Автор |
Pochin Mould, Daphne D. C. |
Дата выпуска |
1946 |
dc.description |
The district of Strath Errick and Foyers, with which the investigation recorded here is concerned, occupies about 70 square miles southeast of Loch Ness, in Inverness-shire. The ground rises steeply from the loch to form a bordering ridge, beyond which it slopes more gently to Strath Errick. Further to the south-east, the hills rise to a height of 2,560 ft. in Beinn Bhuraich. The country is chiefly moor and hill grassland, with numerous exposures of rock; fairly extensive areas are under arable cultivation in Strath Errick. The district is drained by the Rivers Fechlin and Farigaig, both of which enter Loch Ness through deep gorges (Text-fig. 3). |
Формат |
application.pdf |
Издатель |
Cambridge University Press |
Копирайт |
Copyright © Cambridge University Press 1946 |
Название |
The Geology of the Foyers “Granite” and the Surrounding Country |
Тип |
research-article |
DOI |
10.1017/S0016756800077840 |
Electronic ISSN |
1469-5081 |
Print ISSN |
0016-7568 |
Журнал |
Geological Magazine |
Том |
83 |
Первая страница |
249 |
Последняя страница |
265 |
Аффилиация |
Pochin Mould Daphne D. C.; University of Edinburgh |
Выпуск |
6 |