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 /
Hull, Edward,1829-1917.
Geological Society of London.
[London : s.n.,
1869]
"From the Quarterly Journal of the Geological Society for May 1869."--P. [172].
Includes bibliographical references.
Geology, Stratigraphic