II.—Notes upon the Occurrence of the Post-Pliocene Drift of Charnwood Forest

Extract

During the investigations I made on the “Post-Pliocene Gravels of the Severn, Avon, and Evenlode, and their extension over the Cotteswold Hills,” the result of which I embodied in a paper read before the members of the Cotteswold Club in the early part of 1869, and is now published in their “Proceedings,” many of the boulders found by me, on examination by R. Etheridge, Esq., of Jermyn Street, were determined to be syenite and granite from Charnwood.