Cheddar, Somerset facts for kids
Cheddar village, looking due west from the tower at Jacob's Ladder
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Cheddar is a large village and civil parish in the Sedgemoor district of the English county of Somerset. It is situated on the southern edge of the Mendip Hills, 9 miles (14 km) north-west of Wells. The civil parish includes the hamlets of Nyland and Bradley Cross. The village, which has its own parish council, has a population of 5,755 and the parish has an acreage of 8,592 acres (3,477 ha) as of 1961.
Cheddar Gorge, on the northern edge of the village, is the largest gorge in the United Kingdom and includes several show caves, including Gough's Cave. The gorge has been a centre of human settlement since Neolithic times including a Saxon palace. It has a temperate climate and provides a unique geological and biological environment that has been recognised by the designation of several Sites of Special Scientific Interest. It is also the site of several limestone quarries. The village gave its name to Cheddar cheese and has been a centre for strawberry growing. The crop was formerly transported on the Cheddar Valley rail line, which closed in the late 1960s but is now a cycle path. The village is now a major tourist destination with several cultural and community facilities, including the Cheddar Show Caves Museum.
The village supports a variety of community groups including religious, sporting and cultural organisations. Several of these are based on the site of The Kings of Wessex Academy, which is the largest educational establishment.
The name Cheddar comes from the Old English word ceodor, meaning deep dark cavity or pouch.
There is evidence of occupation from the Neolithic period in Cheddar. Britain's oldest complete human skeleton, Cheddar Man, estimated to be 9,000 years old, was found in Cheddar Gorge in 1903. Older remains from the Upper Late Palaeolithic era (12,000–13,000 years ago) have been found. There is some evidence of a Bronze Age field system at the Batts Combe quarry site. There is also evidence of Bronze Age barrows at the mound in the Longwood valley, which if man-made it is likely to be a field system. The remains of a Roman villa have been excavated in the grounds of the current vicarage.
The village of Cheddar had been important during the Roman and Saxon eras. There was a royal palace at Cheddar during the Saxon period, which was used on three occasions in the 10th century to host the Witenagemot. The ruins of the palace were excavated in the 1960s. They are located on the grounds of The Kings of Wessex Academy, together with a 14th century chapel dedicated to St. Columbanus. Roman remains have also been uncovered at the site. Cheddar was listed in the Domesday Book of 1086 as Ceder, meaning "Shear Water", from the Old English scear and Celtic dwr. An alternate spelling in earlier documents, common through the 1850s is Chedder. As early as 1130 AD, the Cheddar Gorge was recognised as one of the "Four wonders of England". Historically, Cheddar's source of wealth was farming and cheese making for which it was famous as early as 1170 AD. The parish was part of the Winterstoke Hundred.
The manor of Cheddar was deforested in 1337 and Bishop Ralph was granted a licence by the King to create a hunting forest.
As early as 1527 there are records of watermills on the river. In the 17th and 18th centuries, there were several watermills which ground corn and made paper, with 13 mills on the Yeo at the peak, declining to seven by 1791 and just three by 1915. In the Victorian era it also became a centre for the production of clothing. The last mill, used as a shirt factory, closed in the early 1950s. William Wilberforce saw the poor conditions of the locals when he visited Cheddar in 1789. He inspired Hannah More in her work to improve the conditions of the Mendip miners and agricultural workers. In 1801, 4,400 acres (18 km2) of common land were enclosed under the Inclosure Acts.
Tourism of the Cheddar gorge and caves began with the opening of the Cheddar Valley Railway in 1869.
Cheddar, its surrounding villages and specifically the gorge has been subject to flooding. In the Chew Stoke flood of 1968 the flow of water washed large boulders down the gorge, washed away cars, and damaged the cafe and the entrance to Gough's Cave.
Cheddar is twinned with Felsberg, Germany and Vernouillet, France, and it has an active programme of exchange visits. Initially, Cheddar twinned with Felsberg in 1984. In 2000, Cheddar twinned with Vernouillet, which had also been twinned with Felsberg. Cheddar also has a friendship link with Ocho Rios in Saint Ann Parish, Jamaica.
The area is underlain by Black Rock slate, Burrington Oolite and Clifton Down Limestone of the Carboniferous Limestone Series, which contain ooliths and fossil debris on top of Old Red Sandstone, and by Dolomitic Conglomerate of the Keuper. Evidence for Variscan orogeny is seen in the sheared rock and cleaved shales. In many places weathering of these strata has resulted in the formation of immature calcareous soils.
