Lava channels on Tristan da Cunha
By: Baker, P.E
.
Contributor(s): Harris, P.G.
Material type: 
ArticleDescription: 345-351pp ; Illustration.Subject(s): Lava streams - Tristan da Cunha - Atlantic ocean island | Volcanic features - Atlantic ocean island
In:
Geological magazine : Vol. 100 Iss. 1-6 Year. 1963Summary: Abstract
Lava channels flanked by lava levees are described from Tristan da Cunha. These have been formed by the building up of the levees by overflow and solidification of fluid lava from the channels. A distinction is made between the terms “lava levee” and “lava moraine”.
| Item type | Current location | Collection | Call number | Status | Date due | Barcode |
|---|---|---|---|---|---|---|
Article
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Library and Information Centre Periodical Section | Bound Journal Collection | Not for loan | 002548_47 | ||
Serials/Scientific Journal
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Library and Information Centre Periodical Section | Bound Journal Collection | 550 GEO (Browse shelf) | Available | 002548 |
Abstract
Lava channels flanked by lava levees are described from Tristan da Cunha. These have been formed by the building up of the levees by overflow and solidification of fluid lava from the channels. A distinction is made between the terms “lava levee” and “lava moraine”.
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