Published online by Cambridge University Press: 01 May 2009
The object of this paper is an attempt to furnish proof of what JL has been a growing conviction in the mind of the writer, that the true age of the Dartmoor granite, and probably its associated line of bosses running south-westwards into Cornwall, might be referable to an interval or period of geological time between the Lower and the Upper Culm, or Carboniferous system.
page 509 note 1 Bead before Section C (Geology), British Association, September, 1898.
page 510 note 1 Vol. li (1895), p. 609.
page 512 note 1 Trans. Geol. Soc., ser. ii, vol. vi p. 457;Google Scholar Geol. Rep. of Cornwall, Devon, etc., p. 111.Google Scholar
page 512 note 2 Rep. Brit. Assoc., 1861, p. 127.Google Scholar
page 513 note 1 Quart. Journ. Geol. Soc., vol. xlv, p. 398, etc.Google Scholar