Hostname: page-component-848d4c4894-x24gv Total loading time: 0 Render date: 2024-05-19T00:49:31.083Z Has data issue: false hasContentIssue false
  • English
  • Français

On the Occurrence of Pre-Cambrian Shale in Guernsey

Published online by Cambridge University Press:  01 May 2009

George Horace Plymen
Get access Rights & Permissions [Opens in a new window]

Extract

It was noted by the Rev. C. Noury in 1886 that sedimentary rocks were found in a small coastal area to the south of Fort Pezerie, on the south-western extremity of Guernsey. Professor T. G. Bonney observed the same area independently in September, 1910, after describing it in field notes in 1888 as a closejointed and rather schistose diabase. The Rev. E. Hill in 1884 had also regarded the rock in this area as constituting a dyke-formed diabase.

Type
Original Articles
Information
Geological Magazine , Volume 59 , Issue 10 , October 1922 , pp. 468 - 469
Copyright
Copyright © Cambridge University Press 1922

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 468 note 1 Phillips, J., Geology of Yorkshire, vol. ii, “The Mountain Limestone,” 1836, p. xi, fig. 7.Google Scholar

page 468 note 2 Davidson, , op. eit., ii, pl. xiv, figs. 1–4.Google Scholar

page 468 note 3 Ibid., ii, pl. xxvii, fig. 2.

page 468 note 4 Géologie de Jersey, par. R. P. Ch. Noury, S.J. 1886.Google Scholar

page 468 note 5 Quart. Journ. Geol. Soc., vol. lxviii, 1912, p. 47.Google Scholar

page 468 note 6 Quart. Journ. Geol. Soc., vol. xl, 1884, p. 417.Google Scholar