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Geology of the glen tromie hydro-electric tunnels, inverness-shire

By: Anderson, J.G.C.
Material type: ArticleArticleDescription: 133-139pp ; Illustration.Subject(s): Geology - Glen tromie - Scotland | Glen tromie hydro electric trunnels - North Central Scotland | Moinian granulite - Scotland | Historical geology - Inverness shire - Scotland In: Geological magazine : Vol. 88 Iss. 1-6 Year. 1951Summary: 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.
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Article Article Library and Information Centre
Periodical Section
Bound Journal Collection Not for loan 002539_19
Serials/Scientific Journal Serials/Scientific Journal Library and Information Centre
Periodical Section
Bound Journal Collection 550 GEO (Browse shelf) Available 002539

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.

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