Hostname: page-component-cd9895bd7-mkpzs Total loading time: 0 Render date: 2024-12-28T00:13:39.379Z Has data issue: false hasContentIssue false
  • English
  • Français

Glacial Melt-Water Spillways near Kidsgrove, Staffordshire

Published online by Cambridge University Press:  01 May 2009

E. M. Yates
E. M. Yates
Affiliation:
University Of London, King's College, Strand, W.C. 2
Get access Rights & Permissions [Opens in a new window]

Abstract

As a result of the drainage contest between the Weaver headstreams and the headstreams of the Trent the west facing edge of the Potteries coalfield has been breached in a number of places, in particular at Kidsgrove. During the last retreat of the ice the Kidsgrove breach came ultimately to act as a spillway for the large lake contained between the ice and the coalfield. Before the breach was uncovered, however, a number of spillways were cut further east.

Type
Articles
Information
Geological Magazine , Volume 92 , Issue 5 , October 1955 , pp. 413 - 418
Copyright
Copyright © Cambridge University Press 1955

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

REFERENCES

Gibson, W., and Wedd, C. B., 1902. The Geology of the Country around Stoke-upon-Trent (Explanation of Sheet 123). Mem. Geol. Surv.Google Scholar
Jowett, A., and Charlesworth, J. K., 1929. The Glacial Geology of the Derbyshire Dome. Quart. Journ. Geol. Soc., cxxxv, 307–337.CrossRefGoogle Scholar