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Some underwater disturbances in the torridonian of skye and raasay

By: Selley, R.C.
Contributor(s): Shearman, D.J | Sutton, J | Watson, J.
Material type: ArticleArticleDescription: 224-243pp ; Illustration.Subject(s): Torridonian rocks - Great Britain | Disturbances - Torridonian of skye and raasay In: Geological magazine : Vol. 100 Iss. 1-6 Year. 1963Summary: Abstract The paper deals with disturbances of bedding contemporaneous with deposition in Torridonian rocks of Skye and Raasay. Most of the structures described have the general form of sharp upwardly-directed peaks separated by areas of more or less undisturbed bedding; within the peaks the bedding is often contorted or destroyed. The structures are developed in sandstones and are thought to have been formed more or less in situ by the shifting and rearrangement of quicksands. An origin as a result of slumping is rejected. The appearance of the structures is thought to be connected with the environment of deposition which appears to be that of very shallow water.
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Article Article Library and Information Centre
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Bound Journal Collection Not for loan 002548_29
Serials/Scientific Journal Serials/Scientific Journal Library and Information Centre
Periodical Section
Bound Journal Collection 550 GEO (Browse shelf) Available 002548

Abstract
The paper deals with disturbances of bedding contemporaneous with deposition in Torridonian rocks of Skye and Raasay. Most of the structures described have the general form of sharp upwardly-directed peaks separated by areas of more or less undisturbed bedding; within the peaks the bedding is often contorted or destroyed. The structures are developed in sandstones and are thought to have been formed more or less in situ by the shifting and rearrangement of quicksands. An origin as a result of slumping is rejected. The appearance of the structures is thought to be connected with the environment of deposition which appears to be that of very shallow water.

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