Pen y Fan from the summit of Corn Du
|Elevation||873 m (2,864 ft)|
|Prominence||28 m (92 ft)|
|Parent peak||Pen y Fan|
|Translation||Black Horn (Welsh)|
|Topo map||OS Landranger 160|
Corn Du is a mountain immediately to the southwest of Pen y Fan and the second highest peak in South Wales at 2864 feet, situated in the Brecon Beacons National Park. The summit itself is marked by a well structured Bronze Age cairn with a central burial cist like that on nearby Pen y Fan. The two summits are visible from great distances owing to their height above the surrounding moorland, and are famous landmarks. The views from the peaks are also panoramic and very extensive, the Black Mountain (range) and Fforest Fawr being especially obvious to the west.
The summit is often crossed on the way to Pen y Fan, and forms part of a well-known circuit of the Beacons. It offers good views down into Cwm Llwch and across the Usk valley to Brecon as well as east towards the Sugar Loaf, Monmouthshire above Abergavenny. Tommy Jones' Obelisk is found on its western flanks, in between the summit and Y Gyrn. All of the surrounding moorland is open to access, but crossing the many peat bogs is difficult and the paths are well engineered and maintained by the National Trust.
The summit is very similar to that of Pen y Fan: flat and anvil shaped. It is similarly formed from the relatively erosion-resistant Devonian age sandstones from the Upper Old Red Sandstone known as the Plateau Beds. The rock strata are clearly visible at the edge of the escarpment, where they form a resistant edge to the cliff. The same strata are visible all along the escarpment facing north, as well as the rearward edge facing south-east and lying behind the main peaks.
Nearby is one of the few natural lakes in the park, the small Llyn Cwm Llwch. It may be compared with the much larger glacial lakes of Llyn y Fan Fach and Llyn y Fan Fawr below the peak ridge of the Black Mountain about 15 miles west at the end of the Brecon Beacons escarpment. All three are glacial lakes and were formed during the last ice age by ice scouring out hollows below the peaks, the water being dammed by moraines of rock debris swept down by ice action such as frost shattering.
- Nuttall, John & Anne (1999). The Mountains of England & Wales - Volume 1: Wales (2nd edition ed.). Milnthorpe, Cumbria: Cicerone. ISBN 1-85284-304-7.
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