词条 | Cefn Cul |
释义 |
GeologyCefn 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.[2] ArchaeologyAn 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.[3] AccessThe 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. References1. ^Ordnance Survey Explorer map OL12 'Brecon Beacons National Park: western area' 2. ^British Geological Survey 1:50,000 map sheets 213 'Brecon' & 231 'Merthyr Tydfil' & accompanying sheet explanations/memoirs 3. ^Leighton, D.K. 1997 'Mynydd Du and Fforest Fawr' RCAHMW Aberystwyth External links
3 : Mountains and hills of Powys|Black Mountain, Wales|Fforest Fawr |
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