The Avonian Succession in the South of the Isle of Man
- 1 March 1930
- journal article
- Published by Geological Society of London in Quarterly Journal of the Geological Society
- Vol. 86 (1-4), 234-290
- https://doi.org/10.1144/gsl.jgs.1930.086.01-04.11
Abstract
The Carboniferous rocks described in this paper occur within an area some 8 to 9 square miles in extent surrounding the ancient town of Castletown. The district is coastal and low-lying, a considerable portion being less than 100 feet above sea-level. The highest ground lies north-west of Ballasalla, where a few small tracts rise slightly above 200 feet.Keywords
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