Abstract
Much has been written on the relations of the Devonshire Trias as observed in the south-coast section. The subject itself is associated with many names of high scientific repute, so that, were the following epitome the result of partial examination, or in any way aided by preconceived notions arrived at from the perusal of the labours of those who have gone before, I should not feel justified in differing in many points from men infinitely my superiors in general geological information.
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