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

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Last edited by MARC Bot
October 8, 2017 | History

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

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Publish Date
Publisher
s.n.
Language
English
Pages
184

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Previews available in: English

Book Details


Edition Notes

"From the Quarterly Journal of the Geological Society for May 1869."--P. [172].

Includes bibliographical references.

CAM

Published in
London
Other Titles
Quarterly journal of the Geological Society.

The Physical Object

Pagination
p. [172]-184 :
Number of pages
184

ID Numbers

Open Library
OL24829367M
Internet Archive
onevidencesofrid00hull

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October 8, 2017 Edited by MARC Bot merge duplicate works 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'
December 11, 2009 Created by WorkBot add works page