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Beeston Tor
Beeston Tor () 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 Hulme End () is a small hamlet in Staffordshire, England. It is located in the Peak District National Park about 10 miles north of Ashbourne. A natural gateway to the Manifold valley, the settlement is located beside the river Manifold where .... References ...
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Beeston Tor - Geograph
Beeston may refer to: People * Beeston (surname) Places in the United Kingdom *Beeston, Bedfordshire, a hamlet *Beeston, Cheshire, a village and civil parish **Beeston Castle *Beeston, Leeds, West Yorkshire, a suburb of Leeds **Beeston railway station (West Yorkshire) *Beeston, Norfolk, a village *Beeston Regis *Beeston St Andrew *the former parish of Beeston St Lawrence now part of Ashmanhaugh *the parish of Beeston with Bittering *Beeston Beck (Norfolk), a minor watercourse *Beeston, Nottinghamshire, a town in Nottinghamshire **Beeston railway station **Beeston (UK Parliament constituency) **Beeston Urban District * Beeston Tor, Staffordshire Other uses * Beeston Brewery Company, a brewery based in Beeston, Nottinghamshire (1880–1922) See also *Breaston Breaston ( ) is a large village and civil parish in the Erewash district, in the south-east of Derbyshire and lies approximately east of the city of Derby and west of the city of Nottingham. The population of th ...
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Staffordshire
Staffordshire (; postal abbreviation Staffs.) is a landlocked county in the West Midlands region of England. It borders Cheshire to the northwest, Derbyshire and Leicestershire to the east, Warwickshire to the southeast, the West Midlands County and Worcestershire to the south and Shropshire to the west. The largest settlement in Staffordshire is Stoke-on-Trent, which is administered as an independent unitary authority, separately from the rest of the county. Lichfield is a cathedral city. Other major settlements include Stafford, Burton upon Trent, Cannock, Newcastle-under-Lyme, Rugeley, Leek, and Tamworth. Other towns include Stone, Cheadle, Uttoxeter, Hednesford, Brewood, Burntwood/Chasetown, Kidsgrove, Eccleshall, Biddulph and the large villages of Penkridge, Wombourne, Perton, Kinver, Codsall, Tutbury, Alrewas, Barton-under-Needwood, Shenstone, Featherstone, Essington, Stretton and Abbots Bromley. Cannock Chase AONB is within the county as well as parts of the ...
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River Hamps
The River Hamps is a river in Staffordshire, England. It is tributary of the River Manifold, which itself flows into the River Dove near Ilam. For much of its length the river flows through the Peak District National Park. Etymology The name Hamps derives from its Middle English title, "Hanespe" which derives from the British name, which means "summer dry", i.e. dry in summer. This is because the river disappears underground during the summer. Course The Hamps rises on the high moorland (), on the south side of Merryton Low, east of Upper Hulme. It flows south through the villages Onecote and Winkhill, then flows east, to Waterhouses and finally north to meet the Manifold under Beeston Tor. The woodlands of this last stretch are part of the National Trust's South Peak Estate. From Waterhouses to the River Manifold the valley carries the track of the former Leek and Manifold Valley Light Railway, now part of the Manifold Way, an 8-mile walk- and cycle-path. During t ...
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River Manifold
The River Manifold is a river in Staffordshire, England. It is a tributary of the River Dove (which also flows through the Peak District, forming the boundary between Derbyshire and Staffordshire). The Manifold rises at Flash Head just south of Buxton near Axe Edge, at the northern edge of the White Peak, known for its limestone beds. It continues for before it joins the Dove. For part of its course, it runs underground (except when in spate), from Wetton Mill to Ilam. During this section it is joined by its major tributary, the River Hamps. Villages on the river include Longnor, Hulme End and Ilam. Its name may come from Anglo-Saxon ''manig-fald'' = "many folds", referring to its meanders. Manifold Way The Manifold Way is an long-distance footpath from Hulme End to Waterhouses, along the former route of the narrow-gauge (2' 6") Leek and Manifold Valley Light Railway which operated between 1904 and 1934. Opened in July 1937 after the LMS handed over the trackbed t ...
