of the clun-fobest district. 223 Previous Work. The country was mapped on the 1-inch scale by the GeologicalSurvey in 1819,l and a horizontal section 2 is taken almost alongthe line of the Bedlake Valley. No descriptions were published,and Jukes-Browne,3 writing in 1912, sums up the informationconcerning the district in these words : In the country round Kington, Clun, and Radnor Forest these graptoliticshales (Lower Ludlow) are succeeded by a great thickness of brownish sandyshale

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Volume
InfoField
1918
Flickr tags
InfoField
  • bookid:quarterlyjourna741918geol
  • bookyear:1845
  • bookdecade:1840
  • bookcentury:1800
  • bookauthor:Geological_Society_of_London
  • booksubject:Geology
  • bookpublisher:London__etc__
  • bookcontributor:Smithsonian_Institution_Libraries
  • booksponsor:Biodiversity_Heritage_Library
  • bookleafnumber:389
  • bookcollection:biodiversity
  • BHL Collection
  • BHL Consortium
Flickr posted date
InfoField
30 July 2014


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