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Beeston Tor

Cliffs of EnglandDisused railway stations in StaffordshireEngland rail transport stubsLandforms of StaffordshireUse British English from February 2017
Beeston Tor geograph.org.uk 2392637
Beeston Tor geograph.org.uk 2392637

Beeston Tor (grid reference SK105540) is a limestone cliff in Staffordshire. It overlooks the confluence of the River Hamps with the River Manifold, and is a popular venue for rock climbing (seasonal restrictions for rock climbing apply). There was a small station here, of the same name, opened by the narrow gauge (2' 6") Leek and Manifold Valley Light Railway on 27 June 1904, whilst being entirely operated by the North Staffordshire Railway. The station had no siding – unlike most of the stations on the line – but there was a refreshment room. The line closed in 1934, and the route of the railway past the station is now designated the Manifold Way, an 8-mile walk- and cycle-path which runs from Waterhouses to Hulme End.

Excerpt from the Wikipedia article Beeston Tor (License: CC BY-SA 3.0, Authors, Images).

Beeston Tor
Manifold Track, Staffordshire Moorlands

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Geographical coordinates (GPS)

Latitude Longitude
N 53.08312 ° E -1.8447 °
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Manifold Track
ST13 7TX Staffordshire Moorlands
England, United Kingdom
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Beeston Tor geograph.org.uk 2392637
Beeston Tor geograph.org.uk 2392637
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Manifold Way
Manifold Way

The Manifold Way is a footpath and cycle way in Staffordshire, England. Some 8 miles (13 km) in length, it runs from Hulme End (53.1307°N 1.8480°W / 53.1307; -1.8480 (Manifold Way (Hulme End trailhead))) in the north to Waterhouses (53.0480°N 1.8654°W / 53.0480; -1.8654 (Manifold Way (Waterhouses trailhead))) in the south, mostly through the Manifold Valley and the valley of its only tributary, the River Hamps, following the route of the former Leek and Manifold Valley Light Railway, a 2 ft 6 in (762 mm) gauge line which closed in 1934 after a short life. The Manifold Way was opened in July 1937 by Staffordshire County Council after the LMS handed over the trackbed to them. Tarmacked throughout, and with only a slight downhill gradient from north to south, the path is also ideal for wheelchair users, prams, etc. For about 1+1⁄2 miles (2.4 km), near Wetton Mill, the original route along the former railway is shared with motor traffic where what is now a minor unclassified road has been diverted along its route. This section includes Swainsley Tunnel. However, the signed Manifold Trail is routed along the eastern bank of the river and largely avoids the on-road route. Unlike other nearby walk- and cycleways, such as the Tissington Trail and the High Peak Trail, which cross elevated areas of the Peak District, the Manifold Way follows the valley bottoms and is altogether more sheltered. The path passes through attractive scenery, and indeed tourism was one of the reasons for the original construction of the line. Popular locations along the route include Thor's Cave, the mill at Wetton Hill and Beeston Tor. A little to the east lies Dovedale, a better-known beauty spot. The Manifold Way does not pass through any significant centres of population; indeed it was once described by a railway worker as a line that started in the middle of nowhere, and ended up in the same place. Whilst the railway did serve villages and hamlets along its route, these were mostly located about a mile above the valley, a fact which contributed to the railway's ultimate demise. Whilst walking along the Manifold Way the rivers Manifold and Hamps are never far away - in fact there are dozens of small bridges crossing them. However, over the summer months the River Manifold disappears down a swallet or sink hole near Wetton Mill, to reappear some distance way, at Ilam. In all there were ten stations and halts along the line. Most had some sort of waiting room, and also a siding, but were only small affairs. The sites of the halts can be seen today, and there is also some evidence of the loading platforms, especially at Ecton, where the dairy provided much business for the railway. The valley-bottom nature of the Manifold Way offers much to see in the way of flora and fauna, and animal wildlife. Apart from the official Manifold Way route itself, the area also lends itself to many circular walking routes which utilize the route. The Manifold Way passes through some areas which comprise the South Peak Estate, land holdings owned by the National Trust. At Hulme End, the old station building has been restored as a visitor centre, and the cafe/shop at Wetton Mill is a popular spot. At Ecton Hill lie the remains of a 4,000-year-old copper mine, and the caves at Beeston Tor have revealed Neolithic and Bronze Age remains. The trackway is well maintained and there are a number of car parks and refreshment facilities (some mobile) situated at convenient intervals along its length. There are campsites at Hulme End and Wetton Village, and bikes can be hired at Waterhouses, at the southern end of the trail.

Long Low, Wetton

Long Low is a Neolithic and Bronze Age site in the English county of Staffordshire. It is about 2 km SE of Wetton (grid reference SK122539).It consists of two round cairns linked by a connecting bank – an unusual layout and one that is unique in England. The northern cairn measures 23 metres (75 ft) in diameter and survives to a height of 2.4 metres (7 ft 10 in). It appears to be related to other chamber tombs of the Peak District group and was excavated by Samuel Carrington in 1849. Carrington found a burial chamber built from limestone orthostats with a paved floor. The bones of thirteen individuals were recovered as well as three leaf-shaped flint arrowheads. The smaller southern cairn is 15 metres (49 ft) across and survives to 1.2 metres (3 ft 11 in) in height following extensive modern damage. It contained evidence of a cremation burial. Further cremations were found in the connecting bank which was built from a parallel row of limestone orthostats and is around 200 metres (660 ft) long, 10 metres (33 ft) wide and 2 metres (6 ft 7 in) high. It is now topped by a modern dry stone wall. Because of the damage to the site, its rarity and the antiquity of the Carrington excavation it is unclear as to the precise nature of the monument. It is possible that the bank is a bank barrow which had a later Neolithic chambered cairn (the north cairn) built on one end and then a Bronze Age round barrow finally added at the southern end.