Hostname: page-component-848d4c4894-8bljj Total loading time: 0 Render date: 2024-06-16T19:57:44.907Z Has data issue: false hasContentIssue false
  • English
  • Français

Basement Carboniferous in Upper Teesdale, N. Yorks.

Published online by Cambridge University Press:  01 May 2009

W. T. Harry
Get access Rights & Permissions [Opens in a new window]

Abstract

Excavations in Upper Teesdale, N. Yorks, exposed basement Carboniferous at its unconformable contact with underlying shales of probable Silurian age. The lowest basement beds are tough conglomerates cut by compression joints. The constituent pebbles are unsorted, locally derived, and mainly andesites and rhyolites, with vein quartz and shale pebbles. A dreikanter outline is common. The conglomerate is contrasted with others also between the Carboniferous and Lower Palaeozoic in England.

Type
Articles
Information
Geological Magazine , Volume 87 , Issue 4 , August 1950 , pp. 297 - 299
Copyright
Copyright © Cambridge University Press 1950

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

Gunn, W., and Clough, C. T., 1878. Discovery of Silurian Beds in Teesdale. Quart. Jour. Geol. Soc., xxxiv, 27.Google Scholar
Turner, J. S., 1927. The Lower Carboniferous Succession in the Westmor-land Pennines. Proc. Geol. Assoc., xxxviii, 339.Google Scholar