Hostname: page-component-6bf8c574d5-h6jzd Total loading time: 0.001 Render date: 2025-02-28T05:47:43.077Z Has data issue: false hasContentIssue false
  • English
  • Français

Palaeolith from the Axe gravels

Published online by Cambridge University Press:  08 January 2012

H. St. George Gray
Get access Rights & Permissions [Opens in a new window]

Abstract

An abstract is not available for this content so a preview has been provided. Please use the Get access link above for information on how to access this content.
Image of the first page of this content. For PDF version, please use the ‘Save PDF’ preceeding this image.'
Type
Notes
Information
The Antiquaries Journal , Volume 7 , Issue 1 , January 1927 , pp. 71 - 72
Copyright
Copyright © The Society of Antiquaries of London 1927

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 71 note 1 These gravels have provided the Southern Railway with much ballast for many years, and they form a cliff or mound about 50 ft. high in the Axe Valley. The cliff rests upon clay and the implements occur at a depth of about 40 ft. below the surface. Among the references to this subject are: Memoir on the Geology of Sidmouth and Lyme Regis, 1911; Salter, A. E., Proc. Geol. Assoc, xv, 282Google Scholar; D'Urban, , Geol. Mag., 1878, p. 37CrossRefGoogle Scholar; SirEvans, John, Report Brit. Assoc., 1877, p. 116Google Scholar; Parfitt, E., Trans. Devon Assoc, xvi, 501–4Google Scholar.