Gorge and caves
Cheddar Gorge, which is located on the edge of the village, is the largest gorge in the United Kingdom. The gorge is the site of the Cheddar Caves, where Cheddar Man was found in 1903. Older remains from the Upper Late Palaeolithic era (12,000–13,000 years ago) have been found. The caves, produced by the activity of an underground river, contain stalactites and stalagmites. Gough's Cave, which was discovered in 1903, leads around 400 m (437 yd) into the rock-face, and contains a variety of large rock chambers and formations. Cox's Cave, discovered in 1837, is smaller but contains many intricate formations. A further cave houses a children's entertainment walk known as the "Crystal Quest".
Cheddar Gorge, including Cox's Cave, Gough's Cave and other attractions, has become a tourist destination, attracting about 500,000 visitors per year. In a 2005 poll of Radio Times readers, following its appearance on the 2005 television programme Seven Natural Wonders, Cheddar Gorge was named as the second greatest natural wonder in Britain, surpassed only by the Dan yr Ogof caves.
Sites of Special Scientific Interest
There are several large and unique Sites of Special Scientific Interest (SSSI) around the village.
Cheddar Reservoir is a near-circular artificial reservoir operated by Bristol Water. Dating from the 1930s, it has a capacity of 135 million gallons (614,000 cubic metres). The reservoir is supplied with water taken from the Cheddar Yeo, which rises in Gough's Cave in Cheddar Gorge and is a tributary of the River Axe. The inlet grate for the 54-inch (1.4 m) water pipe that is used to transport the water can be seen next to the sensory garden in Cheddar Gorge. It has been designated as a Site of Special Scientific Interest (SSSI) due to its wintering waterfowl populations.
Cheddar Wood and the smaller Macall's Wood form a biological Site of Special Scientific Interest from what remains of the wood of the Bishops of Bath and Wells in the 13th century and of King Edmund the Magnificent's wood in the 10th. During the 19th century, its lower fringes were grubbed out to make strawberry fields. Most of these have been allowed to revert to woodland. The wood was coppiced until 1917. This site compromises a wide range of habitats which include ancient and secondary semi-natural broadleaved woodland, unimproved neutral grassland, and a complex mosaic of calcareous grassland and acidic dry dwarf-shrub heath. Cheddar Wood is one of only a few English stations for starved wood-sedge (Carex depauperata). Purple gromwell (Lithospermum purpurocaeruleum), a nationally rare plant, also grows in the wood. Butterflies include silver-washed fritillary (Argynnis paphia), dark green fritillary (Argynnis aglaja), pearl-bordered fritillary (Boloria euphrosyne), holly blue (Celastrina argiolus) and brown argus (Aricia agestis). The slug Arion fasciatus, which has a restricted distribution in the south of England, and the soldier beetle Cantharis fusca also occur.
By far the largest of the SSSIs is called Cheddar Complex and covers 441.3 hectares (1,090.5 acres) of the gorge, caves and the surrounding area. It is important because of both biological and geological features. It includes four SSSIs, formerly known as Cheddar Gorge SSSI, August Hole/Longwood Swallet SSSI, GB Cavern Charterhouse SSSI and Charterhouse on-Mendip SSSI. It is partly owned by the National Trust who acquired it in 1910 and partly managed by the Somerset Wildlife Trust.
Close to the village and gorge are Batts Combe quarry and Callow Rock quarry, two of the active Quarries of the Mendip Hills where limestone is still extracted. Operating since the early 20th century, Batts Combe is owned and operated by Hanson Aggregates. The output in 2005 was around 4,000 tonnes of limestone per day, one third of which was supplied to an on-site lime kiln, which closed in 2009; the remainder was sold as coated or dusted aggregates. The limestone at this site is close to 99 percent carbonate of calcium and magnesium (dolomite).
The Chelmscombe Quarry finished its work as a limestone quarry in the 1950s and was then used by the Central Electricity Generating Board as a tower testing station. During the 1970s and 1980s it was also used to test the ability of containers of radioactive material to withstand impacts and other accidents.
Along with the rest of South West England, Cheddar has a temperate climate which is generally wetter and milder than the rest of the country. The annual mean temperature is approximately 10 °C (50.0 °F). Seasonal temperature variation is less extreme than most of the United Kingdom because of the adjacent sea, which moderates temperature. The summer months of July and August are the warmest with mean daily maxima of approximately 21 °C (69.8 °F). In winter mean minimum temperatures of 1 °C (33.8 °F) or 2 °C (35.6 °F) are common. In the summer the Azores high-pressure system affects the south-west of England. Convective cloud sometimes forms inland, reducing the number of hours of sunshine; annual sunshine rates are slightly less than the regional average of 1,600 hours. In December 1998 there were 20 days without sun recorded at Yeovilton. Most the rainfall in the south-west is caused by Atlantic depressions or by convection. Most of the rainfall in autumn and winter is caused by the Atlantic depressions, which are most active during those seasons. In summer, a large proportion of the rainfall is caused by sun heating the ground leading to convection and to showers and thunderstorms. Average rainfall is around 700 mm (28 in). About 8–15 days of snowfall per year is typical. November to March have the highest mean wind speeds, and June to August have the lightest winds. The predominant wind direction is from the south-west.
