Ingleton Waterfalls Trail is a well-known circular trail beginning and ending in the village of Ingleton in the English county of North Yorkshire, now maintained by the Ingleton Scenery Company. It is claimed that the trail, some 8 kilometres (5 mi) long, and with a vertical rise of 169 m (554 feet) has some of the most spectacular waterfall and woodland scenery in the north of England. It is on private land and an entrance fee is charged.

1. Beginnings

Following a number of articles in the Lancaster Guardian and other newspapers about the scenery in and around Ingleton, public interest led to the creation of the trail in an area which was previously hidden from view. Paths and bridges were built and the trail opened on Good Friday, 11 April 1885. The presence of Ingleton railway station played a major role in the early success of the trail, attracting visitors from Bradford, Manchester and Leeds.

1. Geology

Ingleton lies on the North and South Craven fault, exposing Carboniferous and Ordovician rocks. The Ingletonian rock has been classified as Ordovician.

1. The walk

Starting in the Broadwood car park the trail takes walkers along the banks of the River Twiss, through Swilla Glenn with its coin embedded tree and on to Pecca Falls, Pecca Twin Falls, Holly Bush Spout and Thornton Force. A footbridge bridge crosses the Twiss and leads on to Twistleton Lane, which crosses out of the valley of the River Twiss at 285 metres (934 ft). Following Twistleton Lane down past Scar End Farm and Twistleton Hall the walk crosses Oddies Lane to Beezley's Farm.

Past Beezley's the trail starts its descent along the banks of the River Doe. This river emerges near God's Bridge close to the settlement of Chapel-le-Dale and flows gently until it reaches the waterfalls walk at Beezley's Falls Triple Spout (with its three waterfalls side-by side). As the trail continues, you look down 18 metres (59 feet) onto Rival Falls and then onto Baxenghyll Gorge, Snow Falls and finally walk through Twistleton Glen and back to Ingleton. In Ingleton, the Twiss and the Doe meet to form the River Greta, which in turn flows into the River Lune. English Nature designated the River Twiss and River Doe areas of the Waterfalls Trail as a Site of Special Scientific Interest (SSSI) due to the interesting plants and animals and the geological structures located there.

1. See also

List of waterfalls List of waterfalls in England

1. References

Bibliography CPGS (2003). "Ingleton Waterfalls trail" (PDF). Craven and Pendle Geological Society. Archived from the original (PDF) on 12 May 2013. Retrieved 5 March 2014.

1. External links

Ingleton Waterfalls Trail Lancaster Guardian Natural England Detailed Walk description on Car Free Walks

Nearby Places View Menu
Location Image
116 m

River Doe

The River Doe is a river in North Yorkshire, England. The river's source is near God's Bridge close to the settlement of Chapel-le-Dale and flows through Twisleton in a south-westerly direction to Ingleton, where it meets the River Twiss to form the River Greta. The river forms part of the River Lune system that flows into the Irish Sea.
Location Image
146 m

River Twiss

The River Twiss is a river in the county of Yorkshire, England. The source of the river is Kingsdale Beck, which rises at Kingsdale Head at the confluence of Back Gill and Long Gill in the Yorkshire Dales. Beneath Keld Head, the river changes its name to the River Twiss. It has two notable waterfalls, Thornton Force and Pecca Falls, and its course follows part of the Ingleton Waterfalls Walk, then through Swilla Glen to Thornton in Lonsdale and down to Ingleton, where it meets the River Doe to form the River Greta. The English landscape artist J. M. W. Turner was a frequent visitor to the area, and his sketch of Thornton Force in 1816 is currently part of the Tate collection.
Location Image
191 m

St Mary's Church, Ingleton

St Mary's Church is the parish church of Ingleton, North Yorkshire, a village in England. There was a church on the site by the 12th century. The oldest part of the current building is the tower, dating from the 15th century. Between 1886 and 1887 the remainder of the church was rebuilt, to a Decorated Gothic-style design, by Cornelius Sherlock. The building was grade II* listed in 1958. The church is built of stone with a slate roof, and consists of a nave with a clerestory, north and south aisles, a south porch, a chancel with a north vestry, and a west tower. The tower has three stages, diagonal buttresses, a west doorway with a pointed arch, a chamfered surround and a hood mould, above which is a three-light window, a south clock face, two-light bell openings, a string course, and an embattled parapet with corner finials. Inside, some fragments of wall painting survive, but the highlight is the 12th century font, described by Nikolaus Pevsner as "one of the best in the West Riding". It is cylindrical, and is carved with an arcade design, with fourteen Biblical scenes. It was rediscovered in the 18th century, cleaned and brought back into use in 1830, and mounted on its current base in 1858.
249 m

Ingleton railway station (London and North Western Railway)

Ingleton (L&NW) railway station (also known as Ingleton Thornton station) was one of two stations serving the village of Ingleton, North Yorkshire, England. It owed its existence to the intense rivalry between the two stations' owners. It opened, along with the Ingleton Branch Line, in 1861, and closed in 1917, by which time the two railway companies had become more cooperative.