Stainforth Bridge | |
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Coordinates | 54°06′00″N2°16′48″W / 54.100°N 2.280°W Coordinates: 54°06′00″N2°16′48″W / 54.100°N 2.280°W |
OS grid reference | SD818672 |
Crosses | River Ribble |
Locale | Stainforth, North Yorkshire, England |
Other name(s) | Stainforth Packhorse Bridge Knight Stainforth Bridge |
Characteristics | |
Total length | 57 feet (17.4 m) |
Width | 7 feet 2 inches (2.18 m) [note 1] |
Height | 5.3 metres (17 ft) [note 2] |
No. of spans | 1 |
History | |
Opened | c. 1675 |
Location | |
Stainforth Bridge, (also known as Stainforth packhorse bridge and Knight Stainforth bridge) is a 17th century, arched packhorse bridge over the River Ribble in Stainforth, North Yorkshire, England. The bridge was formerly on the main packhorse road between York and Lancaster, which has been superseded by later roads. It was in private ownership until the 1930s, when it was taken on by the National Trust. It is now a grade II listed structure and provides access to Stainforth Force, which is just below the bridge.
The bridge was built by Samuel Watson c. 1675, [note 3] a local Quaker who owned Knight Stainforth Hall, a Jacobean house which was nearby. [4] [5] [6] Previous to this, the site was a ford which was impassable during times of flood, and a local legend suggests that the crossing was used by the Romans. [7] [8] The bridge carries a minor road, Dog Hill Brow, over the river connecting Knight and Little Stainforth. [9] Besides being a Medieval road linking York and Lancaster, and a monastic route taken by monks between their houses in Yorkshire and the Lake District, the route was also a packhorse road connecting Clapham with Malham. [10] [11] A covenant was drawn up in the year of the bridge's building stating that people on foot, or with carts and cattle, had "free passage between the towns of Knight Stainforth and Stainforth Under Bargh." [12] The bridge was built by using tradesmen from Stainforth-under-Bargh (now the main village of Stainforth), and in return, the people of Stainforth were afforded full usage rights, as the bridge was also a necessity locally. [13]
Both of the bridge abutments are set into solid rock and the bridge itself is 17.4 metres (57 ft) long and 5.3 metres (17 ft) at its highest point above the normal water level. [14] At its widest point, it reaches 7 feet 2 inches (2.18 m). [15] The limestone that the bridge is built on, is part of the Kilnsey Limestone, which is younger than the Chapel House limestone underneath Stainforth Force, which is only 100 yards (91 m) below the bridge. [16] [17]
On 23 September 1931, the bridge went from private ownership into the National Trust, helped by an endowment by the previous owners. Doubts had been expressed about the structure after heavy motor vehicles had been using it, causing the bridge to be weakened. [18] It was thought that the National Trust could enforce restrictions on heavy goods vehicles more effectively than private owners. [8]
The bridge was registered in 1988 by Historic England as a Grade II listed structure under the name of Knight Stainforth Bridge. [19]
Craven is a local government district of North Yorkshire, England centred on the market town of Skipton. In 1974, Craven District was formed as the merger of Skipton urban district, Settle Rural District and most of Skipton Rural District, all in the West Riding of Yorkshire. The population of the Local Authority area at the 2011 Census was 55,409. It comprises the upper reaches of Airedale, Wharfedale, Ribblesdale, and includes most of the Aire Gap and Craven Basin.
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Ribblesdale is one of the Yorkshire Dales in England. It is the dale or upper valley of the River Ribble in North Yorkshire. Towns and villages in Ribblesdale include Selside, Horton-in-Ribblesdale, Stainforth, Langcliffe, Giggleswick, Settle, Long Preston and Hellifield. Below Hellifield the valley of the river is generally known as the Ribble Valley.
Long Preston is a village and civil parish in the Craven district of North Yorkshire, England, in the Yorkshire Dales. It lies along the A65 road, and is 12 miles (19 km) from Skipton and 4 miles (6 km) from Settle. The population of Long Preston in 2001 was 680, increasing to 742 at the 2011 Census.
Stainforth is a village and civil parish in the Craven district of North Yorkshire, England. It is situated north of Settle. Nearby there is a waterfall, Stainforth Force, where the river falls over limestone ledges into a deep, broad pool which can be accessed by walking a short way from the village. There was a Youth Hostel at Taitlands between 1942 and 2007.
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Dent Marble is a highly polished form of limestone which occurs in the Dentdale district of Cumbria in England. The stone is noted for the presence of fossils which gives it its distinctive look. The stone is actually a crinoidal limestone and is not a true marble, but is known as a marble because it polished quite well. Dent Marble has been used for staircases, floors and hearths in railway stations and large buildings in England, Australia and Russia. The trade died out when import tariffs on Italian marble were relaxed, and Dent Marble became less popular.
Horton Quarry is a limestone quarry near to Horton-in-Ribblesdale, North Yorkshire, England. The quarry, which is some 6 miles (9.7 km) north of Settle, has been operating since at least 1889, and produces limestone for a variety of purposes. Stone used to be exported from the quarry by rail, but now leaves by lorry, although there are plans to re-instate the railway sidings. The quarry used to produce its own lime by roasting the limestone in big kilns on the site, but the last of these were removed in the 1980s. Since 2000, the quarry has been owned and operated by Hanson.
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Crummackdale,, is a small valley north of the village of Austwick in the Craven District of North Yorkshire, England. The Valley is drained by Austwick Beck, which flows into the River Wenning, which in turn heads westwards to empty into the Irish Sea. Crummackdale is a narrow south west facing dale, at the south west corner of the Yorkshire Dales National Park.
Stainforth Force, is a 2.5-metre high cascade waterfall on the River Ribble at Stainforth, 3 miles (5 km) north of Settle in North Yorkshire, England. The waterfall is a popular tourist attraction in autumn when salmon are migrating up the river.
The geology of the Yorkshire Dales National Park in northern England largely consists of a sequence of sedimentary rocks of Ordovician to Permian age. The core area of the Yorkshire Dales is formed from a layer-cake of limestones, sandstones and mudstones laid down during the Carboniferous period. It is noted for its karst landscape which includes extensive areas of limestone pavement and large numbers of caves including Britain's longest cave network.
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