Hostname: page-component-78c5997874-t5tsf Total loading time: 0 Render date: 2024-11-14T04:50:47.746Z Has data issue: false hasContentIssue false
  • English
  • Français

The Western Longmyndian Rocks of the Shrewsbury District

Published online by Cambridge University Press:  01 May 2009

T. H. Whitehead
T. H. Whitehead*
Affiliation:
Ragleth House, Little Stretton, Shropshire.
Get access Rights & Permissions [Opens in a new window]

Abstract

Evidence from graded bedding and other sedimentary structures has shown that in the eastern outcrop of the Western Longmyndian rocks of the Shrewsbury area the stratigraphical base lies towards the east. Since in the western outcrop of these rocks the base is believed to lie towards the west, Professor Whittard's suggestion that the Western Longmyndian rocks are folded into a syncline, with the “ Oakswood Group ” representing a repetition of the “ Bayston Group ”, is accepted. The form and age of the fold are briefly discussed.

Type
Research Article
Information
Geological Magazine , Volume 92 , Issue 6 , December 1955 , pp. 465 - 470
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

Blake, J. F., 1890. On the Monian and Basal Cambrian Rocks of Shropshire. Quart. Journ. Geol. Soc., xlvi, 386–419.CrossRefGoogle Scholar
Callaway, C., 1882. The Pre-Cambrian Rocks of Shropshire, Part II. Quart. Journ. Geol. Soc., xxxviii, 119–123.CrossRefGoogle Scholar
Callaway, C., 1888. On some Ancient Salopian Conglomerates. Trans. Shropshire Archaeol. & Nat. Hist. Soc., xi, 239–243.Google Scholar
Callaway, C., 1891. On the Unconformities between the Rock-systems underlying the Cambrian Quartzite in Shropshire. Quart. Journ. Geol. Soc., xlvii, 109–124.Google Scholar
Cantrill, T. C., 1925. In The Geology of the Country around Wem (Explanation of Sheet 138). Mem. Geol. Surv. Great Britain.Google Scholar
Challinor, J., 1948. New Evidence concerning the Original Order of Deposition of the Longmyndian Rocks. Geol. Mag., lxxxv, 107–9.CrossRefGoogle Scholar
Cobbold, E. S., 1900. Church Stretton: Geology. Shrewsbury, Wilding and Son.Google Scholar
James, J. H., 1952. Notes on the Relationship of the Uriconian and Longmyndian Rocks near Linley, Shropshire. Proc. Geol. Assoc., lxiii, 198–200.CrossRefGoogle Scholar
Lapworth, C., and Watts, W. W., 1894. The Geology of South Shropshire. Proc. Geol. Assoc., xiii, 297–355.CrossRefGoogle Scholar
Lapworth, C., and Watts, W. W., 1910. Shropshire. Geology in the Field. Geol. Assoc. Jubilee Vol., 739–769.Google Scholar
Pocock, R. W., and Whitehead, T. H., 1948. British Regional Geology: The Welsh Borderland (second edition), Geol. Surv. and Museum.Google Scholar
“Shrewsbury Memoir,” 1938. Pocock, R. W., Whitehead, T. H., Wedd, C. B., and Robertson, T., Shrewsbury District, including the Hanwood Coalfield (Explanation of Sheet 152). Mem. Geol. Surv. Great Britain.Google Scholar
Watts, W. W., 1925. The Geology of South Shropshire. Proc. Geol. Assoc., xxxvi, 321–363.CrossRefGoogle Scholar
Whitehead, T. H., 1948. Longmyndian Stratigraphy. Geol. Mag., lxxxv, 181–2.CrossRefGoogle Scholar
Whittard, W. F., 1952. A Geology of South Shropshire. Proc. Geol. Assoc., lxiii, 143–197.CrossRefGoogle Scholar