Hostname: page-component-77c89778f8-9q27g Total loading time: 0 Render date: 2024-07-21T00:22:10.982Z Has data issue: false hasContentIssue false
  • English
  • Français

The Structure of the Edale, Mam Tor and Castleton Area

Published online by Cambridge University Press:  01 May 2009

O. T. Jones
Get access Rights & Permissions [Opens in a new window]

Extract

Edale lies in the valley of the River Noe about 3 miles north-west of Castleton. Near Edale End, about 2½ miles below the village, the Noe turns from a nearly east and west course to a nearly north and south course past Hope to join the River Derwent. In the neighbourhood of Edale the floor and lower flanks of the valley are formed of black shales known as the Edale Shales; they are overlain in succession by the Mam Tor Sandstones, the Shale Grit, the Grindslow Shales, and the coarse Kinder Scout Grits which form the great plateau of the Peak and the precipitous edge of Kinder Scout. North of the Edale valley the Mam Tor Sandstones reappear below the Shale Grit in Ashop Dale and Alport Dale. They occur also to the west of the valley in two narrow inliers just north of the railway in Roych Clough and Moor Clough.

Type
Articles
Information
Geological Magazine , Volume 79 , Issue 3 , June 1942 , pp. 188 - 196
Copyright
Copyright © Cambridge University Press 1942

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

1 Journ. Manchester Geol Association, i, pt. i (1925–1926), fig. 3 (p. 20), 1927.Google Scholar

1 Fearnsides, W. G., Proc, Geol. Assoc., 1932, xliii, 158.Google Scholar

2 Fearnsides, op. cit. sup., p. 157.Google Scholar

1 Quart. Journ. Geol. Soc., xcvi, 271–296.Google Scholar

1 Abs. Proc. Geol. Soc., 9th November, pp. 2, 3, 1939.Google Scholar

2 Fearnsides, W. G. and Templeman, A., Proc. Yorks. Geol. Soc., 1934, xxii, 100.Google Scholar