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Published online by Cambridge University Press: 01 May 2009
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.
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page 157 note 2 Trans. Geol. Soc. Glasgow, xvii, pt. iii, 1925–1926.Google Scholar
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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
