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XXXIV.—The Geology of South-Eastern Kincardineshire.

Published online by Cambridge University Press:  06 July 2012

Robert Campbell
Affiliation:
Lecturer in Petrology in the University of Edinburgh.

Extract

In 1804, Lieutenant-Colonel Imrie communicated to the Royal Society of Edinburgh a paper entitled “A Description of the Strata which occur in ascending order from the Plains of Kincardineshire to the Summit of Mount Battoc, one of the most elevated points in the Eastern District of the Grampian Mountains.” He pointed out that, in a short stretch of six miles in the North Esk section, “we pass from the secondary horizontal strata of the newest formation to the vertical, contorted primary strata of the oldest date, and terminate with granite, the primitive rock in the conception of many geologists.”

Type
Research Article
Copyright
Copyright © Royal Society of Edinburgh 1913

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References

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