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Leek And Manifold Valley Light Railway
The Leek and Manifold Valley Light Railway (L&MVLR) was a narrow gauge railway in Staffordshire, England that operated between 1904 and 1934. The line mainly carried milk from dairies in the region, acting as a feeder to the system. It also provided passenger services to the small villages and beauty spots along its route. The line was built to a narrow gauge and to the light rail standards provided by the Light Railways Act 1896 to reduce construction costs. The route of the line is now a foot- and cycle- path. Route The North Staffordshire Railway's branch from Leek ended at Waterhouses (). The L&MVLR continued from an end-on junction with this line. It ran for down the valley of the River Hamps as far as Beeston Tor, before turning up the limestone gorge that the River Manifold had formed, through to Hulme End (). The line had a large number of stations in a relatively short distance, and there were refreshment rooms at Thor's Cave and Beeston Tor. In all the lin ...
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North Staffordshire Railway
The North Staffordshire Railway (NSR) was a British railway company formed in 1845 to promote a number of lines in the Staffordshire Potteries and surrounding areas in Staffordshire, Cheshire, Derbyshire and Shropshire. The company was based in Stoke-on-Trent and was nicknamed ''The Knotty''; its lines were built to the standard gauge of . The main routes were constructed between 1846 and 1852 and ran from Macclesfield via Stoke to Colwich Junction joining the Trent Valley Railway, with another branch to Norton Bridge, just north of Stafford, and from Crewe to Egginton Junction, west of Derby. Within these main connections with other railway companies, most notably the London and North Western Railway (LNWR), the company operated a network of smaller lines although the total route mileage of the company never exceeded . The majority of the passenger traffic was local although a number of LNWR services from Manchester to London were operated via Stoke. Freight traffic was mo ...
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Manifold Way
The Manifold Way is a footpath and cycle way in Staffordshire, England. Some in length, it runs from Hulme End in the north to Waterhouses 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 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 , 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 oth ...
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Waterhouses, Staffordshire
Waterhouses is a village in the south of the Staffordshire Peak District in England. It is around 8 miles from Leek and Ashbourne, being nearly the halfway point between the two towns on the A523 road, which roughly follows the southern boundary of the Peak District National Park. Waterhouses is also a civil parish, created in 1934 when the parishes of Calton, Cauldon, Waterfall and part of Ilam were merged; previously the village of Waterhouses was on the boundary of Waterfall and Cauldon parishes. The hamlet of Winkhill is also in the parish. The population of the civil parish at the 2011 census was 1,134. Village The village of Waterhouses is on the River Hamps, a tributary of the River Manifold, and at the southern end of the track of the former Leek and Manifold Valley Light Railway (now the Manifold Way, a walk- and cycle-path), which ran to Hulme End. Nearby is the Cauldon cement plant of Lafarge Cement, and a large Tarmac limestone quarry. Waterhouses was serve ...
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Hulme End
Hulme End () is a small hamlet in Staffordshire, England. It is located in the Peak District National Park about 10 miles north of Ashbourne. A natural gateway to the Manifold valley, the settlement is located beside the river Manifold where it crosses the road from Hartington (the nearest village) to Warslow. Although in the county of Staffordshire, the hamlet lies close to the Derbyshire border, and in fact has a Derbyshire postal address, i.e. Hulme End, Hartington, Buxton, Derbyshire. The Leek and Manifold Light Railway The hamlet's primary significance stems from its position as the northern terminus of the former Leek and Manifold Valley Light Railway, an independent narrow gauge () line built following the legislation of the Light Railways Act 1896 which let companies to construct short lines to serve more isolated places. The line primarily acted as a service for milk trains and tourism. On the timetable Hulme End was described as "Hulme End for Hartington" (H ...
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Cliffs Of England
In geography and geology, a cliff is an area of rock which has a general angle defined by the vertical, or nearly vertical. Cliffs are formed by the processes of weathering and erosion, with the effect of gravity. Cliffs are common on coasts, in mountainous areas, escarpments and along rivers. Cliffs are usually composed of rock that is resistant to weathering and erosion. The sedimentary rocks that are most likely to form cliffs include sandstone, limestone, chalk, and dolomite. Igneous rocks such as granite and basalt also often form cliffs. An escarpment (or scarp) is a type of cliff formed by the movement of a geologic fault, a landslide, or sometimes by rock slides or falling rocks which change the differential erosion of the rock layers. Most cliffs have some form of scree slope at their base. In arid areas or under high cliffs, they are generally exposed jumbles of fallen rock. In areas of higher moisture, a soil slope may obscure the talus. Many cliffs also featu ...
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