Abstract
As is well known, the chronological order of deposition of the sediments of that broad band of schists which extends across Scotland from Banffshire and Aberdeenshire in the north-east to Argyllshire in the south-west is a most difficult problem to determine. The noteworthy development that has been made during recent years, leading to a more intimate understanding of the structure of the Southern Highlands, has made this problem much more vital. The question as to the top and bottom of these beds has been much discussed in recent years, and it can not be denied that views have been widely divergent on this matter. When a foreign geologist desires to call attention (through this paper) to certain conditions of fact, it may be pointed out that he is carrying on similar studies of another section—the Norwegian—of this same mountain chain, where one meets similar problems as in the Scottish Highlands.
Publisher
Cambridge University Press (CUP)
Reference5 articles.
1. The Geology of Ben Nevis and Glencoe;Bailey;Mem. Geol. Surv,1916
2. Recumbent Folds in the Schists of the Scottish Highlands
3. The Structure of the South-West Highlands of Scotland
4. The Geology of the Country around Banff, Huntly, and Turriff;Read;Mem. Geol. Surv.,1923
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