Hostname: page-component-586b7cd67f-l7hp2 Total loading time: 0 Render date: 2024-11-28T17:10:58.235Z Has data issue: false hasContentIssue false
  • English
  • Français

II.—The Uppermost Silurian and Old Red Sandstone of South Staffordshire

Published online by Cambridge University Press:  01 May 2009

W. Wickham King  and
W. J. Lewis
Get access Rights & Permissions [Opens in a new window]

Extract

2. The Downton Castle or Yellow Sandstones (see Figs. 2 and 3).— These occur at Lye and Turners Hill, but the best sections are at Saltwells. There the lowest beds are 10 feet of brown yellow and blue soft sandy mudstones (see Fig. 2, Ea), seen resting on the Ludlow Bone-bed, north of the Tram Bridge. Like the same zone at Ludlow, they are practically unfossiliferous.

Type
Original Articles
Information
Geological Magazine , Volume 9 , Issue 11 , November 1912 , pp. 484 - 491
Copyright
Copyright © Cambridge University Press 1912

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

page 485 note 1 The Silurian Brachiopoda, pp. 35, 36.Google Scholar

page 488 note 1 Silurian System, 1839, p. 478.Google Scholar The lower part of the Carboniferous beds set out in this section crop out in Black Brook.

page 489 note 1 South Staffs Coalfields, 2nd ed., p. 80.Google Scholar

page 489 note 2 Q.J.G.S., vol. lxii, p. 195, 1896.Google Scholar

page 489 note 3 Jukes-Browne's, Historical Geology, 1st ed., p. 121.Google Scholar