Structural Geology of Leornian

Units: mainly A12 and PR17

image STR-15

full-size image

annotated image

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

Back to: [Structural geology]

This page is maintained by Roger Suthren

Last Modified: 18 November, 2008