IV.—The Ashburton Limestone: its Age and Relations

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Abstract
It has been for some time a matter of surprise to me that Dr. Holl, in his exhaustive memoir “On the Rocks of S. Devon and East Cornwall,”—after once raising the question “whether the limestones” (those of our present subject) “might or might not be the same as those of Ogwell, Ipplepen, and Dartington thrown over a broad anticlinal axis of the lower slates to the North-West,”1— should have ceased following out that line of thought to what appears to me the only possible issue, since he thoroughly recognized the existence of uniclinal structures in parts of the district.

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