Waterfall Country (Wales)

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Waterfall Country (or sometimes Waterfalls Country) (Welsh: Bro'r Sgydau) is a name often given to the upper reaches of the Vale of Neath in South Wales. The tourist area around the head of the valley has an unusually large number of publicly accessible waterfalls. The area is not officially defined but generally includes the group of falls on the Nedd Fechan, Pyrddin, Hepste and Mellte rivers, all of which lie between the villages of Pontneddfechan and Ystradfellte in the Brecon Beacons National Park. [1]

Contents

Each of these falls lies within or on the boundary of the county of Powys. A few miles further west are Henrhyd Falls on the Nant Llech, a tributary of the Tawe and to the south-west are Melin Court Falls on the Melin Court Brook, a tributary of the River Neath. These, along with Aberdulais Falls on the Dulais, a further tributary of the Neath are also encompassed by the term 'Waterfall/s Country' by some writers.

Collectively the falls are one of the more popular natural attractions in South Wales, which has caused problems of erosion in the vicinity of many of the falls. Most occupy locations designated as sites of special scientific interest and as special areas of conservation which aim to protect the biodiversity and geodiversity of these sites. The designations place a duty on the landowners and managers to protect the sites and so various erosion control measures have been put in place in an attempt to counter the worst problems.

Origins

Virtually all of the falls occur on tributaries of the River Neath occupying valleys that have been deeply incised into the landscape. It is suggested that overdeepening of the Vale of Neath by glacier ice during the succession of ice ages has resulted in these tributaries cutting down into their own beds as they adjust to a base level lower than in pre-glacial times. The underlying geology is a generally southerly dipping succession of Carboniferous age sandstones and mudstones assigned by geologists to the Marros Group and formerly referred to as the Millstone Grit Series. Preferential erosion, whereby the less resistant mudstones have been more readily removed by the passage of water, often following various forms of weathering, has left sandstones forming the lips of the falls. The siting of individual falls is closely linked in many cases to the presence of northwest–southeast–aligned faults that have brought different lithologies into proximity. [2]

The Falls

On the Afon Mellte

Sgwd Clun-gwyn (Sgwd Uchaf Clun-gwyn) in high flow conditions Sgand^373,d Uchaf Clyn Glyn - geograph.org.uk - 70655.jpg
Sgwd Clun-gwyn (Sgwd Uchaf Clun-gwyn) in high flow conditions
uppermost fall of the complex Sgwd Isaf Clun-gwyn Sgand^373,d Isaf Clun-Gwyn - geograph.org.uk - 14634.jpg
uppermost fall of the complex Sgwd Isaf Clun-gwyn
Sgwd y Pannwr Sgwd y Pannwr falls.jpg
Sgwd y Pannwr

There are three waterfalls of note on this river though several other lesser falls can also be found along its length. [3]

On the Afon Hepste

Sgwd yr Eira in full flow Sgwd yr Eira in full flow - geograph.org.uk - 70398.jpg
Sgwd yr Eira in full flow

Sgwd yr Eira - famous for being the falls behind which you can walk, the 'falls of snow' plunge over a hard band of sandstone whose overhang protects the walker from the full force of the water. The closure of the path behind this most popular of falls during much of 2007 and 2008 on safety grounds was controversial. Stabilisation works agreed between the then landowners, the Forestry Commission and the Countryside Council for Wales and the Brecon Beacons National Park Authority allowed the route to be re-opened later in 2008. For a walk taking in Sgwd Clun-gwyn, Sgwd Isaf Clun-gwyn and Sgwd yr Eira see 'Waterfall Walk' under Ystradfellte.

On the Nedd Fechan

There are three falls of particular interest to visitors on this river, though like the Mellte, there are other lesser falls. [3]

On the Afon Pyrddin

Sgwd Gwladus 2014-07-30

On other rivers

More falls occur in the section of the river above the cascade. These falls can be viewed from the north bank which is publicly accessible. A further small fall at Pwll y Crochan near where the A465 Heads of the Valleys Road crosses the river though this spot is not accessible to the public.
The Nant Llech rises on the southern slopes of Carreg Cadno and flows to the village of Coelbren at which point it drops 90 feet (27 m) over the lip of a faulted block of the Farewell Rock, a hard sandstone. This spectacular site and section of the gorge below the falls is owned and managed by the National Trust. The waterfall is referred to in Welsh as Sgwd Henryd or as Rhaeadr Henryd.
The Dulais rises near the coalmining town of Aberdulais/Seven Sisters and flows for several miles to join the waters of the River Neath at Aberdulais. The falls are set only 160 yards (150 metres) up the river from that confluence (at OS grid ref SS772995) and are readily accessible from the A465 road which runs the length of the Vale of Neath. Not only is this a spectacular fall but also an important industrial heritage site which is now in the care of the National Trust. [5]
Melin Court Brook rises on the high ground to the southeast of Resolven in the Vale of Neath. It drops from the plateau surface above 450 metres (1,480 ft) above sea level to the floor of the Vale of Neath at around 30 metres (98 ft) in the space of just under 5 kilometres (3.1 mi). Several falls occur over its course but the single big drop of 80 feet (24 m) at Melincourt (OS grid ref SN826016) is the most spectacular and has drawn visitors for over 200 years since it was painted by Turner in 1794.
The falls (otherwise known as Melincwrt Falls), can be viewed from above, where a minor public road bridges the brook immediately upstream of the drop, and from below by means of a footpath which runs up beside the brook from the B4334 road between Melincourt village and Resolven.
The falls are contained within a 13-acre (5 ha) nature reserve managed by the Wildlife Trust of South and West Wales. Neath Port Talbot County Borough Council provide car parking beside the road at the start of the path up the falls. [6]

Information and interpretation for visitors

The Brecon Beacons National Park Authority established a visitor centre at Pontneddfechan in 2008 making use of a building previously used by Neath Port Talbot County Borough Council as a tourist information centre. Renamed as the Waterfalls Centre, it was staffed throughout the year to provide information for visitors to Waterfall Country, the wider national park and the Fforest Fawr Geopark. The Authority announced it was to close permanently on 6 June 2016 [7] after a 4.7% cut in funding to the park authority. There were plans in 2017 to convert the centre into a cafe. [8] The cafe is now operational and offers some information on the area to its clients. There is a smaller visitor facility a few miles to the north operated by the National Park Authority at Cwm Porth near Ystradfellte. [9]

The National Trust operate a centre at Aberdulais Falls which performs a similar role.

