Knowledge (XXG)

Waun Lefrith

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369: 485: 474: 527:, to name a few of the most obvious residents. The kestrel and buzzard are widely distributed, but the raven is restricted to the higher mountains. The red kite survived in this area and was the last refuge of the species thanks to the lack of shoots for game birds. It has now been reintroduced to many parts of England and Wales thanks to campaigns run by the 31: 464:
and local map are essential companions to aid route finding. There are relatively few walkers on the Black Mountain, even when the weather is good and clear, so the walker must rely on his or her own resources to complete a circuit.
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The entire mountain is open country and so freely accessible to walkers. The most popular path of ascent is that from the car park at the foot of the water board road running steeply up to
324:. Its southern slopes are formed from the hard-wearing sandstones of the overlying Plateau Beds Formation which are of upper/late Devonian age. It is those rocks which form vertical 429:, but the footpath is protected at some points by stone pavements. The path follows the edge of the escarpment, giving panoramic views in all directions. The footpath from 646: 194: 591:
Nuttall, John & Anne (1999). The Mountains of England & Wales - Volume 1: Wales (2nd edition ed.). Milnthorpe, Cumbria: Cicerone.
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along the top edge of the scarp. The northern face of Waun Lefrith was home to a glacier during the ice ages which gouged out the
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is plentiful due to the extensive rough pasture present below the main peaks which allows ground nesting of the species. Pied
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runs over Waun Lefrith whilst the low level route runs along the foot of its northern escarpment to the small
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gives excellent aerial views of the lake, although some care is needed in poor visibility or cold weather.
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avoids the parallel tarmacked road to the dam, rising along the ridge which leads directly to the summit.
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British Geological Survey 1:50,000 map sheet 213 'Brecon' & accompanying sheet explanation
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Waun Lefrith is formed from the sandstones and mudstones of the Brownstones Formation of the
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occur to the east of the summit at the base of the scarp, and below the prominent peak of
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disappear, and especially dangerous when walking along the edge of the escarpment. A
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and over which lake the mountain looms. It lies to the east of the small village of
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are common near the streams and torrents running from the hill tops.
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images of Waun Lefrith & surrounding area from Geograph website
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As in all mountains care is needed when the weather is poor, when
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to the north of the peak. Beyond the lake to the north lies the
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are the other, higher summits of the Carmarthen Fans (
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Index


Picws Du
Elevation
Prominence
Parent peak
Picws Du
Listing
Nuttall
Coordinates
51°52′47″N 3°44′57″W / 51.8796°N 3.7492°W / 51.8796; -3.7492
Welsh
Carmarthenshire
Wales
Parent range
Brecon Beacons
OS grid
SN825217
Picws Du
Carmarthen Fans
Welsh
Black Mountain
Brecon Beacons National Park
Carmarthenshire
Wales
Picws Du
Fan Foel
glacial lake
Llyn y Fan Fach
panorama
Usk Reservoir

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