This is a links page to the named waterfalls found in the UK and includes a list of the highest waterfalls.
The list of highest waterfalls is often controversial, due to the ambiguity of whether to measure the single largest fall or the sum of a series of falls, and many falls make false claims to the record. This table lists above-ground waterfalls by tallest single drop (not necessarily unbroken).
Waterfall | Location | Height (metres) | |
---|---|---|---|
1 | Eas a' Chual Aluinn | Scotland | 200 |
2 | Steall waterfall | Scotland | 120 |
3 | Falls of Glomach | Scotland | 113 |
4 | Devil's Appendix | Wales | 93 |
5 | Pistyll y Llyn | Wales | 91 |
6 | Cautley Spout | England | 76 |
7 | Pistyll Rhaeadr | Wales | 73 |
8 | Canonteign Falls | England | 70 |
9 | Falls of Foyers | Scotland | 62 |
10 | Cauldron Snout | England | 60 |
A more complete list of waterfalls in England is available at List of waterfalls of England.
A more complete list of waterfalls in Scotland is available at List of waterfalls of Scotland.
A more complete list of waterfalls in Wales is available at List of waterfalls of Wales.
Waterfalls in Northern Ireland.
Llanrhaeadr-ym-Mochnant is a village, community and an ecclesiastical parish in the extreme north of Powys, Wales; about 9 miles west of Oswestry and 12 miles south of Llangollen, on the B4580. It lies near the foothills of the Berwyn mountains on the river Rhaeadr. At the top end of the valley is the Pistyll Rhaeadr waterfall, one of the Seven Wonders of Wales in the old rhyme. One mile north of the town is the hill Moel Hen-fache. The community includes the hamlet of Llanarmon Mynydd Mawr.
Ystradfellte is a village and community in Powys, Wales, about 6 miles (10 km) north of Hirwaun, with 556 inhabitants. It belongs to the historic county of Brecknockshire (Breconshire) and the Fforest Fawr area of the Brecon Beacons National Park, beside the Afon Mellte river. The village is linked by minor roads with Heol Senni to the north and the A4059 north of Penderyn, and with Pontneddfechan, which lies in the community, at the head of the Vale of Neath to the south.
Devil's Bridge is a village and community in Ceredigion, Wales. Above the River Mynach on the edge of the village is a series of three stacked bridges, constructed hundreds of years apart, from which the village gets its English name.
The River Mellte is a river in south Wales. It is formed by the confluence of the Afon Llia and the Afon Dringarth. It then flows south through the village of Ystradfellte to Pontneddfechan where it joins with the Nedd Fechan to become the River Neath. The river derives its name from 'mellt' - the Welsh word for 'lightning' - after its tendency to rise and fall rapidly in response to heavy rainfall.
The River Conwy is a river in north Wales. From its source to its discharge in Conwy Bay it is 55 kilometres (34 mi) long and drains an area of 678 square km. "Conwy" was formerly anglicised as "Conway."
The Afon Mawddach is a river in Gwynedd, Wales, which has its source in a wide area SH820300 north of Dduallt in Snowdonia. It is 28 miles (45 km) in length, and is much branched; many of the significant tributaries are of a similar size to the main river. The catchment area is bounded to the east by the Aran Fawddwy massif and to the west and north by the Harlech dome which forms a watershed just south of Llyn Trawsfynydd.
Afon Ogwen is a river in north-west Wales draining from some of the greatest peaks in Snowdonia before discharging to the sea on the eastern side of Bangor, Gwynedd.
Pistyll Rhaeadr is a waterfall 4 miles from the village of Llanrhaeadr-ym-Mochnant in Powys, Wales, and 16 miles west of Oswestry.
The River Dwyryd, is a river in Gwynedd, Wales which flows principally westwards; draining to the sea into Tremadog Bay, south of Porthmadog.
The Afon Clun is a 14-mile (23 km) long tributary of the River Ely, in the counties of Cardiff and Rhondda Cynon Taf, Wales. Its bedrock is predominantly of sandstone. Beginning on the western slope of The Garth the river is fast-flowing, in clear shallow water with a hard substrate, flowing to the south of Llantrisant and generally west to its confluence with the River Ely at Pontyclun, falling 715 feet (218 m) over its course.
The Nedd Fechan is a river almost wholly within the county of Powys, Wales, currently administered as part of the unitary authority of Powys. It rises on the eastern slopes of Fan Gyhirych in the Fforest Fawr section of the Brecon Beacons National Park and flows south for 7 miles (12 km) to join with the Afon Mellte at Pontneddfechan, their combined waters continuing as the River Neath to the sea near Swansea. The only significant tributary of the Nedd Fechan is the Afon Pyrddin which joins it at Pwll Du ar Byrddin. Downstream of this confluence it forms the boundary between Powys to its east and Neath Port Talbot to its west.
Waterfall Country 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.
The Rhaeadr y Cwm is a waterfall on the Afon Cynfal river in Gwynedd, North Wales. The falls are located near the B4391 road, some 3 miles (5 km) east of Ffestiniog.
The Tanat Valley is a large valley in northern Powys, Wales, formed by the course of the Afon Tanat and its tributaries. Situated south of the Berwyn range, the valley forms from at Llangynog from the merger of two narrow valleys, the Cwm Pennant and Cwm Rhiwarth. Various historic sites, including the Iron Age hillfort Llwyn Bryn-Dinas and the medieval St Melangell's Church are located along the valley. Largely agrarian, sheep farming has formed a major industry in the region for several centuries. Large-scale slate and lead mining in the region lasted from the 16th to late 20th century, although earlier mines possibly existed during the Iron Age.