IV.—The Physical History of the Norwegian Fjords
The Scandinavian Promontory . — This remarkable promontory, extending for over a thousand miles from the Naze to the North Cape, is formed mainly of Archæan rocks, consisting of gneiss, crystalline schists, and other metamorphic rocks, penetrated by granite and other igneous dykes of later date. The...
| Published in: | Geological Magazine |
|---|---|
| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Cambridge University Press (CUP)
1913
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1017/s0016756800125488 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800125488 |