Chew Valley School

Chew Magna Reservoir is a 5-acre (2 ha) reservoir on the western outskirts of the village of Chew Magna, Somerset, England. It lies just north of the B3130 Winford Road. The reservoir was created by damming Winford brook in order to supply water for villages in the Chew Valley. It is owned and managed by Bristol Water. Chew Magna reservoir provides fly fishing for stocked brown trout (Salmo trutta morpha fario) and rainbow trout (Oncorhynchus mykiss). Rainbows can be fished all year. Parking is close to the lake and there are many stagings erected around the lake. In 2011 the reservoir emptied following a long period without sustained rainfall. Bristol Water rescued the trout and transferred them to the nearby Chew Valley Lake.

The Manor House in Chew Magna, Somerset, England, was a country house built in the middle of the 17th century. It was the principal residence of the Adlam family from the mid-1800s until 1940. The house is a Grade II* listed building and formed part of the Sacred Heart Convent School. It has now been redeveloped and returned to residential use.

The Rectory in Chew Stoke, Somerset, England was built in 1529. It is a Grade II* listed building.It was built in 1529 for Sir John Barry, who was the rector between 1524 and 1546 of the nearby St Andrew's Church. It has undergone substantial renovations including the addition of a clock tower for the Rev. W.P. Wait, which has since been removed and further alterations c.1876 for Rev. J. Ellershaw. The building has an ornate south front with carvings of shields bearing the coat of arms of the St Loe family, who were once chief landowners in the area, alone or impaled with arms of Fitzpane, Ancell, de la Rivere and Malet. Towards the end of the 18th century a new rectory was built in the village and this building became a private house. In 1945 it started to be used again as the rectory. It was sold by the church in 2008 and is now a private dwelling again.

The Pagans Hill Roman Temple was a Romano-British-style temple (Romano-Celtic temple) excavated on Pagans Hill at Chew Stoke in the English county of Somerset.

The Church of St Andrew in Chew Magna, Somerset, England dates from the 12th century with a large 15th-century pinnacled sandstone tower, a Norman font and a rood screen that is the full width of the church. It is a Grade I listed building.

The Old School Room in Chew Magna, Somerset, England was built around 1510. It is a Grade II* listed building.It was built as a church house for the neighbouring Church of St Andrew. The upstairs room was the local school from the mid or early 15th century, with the village poorhouse below. The ground floor was divided into cubicles which housed the destitute and occasionally prisoners. It also served as the meeting place of the Court leet. The building was declared unsafe in 1965. In 1971 the building underwent major renovation, which included replacement of oak beams supporting the upper floor were replaced and preservation work on the wooden roof carried out. The building was then used as a youth club until it was purchased by the parish council in 1981 as a village hall. Since then it has been a venue for social activity in the village.

Chew Magna is a village and civil parish within the Chew Valley in the unitary authority of Bath and North East Somerset, in the ceremonial county of Somerset, England. The parish has a population of 1,149.To the south of the village is Chew Valley Lake. The village is on the B3130 road, about 10 miles (16 km) from Bristol, 15 miles (24 km) from Bath, 13 miles (21 km) from the city of Wells, and 6 miles (10 km) from Bristol Airport. The village is close to the northern edge of the Mendip Hills (a designated Area of Outstanding Natural Beauty), and was designated a conservation area in 1978. There are many listed buildings reflecting the history of the village. The River Chew flows through the village. Just outside the village is Chew Magna Reservoir: this small Bristol Water supply reservoir intercepts the Winford Brook. There is one primary school, and an adjacent secondary school, several shops and small businesses, three churches, and three pubs serving the area. There is also a football pitch and children's play area. The village frequently wins regional categories in the Calor Village of the Year competition, and is currently moving towards zero waste status, having been described as "probably the greenest parish in Britain".

Chew Stoke is a small village and civil parish in the affluent Chew Valley, in Somerset, England, about 8 miles (13 km) south of Bristol and 10 miles north of Wells. It is at the northern edge of the Mendip Hills, a region designated by the United Kingdom as an Area of Outstanding Natural Beauty, and is within the Bristol/Bath green belt. The parish includes the hamlet of Breach Hill, which is approximately 2 miles (3.2 km) southwest of Chew Stoke itself. Chew Stoke has a long history, as shown by the number and range of its heritage-listed buildings. The village is at the northern end of Chew Valley Lake, which was created in the 1950s, close to a dam, pumping station, sailing club, and fishing lodge. A tributary of the River Chew, which rises in Strode, runs through the village. The population of 991 is served by one shop, one working public house, a primary school and a bowling club. Together with Chew Magna, it forms the ward of Chew Valley North in the unitary authority of Bath and North East Somerset. Chew Valley School and its associated leisure centre are less than a mile (1.6 km) from Chew Stoke. The village has some areas of light industry but is largely agricultural; many residents commute to nearby cities for employment.

