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Geology of the Glen Tromie Hydro-electric Tunnels, Inverness-shire

Published online by Cambridge University Press:  01 May 2009

J. G. C. Anderson
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Abstract

Tunnels constructed in connection with hydro-electric development near the head of Glen Tromie cut Moinian granulites and semi-pelitic schists penetrated by pegmatites and by quartz-porphyry and felsite sills. Deep and very extensive deposits of glacial drift are also present. A remarkable feature of the latter is the presence of hollow chambers well below the surface which are interpreted as partially collapsed moulds of buried blocks of ice.

Type
Articles
Information
Geological Magazine , Volume 88 , Issue 2 , April 1951 , pp. 133 - 139
Copyright
Copyright © Cambridge University Press 1951

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References

REFERENCES

Anderson, E. M., 1942. The Dynamics of Faulting, etc. Edinburgh.Google Scholar
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