Nedd Fechan
Geology
The headwaters of the river run over Old Red Sandstone as far as Blaen-nedd-isaf where they encounter the Carboniferous Limestone outcrop. The river then continues through a wooded gorge for the remainder of its course. The section downstream of Pont Rhyd-y-cnau is cut in sandstones and mudstones of the Millstone Grit series. The section between Pont Melin-fach and the confluence of the river with the Afon Pyrddin is perhaps the most dramatic as the river plunges over several falls of which Sgwd Ddwli and Sgwd Pedol are the most acclaimed. Each of the falls is associated with faults bringing harder sandstone beds into contact with the more readily eroded mudstones.
Habitat protection
The entire gorge section of the Nedd Fechan valley is protected as part of a larger site of special scientific interest which also covers neighbouring river gorges. It also forms a part of a larger special area of conservation designated for its rare bryophyte flora.
Archaeology
Downstream of the Pyrddin confluence is abundant evidence of the former silica rock mining industry. A number of adits are visible on both sides of the river, most of which were served by horse-drawn waggonways. The former waggonways now provide easy access along this lower section of the gorge.
References
- ^ Ordnance Survey Explorer sheet OL12 'Brecon Beacons National Park: western area'
- ^ British Geological Survey 1:50,000 map sheet 231 'Merthyr Tydfil' & accompanying memoir
- ^ Countryside Council for Wales website Archived 2013-10-13 at the Wayback Machine
- ^ Brecon Beacons National Park website