Chew Court is a Grade II* listed building next to St Andrew's church in Chew Magna, Somerset, England.It was originally a palace for Gisa the Bishop of Bath and Wells, however little of the original building survives. After use by a succession of bishops it was sold to the Duke of Somerset. The oldest portion is the gatehouse at the southern end of the east wing.The house was largely rebuilt in 1656, from which a little survives as the Chew Court of today including an Elizabethan doorway with Doric pilasters. The room over the gatehouse is said to have been used as a court-room, with the turrets used for holding prisoners. The house now forms an "l" shape of two wings.In 2011 alterations were made to the driveway leading to the house and additional walls built around the gardens.About 45 metres (148 ft) south west of the building is a medieval well, which was later enclosed with a sandstone well house.

The Chew Valley is an affluent area in North Somerset, England, named after the River Chew, which rises at Chewton Mendip, and joins the River Avon at Keynsham. Technically, the area of the valley is bounded by the water catchment area of the Chew and its tributaries; however, the name Chew Valley is often used less formally to cover other nearby areas, for example, Blagdon Lake and its environs, which by a stricter definition are part of the Yeo Valley. The valley is an area of rich arable and dairy farmland, interspersed with a number of villages. The landscape consists of the valley of the River Chew and is generally low-lying and undulating. It is bounded by higher ground ranging from Dundry Down to the north, the Lulsgate Plateau to the west, the Mendip Hills to the south and the Hinton Blewett, Temple Cloud, Clutton and Marksbury plateau areas to the east. The valley's boundary generally follows the top of scarp slopes except at the southwestern and southeastern boundaries where flat upper areas of the Chew Valley grade gently into the Yeo Valley and eastern Mendip Hills respectively. The River Chew was dammed in the 1950s to create Chew Valley Lake, which provides drinking water for the nearby city of Bristol and surrounding areas. The lake is a prominent landscape feature of the valley, a focus for recreation, and is internationally recognised for its nature conservation interest, because of the bird species, plants and insects. The area falls into the domains of councils including Bath and North East Somerset, North Somerset and Mendip. Part of the area falls within the Mendip Hills Area of Outstanding Natural Beauty. Most of the undeveloped area is within the Bristol/Bath Green Belt. Many of the villages date back to the time of the Domesday Book and there is evidence of human occupation since the Stone Age. There are hundreds of listed buildings with the churches being Grade I listed. The main commercial centre is Chew Magna.

Knowle Hill (grid reference ST583613) is a hill in the Chew Valley, Somerset, England situated between the village of Chew Magna and Chew Valley Lake. The south side of the summit of Knowle Hill is home to the grass Wood Small-reed (Calamagrostis epigejos). The population of this plant forms a circular patch some 20 metres wide, which is visible from Bishop Sutton 1.2 km south across Hollow Brook. It has been suggested that this patch is a single clone which has spread by means of underground rhizomes, and may be 200 years old.The hill is declared open access land under the Countryside and Rights of Way Act 2000 and is on the route of the Chew Valley Three Peaks walk, and the Two Rivers Way.

Dundry Main Road South Quarry (grid reference ST566654) is a 0.7 hectare geological Site of Special Scientific Interest near the village of East Dundry, North Somerset, notified in 1974. The quarry was cited in the 19th century by d'Orbigny as the English "type section" for the Inferior Oolite. Dundry has long been a famous palaeontological and stratigraphic locality. The type locality for many species of molluscs and brachiopods, as well as other lesser groups, it is renowned as one of the world's most fossiliferous exposures with well over two hundred species recorded. The Main Road Quarry exposes a fine section in the Middle and Upper Inferior Oolite, with the rocks lying stratigraphically below them visible at Barns Batch Spinney. The former characterised by a typically southern English-Normandy fauna, including the rich ammonite occurrences of the "Brown iron-shot", and the latter by contrasting faunas of Cotswold aspect. This contrast is direct evidence for movements of the Mendip Axis in Middle Jurassic times, making this an outstanding site for its bearing on studies of palaeogeography.