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South Wales Traverse
The South Wales Traverse is a long distance fell running challenge across the mountains of south Wales. It is a linear route of around taking in some 31 summits over high, providing around of ascent. The aim is for challengers to complete the route on foot within 24 hours. The route takes in the mountain ranges of the Black Mountain, Carmarthenshire Fans, Fforest Fawr, Central Brecon Beacons, and the Black Mountains, across most of the Brecon Beacons National Park The Brecon Beacons National Park ( cy, Parc Cenedlaethol Bannau Brycheiniog) is one of three national parks in Wales, and is centred on the Brecon Beacons range of hills in southern Wales. It includes the Black Mountain (range), Black Mountain .... The selection of summits that must be visited is simply all peaks standing at over . Arguably, some of the peaks are points along the ridges rather than true summits in their own right but some consider this to add to the theme of a linear long distance challenge. Ch ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fell Running
Fell running, also sometimes known as hill running, is the sport of running and racing, off-road, over upland country where the gradient climbed is a significant component of the difficulty. The name arises from the origins of the English sport on the fells of northern Britain, especially those in the Lake District. It has elements of trail running, cross country and mountain running, but is also distinct from those disciplines. Fell races are organised on the premise that contenders possess mountain navigation skills and carry adequate survival equipment as prescribed by the organiser. Fell running has common characteristics with cross-country running, but is distinguished by steeper gradients and upland country. It is sometimes considered a form of mountain running, but without the smoother trails and predetermined routes often associated with mountain running. History The first recorded hill race took place in Scotland. - Total pages: 581 King Malcolm Canmore organised ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fan Gyhirych
Fan Gyhirych is a mountain in the Fforest Fawr section of Brecon Beacons National Park in south Wales. It lies within the county of Breconshire, and administered as part of the unitary authority of Powys. Its highest point at 2379 feet (or 725 m) is marked by a trig point which is located towards the western side of the summit plateau. The hill drains to the north into the catchment of the Afon Crai and to the south and west into that of the River Tawe. Fan Fraith is a nearby hill which can be considered a subsidiary top of Fan Gyhirych. Geology The hill is formed largely from sandstones of the Brownstones Formation of the Old Red Sandstone laid down during the Devonian period. A part of the summit plateau is capped by sandstones of the overlying Plateau Beds Formation which also occur on the nearby peak of Fan Fraith. The Cribarth Disturbance, a north-east to south-west aligned zone of faulting and folding, passes through the hill. The hill's finest feature is its nort ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Llangynidr
Llangynidr is a village, community and electoral ward in Powys, Wales, about west of Crickhowell and south-east of Brecon. The River Usk flows through the village as does the Monmouthshire and Brecon Canal. It is in the historic county of Brecknockshire. The village The village is located four miles west of Crickhowell and nine miles southeast of Brecon, beside the River Usk and the Monmouthshire and Brecon Canal. It is situated on the B4558 just to the south of where this road diverges from the A40 trunk road. The stone bridge across the river dates from approximately 1700 and is a Grade I listed building. The canal has five locks and an aqueduct in the vicinity of the village. The village is notionally divided into Upper and Lower Llangynidr. The remains of what may be a medieval reeve's house have been discovered in the course of archaeological excavations in the centre of the village. The village has two public houses, a village shop and a primary school. Histor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cefn Yr Ystrad
Cefn yr Ystrad is a mountain in the Brecon Beacons National Park in Wales. It is an outlier of the Central Beacons group. The broad northeast - southwest aligned ridge reaches an elevation of . One of the southernmost peaks in the Brecon Beacons, it rises to the east of Pontsticill Reservoir. The summit area is a great stretch of wild moorland, with the highest point marked by a trig point. Geology The hill is formed from successive layers of Carboniferous Limestone and the overlying Twrch Sandstone (formerly known as the ''Basal Grit'' of the Millstone Grit). The rock strata generally dip to the south but are locally disrupted by foundering of the sandstone as the underlying limestone has dissolved away. There are extensive ice-smoothed pavements of the latter and loose rock abounds. The crest and southern slopes of the hill are home to dozens of shakeholes, some of which reach considerable proportions. Archaeology The hill is scattered with archaeological sites from th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Allt Lwyd
Allt Lwyd is a top of Waun Rydd in the Brecon Beacons National Park, in southern Powys, Wales. The summit is heathery and marked by a small pile of stones. It is found at the end of Waun Rydd's south-east ridge. It overlooks Talybont Reservoir Talybont Reservoir ( cy, Cronfa Ddŵr Tal-y-bont) is the largest stillwater reservoir in the central Brecon Beacons at . Talybont-on-Usk is downstream of the dam. Construction of the current dam started in 1931 by Newport Corporation, and in ..., and has the Talybont Forest on its steep flanks.Nuttall, John & Anne (1999). The Mountains of England & Wales - Volume 1: Wales (2nd edition). Milnthorpe, Cumbria: Cicerone. . References External links www.geograph.co.uk : photos of Waun Rydd and surrounding area Nuttalls Brecon Beacons Mountains and hills of Powys {{Powys-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waun Rydd
