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
This page is maintained by Roger Suthren
Last Modified: 18 November, 2008