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The Lustleigh Fault in North-East Dartmoor

  • F. G. H. Blyth (a1)
Abstract
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.

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References
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Austen R. A. C., 1842. On the geology of south-east Devonshire. Trans. Geol. Soc., Ser. II, vol. vi, Pt. 2, 433489.
Blyth F. G. H., 1949. The sheared porphyrite dykes of South Galloway. Quart. Jour. Geol. Soc., cv, 393423.
Dearman W. R., 1950. The Structure of the Okehampton District. Ph.D. Thesis, University of London.
Evans J. W., 1925. Regions of tension. Quart. Jour. Geol. Soc., lxxxi, pp. lxxxcxxii.
Osman C. W., 1924. The geology of the northern border of Dartmoor between Whiddon Down and Butterdon Down. Quart. Jour. Geol. Soc., lxxx, 315337.
Reid Clement, 1913. In Ussher, W. A. E., and others: The Geology of the country around Newton Abbot. Mem. Geol. Surv. (sheet 339).
Wooldridge S. W., 1954. The physique of the South-west. Geography, xxxix, 231242.
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Geological Magazine
  • ISSN: 0016-7568
  • EISSN: 1469-5081
  • URL: /core/journals/geological-magazine
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