Waun Rydd is a mountain in the Brecon Beacons National Park, in southern Powys, Wales. Its height is 769 m (2,523 ft) and it tops a large boggy plateau rising to the east of Pen y Fan.Nuttall, John & Anne (1999). The Mountains of England & Wales - Volume 1: Wales (2nd edition ed.). Milnthorpe, Cumbria: Cicerone. . The hill takes the form of a plateau with sharp rims on several sides. To the northeast is Craig Pwllfa overlooking Cwm Banw whilst Craig y Fan looks east over Cwm Tarthwynni. To the south is the edge known as Cwar y Gigfran which translates into English as 'quarry of the crow'. It marks the top of a large landslipped area extending to the stream of Blaen y Glyn below. Several ridges extend north and east from the plateau. That known as Gist Wen runs north-northeast to the subsidiary top of Bryn (561m above sea level). The short ridges of Cefn Bach and Cefn Edmwnt run northeast whilst that of Twyn Du extends eastwards towards Talybont Reservoir Tal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cribyn (hill)
Cribyn is a mountain in the Brecon Beacons with an elevation of 2608 feet (or 795 metres) about 300 feet lower than the neighbouring peaks of Pen y Fan and Corn Du. It is a prominent peak in the long and impressive escarpment facing north and running roughly east–west of the central section of the Brecon Beacons. The summit lies on a ridge stretching from Talybont Reservoir in the east, to the A470 road. The ridge line to the west connects Cribyn with the peak of Pen y Fan. To the east, the ridge line descends to Bwlch ar y Fan, a col crossed by an ancient trail sometimes known as 'The Gap Road' before ascending again to the peak of Fan y Bigbr>https://books.google.com/books?id=ROPTbj9als4C&pg=PA19&lpg=PA19&dq=fan+y+big+the+gap&source=web&ots=FUpLQfSmib&sig=XndaQqqTFH7dYopBTBgGSMaQtcM&hl=en] Geology In common with other peaks of the Brecon Beacons, the upper slopes of Cribyn are formed from sandstones of the Brownstones Formation of the Old Red Sandstone laid down during the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Corn Du
Corn Du is a summit of the twin topped Pen y Fan and the second highest peak in South Wales at 873 m (2,864 ft), 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 and Fforest Fawr being especially obvious to the west. Mynydd Epynt is visible to the north behind the county town of Brecon, and other parts of the escarpment to the east. Access 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.Nuttall, John & Anne (1999). The Mountains of Eng ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Y Gyrn
Y Gyrn is a top of Pen y Fan in South Wales, situated in the Brecon Beacons National Park. Tommy Jones' Obelisk is found in between the summit and Corn Du. The summit is a boggy mound overlooking the A470 The A470 (also named the Cardiff to Glan Conwy Trunk Road) is a trunk road in Wales. It is the country's longest road at and links the capital Cardiff on the south coast to Llandudno on the north coast. While previously one had to navigate t ... and the Storey Arms. It is marked by a pile of stones.Nuttall, John & Anne (1999). The Mountains of England & Wales - Volume 1: Wales (2nd edition ed.). Milnthorpe, Cumbria: Cicerone. . External links www.geograph.co.uk : photos of Pen y Fan and surrounding area References {{coord, 51.88328, N, 3.43684, W, region:GB_source:enwiki-osgb36(SO012215), display=title Brecon Beacons Mountains and hills of Powys Tourist attractions in Powys Hewitts of Wales Nuttalls cy:Pen y Fan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fan Fawr
Fan Fawr ( Welsh 'great peak') is a mountain in the Fforest Fawr section of the Brecon Beacons National Park, in Powys, Wales and over 734 m (2,408 ft) high. The summit overlooks the steep eastern face and is marked by a cairn. Unusually, the trig point on this hill does not sit at the summit but 600 m to the south-west on a subsidiary spur. The hill is drained to the west by streams flowing into the Afon Dringarth and to the east by streams draining into the Taf Fawr. The Dringarth is dammed to the west to form Ystradfellte Reservoir as is the Taf Fawr east of the hill to form Beacons Reservoir. To the north-east water flows into the Afon Tarell, a tributary of the River Usk whilst to the south the headwaters of the Afon y Waun conduct water to the Afon Hepste and eventually to the River Neath. Geology The hill is largely formed from sandstones of the Brownstones Formation of the Old Red Sandstone which were laid down during the Devonian period. On the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Craig Cerrig-gleisiad
Craig Cerrig-gleisiad is a subsidiary summit of Fan Fawr in the Fforest Fawr section of the Brecon Beacons National Park, South Wales. It makes up half of the Craig Cerrig-gleisiad and Fan Frynych National Nature Reserve with its sister peak Fan Frynych. The summit is marked by a pile of stones, and sits on the edge of steep north facing cliffs which provide one of the few habitats for Arctic–alpine plants this far south in the British Isles. To the south-west is Fan Llia. Geology The outstanding feature of the mountain is the L-shaped glacial cwm which faces to the northeast. Its modern form is considered to be the result of a complex history of both glacial action and rock-slope failure, a portion of the west wall having collapsed after the main part of the last ice age. Some of the debris was re-worked during the Loch Lomond Stadial and parts stretch as far as the A470 road.Richard Shakesby, Classic Landforms of the Brecon Beacons, 2002, Geological Association Landform G ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fan Frynych
Fan Frynych is the northernmost peak of the Fforest Fawr massif in the Brecon Beacons National Park, South Wales. It is classed as a subsidiary summit of Fan Fawr and makes up half of the Craig Cerrig-gleisiad and Fan Frynych National Nature Reserve with its sister peak Craig Cerrig-gleisiad. The summit is marked by a trig point, where the northern face of Craig Cerrig-gleisiad can be viewed. Geology The upper parts of the mountain are formed from brown-coloured sandstones of the Senni Formation. At lower level and hence older, and forming the lower northern slopes, though largely unseen, are the mudstones of the St Maughans Formation. Both are units of the Lower Old Red Sandstone of early Devonian age. Though locally variable, the rock strata dip generally towards the southeast. The northeastern flank of the mountain is defined by a NE-SW aligned geological fault, the Cribarth Fault downthrowing to the southeast, which forms a part of the Swansea Valley Disturbance. Large parts ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
