Hostname: page-component-586b7cd67f-rcrh6 Total loading time: 0 Render date: 2024-11-22T00:22:11.793Z Has data issue: false hasContentIssue false
  • English
  • Français

A Unique Chert Nodule from the Hawes Limestone (Lower Carboniferous, D1) of Wensleydale, Yorkshire

Published online by Cambridge University Press:  01 May 2009

D. Moore
D. Moore
Affiliation:
Geological Department, Accra, Ghana.
Get access Rights & Permissions [Opens in a new window]

Abstract

A unique chert nodule, bowl-shaped, ten feet in diameter and three feet deep, with a mass of crystalline calcite in the bottom, occurs in the lower part of the Hawes Limestone at the base of the Yoredale Series. The overall peculiarities of the nodule require an origin after consolidation of the enclosing work.

Type
Articles
Information
Geological Magazine , Volume 96 , Issue 6 , December 1959 , pp. 453 - 456
Copyright
Copyright © Cambridge University Press 1959

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

Chatwin, C. P., 1948. British Regional Geology—East Anglia and adjoining areas. Geol. Surv. Gt. Britain.Google Scholar
Hey, R. W., 1956. Cherts and limestone from the Crow Series near Richmond, Yorkshire. Proc. Yorks. Geol. Soc., xxx, 289–300.CrossRefGoogle Scholar
Moore, D., 1958. The Yoredale Series of upper Wensleydale and adjacent parts of north-west Yorkshire. Proc. Yorks. Geol. Soc., xxxi, 91–146.Google Scholar
Wells, A. J., 1955. The Development of chert between the Main and Crow Limestones in north Yorkshire. Proc. Yorks. Geol. Soc., xxx, 177–196.CrossRefGoogle Scholar
Pettijohn, F. J., 1957. Sedimentary Rocks (2nd Ed.) Harper and Brothers, New York.Google Scholar