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The Tectonics of the Purbeck and Ridgeway Faults in Dorset

Published online by Cambridge University Press:  01 May 2009

W. J. Arkell
W. J. Arkell
Affiliation:
University Museum, Oxford.
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Extract

The Ridgeway Fault may begin along the north margin of the Chaldon Anticline as mapped by Bristow (1855), but its existence there was doubted by Strahan. From the “bridge” at Holworth it certainly continues along the north margin of the Poxwell-Sutton Poyntz Anticline to Greenhill. Here it turns a double corner, the exact nature of which is problematical, and runs thence obliquely across and later along and parallel to the north limb of the Upwey Syncline to a point ½ mile west of Portisham, where it dies out in Kimeridge Clay. The total length from near Chaldon is 13 miles.

Type
Original Articles
Information
Geological Magazine , Volume 73 , Issue 3 , March 1936 , pp. 97 - 118
Copyright
Copyright © Cambridge University Press 1936

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References

REFERENCES

Arkell, W. J., 1933–1935. “Analysis of the Mesozoic and Cainozoic Folding in England,” XVIth International Geol. Congress, Washington, 07, 1933 (abstract). Full text winter, 1935–36.Google Scholar
Bristow, H. W., 1852–5. Horizontal Section No. 20 (1852) and Sheet 17, Geol. Survey Map, Old Ser., 1 inch to 1 mile (1855).Google Scholar
Buckland, W., and De La Beche, H. T., 1836. “On the Geology of the Neighbourhood of Weymouth and the adjacent parts of the Coast of Dorset,” Trans. Geol. Soc., iv (2), 1.Google Scholar
Conybeare, W. D., 1822. “Isle of Purbeck,” in Conybeare and Phillips, Outlines of the Geology of England and Wales, Sect, iii (e), 110.Google Scholar
Dines, H. G., and Edmunds, F. H., 1927. “The Tectonic Structure of the Hogs Back,” Proc. Geol. Assoc., xxxviii, 395.CrossRefGoogle Scholar
Fisher, O., 1896. “Vertical Tertiaries at Bincombe, Dorset,” Geol. Mag., p. 246.CrossRefGoogle Scholar
Hudleston, W. H., 1889. “Excursion to Weymouth,” Proc. Geol. Assoc., xi, p. xlix.Google Scholar
Pruvost, P., 1922. “La faille de Landrethun et son prolongement au Cap Gris-Nez,” Ann. Soc. géol. du Nord, xlvi, 54.Google Scholar
Rowe, A. W., 1901. “The Zones of the White Chalk of the English Coast—Part 2, Dorset,” Proc. Geol. Assoc., xvii, 1.CrossRefGoogle Scholar
Strahan, A., 1895. “On Overthrusts of Tertiary Date in Dorset,” Quart. Journ. Geol. Soc., li, 549.CrossRefGoogle Scholar
Strahan, A., 1898. “The Geology of the Isle of Purbeck and Weymouth,” Mem. Geol. Surv.Google Scholar
Strahan, A., 1904–1905. Sheets 341–3, Geol. Survey Maps, colour printed, 1 inch to 1 mile.Google Scholar
Strahan, A., 1906–1932. “Guide to the Geological Model of the Isle of Purbeck,” 2nd ed., 1932, Mem. Geol. Surv.Google Scholar
Stuart, M. G., 1889. “The Ridgway Fault,” Proc. Dorset Field Club, x, 55.Google Scholar
Turner, J. S., 1935. “Structural Geology of Stainmore, Westmorland,” Proc. Geol. Assoc., xlvi, 121.CrossRefGoogle Scholar
Webster, T., 1816. Letters from Dorset, in Englefield, H., Picturesque Beauties of the Isle of Wight (written 1812, with drawings).Google Scholar
Weston, C. H., 1848–1849. “On the Geology of the Ridgway near Weymouth,” Quart. Journ. Geol. Soc., iv, 245, and v, 317. Also in viii, 110 (1852).Google Scholar
White, H. J. O., 1921. “A Short Account of the Geology of the Isle of Wight,” Mem. Geol. Surv. (revision and abridgement of a larger memoir by Bristow, revised by Strahan, and published in 1889).Google Scholar
Woodward, H. B., 1895. “Jurassic Rocks of Britain,” vol. v, Mem. Geol. Surv.Google Scholar