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Note on the Relation of the Upper and Lower Old Red Sandstone of Gower

Published online by Cambridge University Press:  01 May 2009

Daisy M. Williams
Daisy M. Williams
Affiliation:
University College, Swansea.
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Extract

The Old Red Sandstone occurs in Gower in several inliers which form hills rising above the undulating plateau of Carboniferous Limestone. The chief are Cefn-y-bryn (548 feet) in mid-Gower, Llanmadog Hill (609 feet), the westerly extension of Cefn-y-bryn in north-west Gower, and Rhosilli Down (633 feet) in the extreme west of Gower.

Type
Original Articles
Information
Geological Magazine , Volume 63 , Issue 5 , May 1926 , pp. 219 - 223
Copyright
Copyright © Cambridge University Press 1926

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References

page 219 note 1 “The Geology of the South Wales Coalfield,” part ix, “West Gower and the Country around Pembrey,” pp. 4, 5, 1907, Mem. Geol. Surv. This work is referred to subsequently as the “West Gower Memoir”.Google Scholar

page 219 note 2 “The Geology of the South Wales Coalfield,” part v, “The Country around Merthyr Tydfil,” 1904, Mem. Geol. Surv.Google Scholar

page 219 note 3 “West Gower Memoir,” p. 5.Google Scholar

page 220 note 1 “The Old Red Sandstone of the Cardiff District,” Q.J.G.S., vol. lxxx, 1924, p. 496.Google Scholar

page 220 note 2 “West Gower Memoir,” p. 6.Google Scholar

page 220 note 3 “The Geology of the South Wales Coalfield”; pt. xiii, “The Country around Pembroke and Tenby,” 1921, pp. 27, 28; pt. xi, “The Country around Haverfordwest,” Mem. Geol Surv., pp. 123, 124, 136, 204, 1914.Google Scholar

page 220 note 4 Certain bands within the Lower Old Red Sandstone of Pembrokeshire frequently show evidence of contemporaneous erosion, but there does not appear to be evidence of such discordant junctions within the Red Marl of South Glamorgan.

page 221 note 1 The Building of the British Isles, 1911, p. 128.Google Scholar

page 221 note 2 Op. cit., p. 128.Google Scholar

page 221 note 3 An Introduction to Stratigraphy (British Isles), 1923, p. 95.Google Scholar

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page 223 note 1 Evans, J. W., op. cit., p. 204.Google Scholar