We use cookies to distinguish you from other users and to provide you with a better experience on our websites. Close this message to accept cookies or find out how to manage your cookie settings.
Published online by Cambridge University Press: 01 May 2009
The classification set forth in this paper is founded essentially on an examination of the junction-beds between the Silurian and the Devonian in the field. All the localities described have been studied personally by the writer, and in most cases the actual junction has been mapped on the 6-inch scale. The names of localities are taken from the 6-inch Ordnance Survey maps, the sheet number being quoted in each case.
page 333 note 1 Lapworth, & Watts, , “Shropshire” in “Geology in the Field”: Jub. Vol. Geol. Assoc., 1910, p. 756.Google Scholar
page 333 note 2 Elles, & Slater, , op. cit., p. 204.Google Scholar
page 333 note 3 Stamp, , op. cit., supra, 1918.Google Scholar
page 334 note 1 Trans. Caradoc Field Club, vol. i, pt. iv, issued for 1896, 1897, pp. 181–3.Google Scholar
page 334 note 2 In this and all other tabulated successions the rocks are Downtonian unless otherwise stated.
page 335 note 1 Op. cit., p. 209.Google Scholar
page 335 note 2 To economize space by avoiding the repetition of fossil names, the fossils recorded are indicated by numbers referring to the lists in a later section.
page 336 note 1 Stamp, , op. cit., 1918, p. 238.Google Scholar
