Cefn Cul
Geology
Cefn Cul is formed from sandstones and mudstones of the Senni Beds and Brownstones Formations of the Old Red Sandstone laid down during the Devonian period. Whilst the regional dip of the rock beds is to the south, locally they vary and a broad anticlinal structure coincides with the hill. It is within the area designated in 2005 as Fforest Fawr Geopark.
Archaeology
An ancient cairn occurs near the southern end and a standing stone can be found just above the minor road to the west of Cefn Cul. Arguably the principal feature of the hill is the scatter of pillow mounds across its southern spur and over its lower eastern slopes above Cray Reservoir. These were established in the nineteenth century for the production of rabbit fur and meat.
Access
The hill is designated as open country so freely accessible to walkers though a series of fences and walls cross the hill and require negotiation without damage.