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View towards the north of the hill centred on 918 236. The upper part of the hill is formed of high-grade metamorphic rocks. The lower part consists of low-grade metamorphic rocks (slate and phyllite). Separating these two groups of rocks is a low-angled fault. Scale: see map. Grid reference: from
918 226
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This page is maintained by Roger Suthren
Last Modified: 18 November, 2008