Hostname: page-component-cd9895bd7-gbm5v Total loading time: 0 Render date: 2024-12-27T07:03:32.307Z Has data issue: false hasContentIssue false

II.—Notes on the Correlation of the Lower Carboniferous Rocks of England and Scotland

Published online by Cambridge University Press:  01 May 2009

William Gunn
Affiliation:
H.M. Geological Survey of Scotland.

Extract

The substance of the following paper was given at a meeting of the Geological Society of Edinburgh on January 20th this year. Its object is to show that the group of Lower Scottish Limestones about Dunbar and round the Midlothian Coalfield does not represent any part of the Mountain Limestone of Yorkshire, but is the equivalent of the upper part of the Yoredale Series of Phillips, while the Edge Coals and Upper Limestones of Midlothian represent a series of beds which in Yorkshire and Northumberland lie above the true Yoredale Series of Phillips, and which were included by him in the Millstone Grit. It necessarily follows from this correlation that the lower part of Phillips' Yoredale Series, together with the Scar or Mountain Limestone of Yorkshire, are represented in Scotland by the Calciferous Sandstone Series, which is mainly a fresh-water deposit.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1898

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

page 344 note 1 Manual of Geology, p. 165 (1855).

page 345 note 1 Proc. Berwickshire Nat. Field Club, vol. iv, p. 151.

page 345 note 2 De la Beche, Geological Manual, 1833, pp. 391, 392.