Pen Y Gadair Fawr
Geology
The summit and upper slopes of Pen y Gadair Fawr are formed from the Early Devonian Epoch sandstones of the Brownstones Formation, a division of the Old Red Sandstone. Beneath these and forming the lower slopes are the sandstones of the Senni Formation (traditionally the Senni Beds). Mudstone layers within these sandstones are more readily eroded and have given rise to the stepped appearance of parts of the mountain, not least the summit section. Peat has accumulated on parts of the hill in the postglacial period, notably north towards Waun Fach.
Access
The hill is wholly within land mapped under the Countryside and Rights of Way Act 2000 as open country and hence is legally accessible to walkers despite their being no public rights of way leading to it. Mountain bikers can follow the forest roads within nearby Mynydd Du Forest, one of which tops out at 715m, just 0.5 km from the summit, but have no legal access to the hill itself.
References
- ^ Nuttall, John & Anne (1999). The Mountains of England & Wales - Volume 1: Wales (2nd edition ed.). Milnthorpe, Cumbria: Cicerone. ISBN 1-85284-304-7.
- ^ "England and Wales sheet 214 'Talgarth'". Maps portal. British Geological Survey. Retrieved 17 May 2020.
- ^ "Cycling". Natural Resources Wales. Retrieved 17 May 2020.
- ^ "Bing maps". Bing. Retrieved 17 May 2020.