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XVIII.—The Geology of the Highland Border: Stonehaven to Arran

Published online by Cambridge University Press:  06 July 2012

J. G. C. Anderson
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Extract

(a) Scope of Paper.—The distinction between Highlands and Lowlands is a most striking feature of the topography of Scotland and has for long played an important part in the political, economic and social life of the country. Although the dividing line between the two regions, in a purely geographical sense, is ill-defined in some districts, on the whole it coincides fairly closely with a powerful geological dislocation which can be traced across Scotland from Stonehaven to Arran (fig. 1), a distance of 160 miles. This dislocation has for long been termed the Highland Boundary Fault. On detailed study it is found to be only one of several faults making up a complex fracture-zone, one of the most important in the British Isles, within which movements on a considerable scale have taken place from Ordovician to Carboniferous times.

Type
Research Article
Information
Earth and Environmental Science Transactions of The Royal Society of Edinburgh , Volume 61 , Issue 2 , 1947 , pp. 479 - 515
Copyright
Copyright © Royal Society of Edinburgh 1947

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