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The parish has a population of 5,093, with a mean age of 43 years. Residents live in 2,209 households. The vast majority of households (2,183) give their ethnic status as white.
Culture and community
Cheddar has a number of active service clubs including Cheddar Vale Lions Club, Mendip Rotary and Mendip Inner Wheel Club. The clubs raise money for projects in the local community and hold annual events such as a fireworks display, duck races in the Gorge, a dragon boat race on the reservoir and concerts on the grounds of the nearby St Michael's Cheshire Home.
Several notable people have been born or lived in Cheddar. Musician Jack Bessant, the bass guitarist with the band Reef grew up on his parents' strawberry farm, and Matt Goss and Luke Goss, former members of Bros, lived in Cheddar for nine months as children. Trina Gulliver, eight-time World Professional Darts Champion, currently lives in Cheddar. The comedian Richard Herring grew up in Cheddar. His 2008 Edinburgh Festival Fringe show, The Headmaster's Son is based on his time at The Kings of Wessex School, where his father Keith was the headmaster. The final performance of this show was held at the school in November 2009. He also visited the school in March 2010 to perform his show Hitler Moustache. In May 2013, a community radio station called Pulse was launched.
The market cross in Bath Street dates from the 15th century, with the shelter having been rebuilt in 1834. It has a central octagonal pier, a socket raised on four steps, a hexagonal shelter with six arched four-centred openings, shallow two-stage buttresses at each angle, and an embattled parapet. The shaft is crowned by an abacus with figures in niches, probably from the late 19th century, although the cross is now missing. It was rebuilt by Thomas, Marquis of Bath. It is a Scheduled Ancient Monument (Somerset County No 21) and Grade II* listed building. In January 2000, the cross was seriously damaged in a traffic accident. By 2002, the cross had been rebuilt and the area around it was redesigned to protect and enhance its appearance. The cross was badly damaged again in March 2012, when a taxi crashed into it late at night demolishing two sides. Repair work, which included the addition of wooden-clad steel posts to protect against future crashes, was completed in November 2012 at a cost of £60,000.
Hannah More, a philanthropist and educator, founded a school in the village in the late 18th century for the children of miners. Her first school was located in a 17th-century house. Now named "Hannah More's Cottage", the Grade II-listed building is used by the local community as a meeting place.
The village is situated on the A371 road which runs from Wincanton, to Weston-super-Mare. It is approximately 5 miles (8.0 km) from the route of the M5 motorway with around a 10 miles (16 km) drive to junction 21 or 22.
It was on the Cheddar Valley line, a railway line that was opened in 1869 and closed in 1963. It became known as The Strawberry Line because of the large volume of locally-grown strawberries that it carried. It ran from Yatton railway station through Cheddar to Wells (Tucker Street) railway station and joined the East Somerset Railway to make a through route via Shepton Mallet (High Street) railway station to Witham. Sections of the now-disused railway have been opened as the Strawberry Line Trail, which currently runs from Yatton to Cheddar. The Cheddar Valley line survived until the "Beeching Axe". Towards the end of its life there were so few passengers that diesel railcars were sometimes used. The Cheddar branch closed to passengers on 9 September 1963 and to goods in 1964. The line closed in the 1960s, when it became part of the Cheddar Valley Railway Nature Reserve, and part of the National Cycle Network route 26. The cycle route also intersects with the West Mendip Way and various other footpaths.
The Church of St Andrew dates from the 14th century. It was restored in 1873 by William Butterfield. It is a Grade I listed building and contains some 15th century stained glass and an altar table of 1631. The chest tomb in the chancel is believed to contain the remains of Sir Thomas Cheddar and is dated 1442. The tower, which rises to 100 feet (30 m), contains a bell dating from 1759 made by Thomas Bilbie of the Bilbie family.
There are also churches for Roman Catholic, Methodist and other denominations, including Cheddar Valley Community Church, who not only meet at The Kings of Wessex School on Sunday, but also have their own site on Tweentown for meeting during the week. The Baptist chapel was built in 1831.
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