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: by Edward Hull
Contributors: Geological Society of London
Publisher: s.n.
Published: 1869
Place of publication: London
Language: eng
Number of pages: 184
Subjects: Carboniferous; Stratigraphic Geology
Other titles: Quarterly journal of the Geological Society.
Notes: "From the Quarterly Journal of the Geological Society for May 1869."--P. [172].

Includes bibliographical references.

CAM