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The Green Beds of South Knapdale

Published online by Cambridge University Press:  01 May 2009

William J. McCallien
William J. McCallien
Affiliation:
Glasgow University.
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Extract

In his description of the older rocks of Kintyre the writer has described in some detail the field characters of the Green Beds of that peninsula. Many difficulties were met with in the southern part of Kintyre where the rock-groups are repeated by folding. The chief of these difficulties were occasioned by the knowledge that schists identical in composition and appearance to the Green Beds occur at many different horizons below the Erins Quartzite.

Type
Original Articles
Information
Geological Magazine , Volume 70 , Issue 4 , April 1933 , pp. 156 - 167
Copyright
Copyright © Cambridge University Press 1933

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References

page 156 note 1 Trans. Roy. Soc. Edin., lvi, pt. ii, No. 17, 1929.Google Scholar

page 157 note 1 Trans. Geol. Soc. Glasgow, xvii, pt. ii, 1924–1925.Google Scholar

page 157 note 2 Trans. Geol. Soc. Glasgow, xvii, pt. iii, 1925–1926.Google Scholar

page 157 note 3 Min. Mag., xvii, No. 29, 1930, 239–256.Google Scholar

page 157 note 4 Geol. Mag., LXVIII, 1931, 126–133.Google Scholar

page 159 note 1 Mem. Geol. Surv. Scotland, “The Geology of Cowal” and Sheet 29.Google Scholar

page 159 note 2 “The Structure of the South-West Highlands of Scotland ”: Q.J.G.S., xxviii, pt. ii, 1922.Google Scholar

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page 164 note 1 Trans. Geol. Soc. Glasgow, xvii, pt. ii, 1924–1925.Google Scholar

page 164 note 2 Trans. Roy. Soc. Edinburgh, lvi, pt. iii, No. 25, 1930.Google Scholar

page 166 note 1 Trans. Geol. Soc. Glasgow, xvii, iii, 1925–1926.Google Scholar

page 166 note 2 Op. cit., fig. 2.Google Scholar

page 166 note 3 On Fig. 1 Glenralloch runs between the head of West Loch Tarbert and the northern end of Barmore Island.Google Scholar