View to the east showing shallow north-easterly dipping beds of unit 26 cut by a north-easterly trending fault. The presence of the fault is shown by two typical features:
- lack of exposure due to
preferential erosion in the zone of fracturing;
- flexuring of the beds adjacent to the fault on the NW side.
Scale: approx. width of outcrop in foreground is 50 m.
Grid reference: 995
322