Page:Transactions of the Geological Society, 1st series, vol. 1.djvu/193

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of Devonshire and Cornwall.
181

down into the plain on the eastern side,[1] were accumulated there, and again consolidated by the waters, thus affording those beds of conglomerate which have been already noticed in the course of this memoir.

  1. Does not the weight of the substances included in the conglomerate, described p. 98. seem to give some weight to this conjecture?