An edition of On the evidences of a ridge of lower Carboniferous rocks crossing the plains of Cheshire beneath the Trias, and forming the boundary between the Permian rocks of the Lancashire type on the north, and those of the Salopian type on the south (1869)

On the evidences of a ridge of lower Carboniferous rocks crossing the plains of Cheshire beneath the Trias, and forming the boundary between the Permian rocks of the Lancashire type on the north, and those of the Salopian type on the south

By Edward Hull