Published online by Cambridge University Press: 01 May 2009
In 1862 Mr. John E. Taylor (of Norwich), while surveying a newly-opened slate quarry at Dalby, on the western side of the Isle of Man, discovered three impressions of an oval form about nine inches long, and described them as resembling the tracks of Protichnites, figured in Owen's Plaæontology; the quarrymen told him that they were of frequent occurrence.
This communication was received some time since, but from want of space we have been unwillingly compelled to postpone it, and even now cannot give it in full.—Edit.
† Geologist, Vol. v. (1862). p. 322/Google Scholar
‡ 2nd edition, (1861), p. 183.Google Scholar