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The Aberdulais Falls are found on the River Dulais at Aberdulais, near Neath in the county borough of Neath Port Talbot, Wales. The falls are formed as the river plunges over beds of hard Lower Pennant Sandstone just before meeting the River Neath flowing down the Vale of Neath. They are home to Europe's largest electricity-generating water wheel.

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Melincourt Falls is an 80 feet (24 m) high waterfall on Melin Court Brook, a left-bank tributary of the River Neath / Afon Nedd, located 1-mile (1.6 km) south of Resolven in the county borough of Neath Port Talbot, south Wales. It is formed where the brook plunges over a resistant band of 'Lower Pennant Sandstone' in a 13 acres (5.3 ha) nature reserve managed by the Wildlife Trust of South and West Wales. The falls have been drawing visitors for at least two centuries – they are certainly known to have inspired J. M. W. Turner to paint them in 1794. The falls are considered by some to constitute a part of Waterfall Country though the bulk of these falls are a few miles further northeast at the head of the Vale of Neath.

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The Afon Dringarth is a river in Powys, Wales and wholly contained within the Brecon Beacons National Park. Its headwater streams drain the eastern slopes of Fan Dringarth, the southern slopes of Craig Cerrig-gleisiad and the western slopes of Fan Fawr. The river flows south-southwest for about 6 km / 3.5 mi to its confluence with the Afon Llia one mile north of the village of Ystradfellte, continuing south as the Afon Mellte. The river may derive its name from the hill immediately to its west, Fan Dringarth.

The Nant Llech is a minor river in Powys, Wales and which lies wholly within the Brecon Beacons National Park. The name means 'slab stream', presumably in reference to the sandstones across which it runs. Its headwater streams, the Nant Llech Pellaf and the Nant Llech Isaf join forces at Blaen Llech and then continue westwards as the Nant Llech for 3 km / 2 mi to a confluence with the River Tawe just east of the village of Abercraf.

Fforest Fawr Geopark is a Geopark in the Brecon Beacons National Park, south Wales. It is the first designated Geopark in Wales having gained membership of both the European Geoparks Network and the UNESCO-assisted Global Network of National Geoparks in October 2005. The Geopark aims to promote and support sustainable tourism and other opportunities to improve the economy of the area whilst safeguarding the natural environment. Its aims largely coincide with the statutory duties and purpose of the National Park within which it sits.

<span class="mw-page-title-main">Moel Penderyn</span> Hill (371m) in Rhondda Cynon Taf, Wales

Moel Penderyn is a hill on the edge of Penderyn village, in the Brecon Beacons National Park in the county borough of Rhondda Cynon Taff, south Wales. It also appeared on older maps as 'Y Foel Penderyn'. Its summit at 371m is marked by a trig point.

Hirfynydd is a 481-metre-high hill in Neath Port Talbot county borough in South Wales. A Roman road, Sarn Helen, runs along its entire northeast–southwest ridge-line, a route followed by a modern-day byway. To its west is Cwm Dulais and to its southeast is the Vale of Neath. The northern end of the ridge falls away to a broad upland vale containing the Afon Pyrddin and beyond which is the Brecon Beacons National Park.

This article describes the geology of the Brecon Beacons National Park in mid/south Wales. The area gained national park status in 1957 with the designated area of 1,344 km2 (519 sq mi) including mountain massifs to both the east and west of the Brecon Beacons proper. The geology of the national park consists of a thick succession of sedimentary rocks laid down from the late Ordovician through the Silurian and Devonian to the late Carboniferous period. The rock sequence most closely associated with the park is the Old Red Sandstone from which most of its mountains are formed. The older parts of the succession, in the northwest, were folded and faulted during the Caledonian orogeny. Further faulting and folding, particularly in the south of the park is associated with the Variscan orogeny.

References

  1. "Visiting Waterfall Country". Brecon Beacons National Park Authority. Retrieved 5 December 2023.
  2. Owen, T.R. (1973). Geology Explained in South Wales. David & Charles. ISBN   978-0715358603.
  3. 1 2 "Walking trails in Waterfall Country - Brecon Beacons National Park, Wales". Archived from the original on 18 May 2017. Retrieved 18 May 2017.
  4. Jones, John Llewelyn (1986). The Waterfalls of Wales (First ed.). London: Robert Hale Ltd. p. 49. ISBN   070902584X.
  5. "Aberdulais Tin Works and Waterfall". National Trust. Retrieved 15 February 2014.
  6. "Melincourt Waterfalls, Resolven". Neath Port Talbot County Borough. Retrieved 15 February 2014.
  7. [ dead link ]
  8. David Higgs (16 April 2017) Former visitor centre at Welsh beauty spot could become cafe and lodge, Wales Online. Retrieved 8 October 2017.
  9. "CWM Porth Information Point - Brecon Beacons National Park, Wales". Archived from the original on 9 June 2017. Retrieved 18 May 2017.

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