Hostname: page-component-7c8c6479df-94d59 Total loading time: 0 Render date: 2024-03-29T01:46:41.410Z Has data issue: false hasContentIssue false

The Lustleigh Fault in North-East Dartmoor

Published online by Cambridge University Press:  01 May 2009

F. G. H. Blyth
Affiliation:
Geology Department, Imperial College, London, S.W. 7.

Abstract

The north-eastern area of Dartmoor is traversed by a series of straight valleys which follow fault lines. One fault-system, which crosses the granite from near Lustleigh north-westwards to Stickle-path, is described in detail, and its relationships to structures in a wider area are briefly discussed.

Type
Articles
Copyright
Copyright © Cambridge University Press 1957

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

Austen, R. A. C., 1842. On the geology of south-east Devonshire. Trans. Geol. Soc., Ser. II, vol. vi, Pt. 2, 433489.CrossRefGoogle Scholar
Blyth, F. G. H., 1949. The sheared porphyrite dykes of South Galloway. Quart. Jour. Geol. Soc., cv, 393423.CrossRefGoogle Scholar
Dearman, W. R., 1950. The Structure of the Okehampton District. Ph.D. Thesis, University of London.Google Scholar
Evans, J. W., 1925. Regions of tension. Quart. Jour. Geol. Soc., lxxxi, pp. lxxxcxxii.Google Scholar
Osman, C. W., 1924. The geology of the northern border of Dartmoor between Whiddon Down and Butterdon Down. Quart. Jour. Geol. Soc., lxxx, 315337.CrossRefGoogle Scholar
Reid, Clement, 1913. In Ussher, W. A. E., and others: The Geology of the country around Newton Abbot. Mem. Geol. Surv. (sheet 339).Google Scholar
Wooldridge, S. W., 1954. The physique of the South-west. Geography, xxxix, 231242.Google Scholar