Pagans Hill Roman temple

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.

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 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.

Chew Valley School is a coeducational secondary school and sixth form situated within the Chew Valley in Somerset in South West England. It is 8 miles (13 km) south of Bristol in the village of Chew Stoke, on a 30-acre (12 ha) site in open countryside overlooking the Chew Valley Lake. It is the only secondary school in the Chew Valley area, providing further education to local children, from various local primary schools, and some pupils who live outside the catchment area. As of 2015, the school had over 1,160 pupils, including 186 in the Sixth Form.

Littleton gunpowder works between Winford and Chew Magna in the English county of Somerset, started gunpowder production around 1650 and continued until approximately 1820. It is a listed as a scheduled monument.The powder mill opened around 1740 following the expansion of the port in Bristol and increased availability of saltpetre from India. The mill was controlled by merchants based in the city and supplied gunpowder to ships sailing from the port. A previous warehouse, on the site where Bristol Temple Meads railway station now stands was considered too dangerous in the city. Despite a fire in 1755 the Littleton works expanded to become the largest gunpowder producing works in South West England by the middle of the 18th century. There was some association with another gunpowder mill at Woolley near Bath and the purchase and conversion of a snuff mill at nearby Stanton Drew was considered. It closed in the 1820s after the end of the Napoleonic Wars. It was powered by an overshot water wheel on Winford Brook a tributary of the River Chew.Some of the buildings remain intact, while others are ruined. The farmhouse was built in the mid 16th century but has been added to and revised in the 17th, 18th and 19th centuries. It is a Grade II* listed building, as is the 17th century barn. Powder Mill Cottage was built in the 18th century as the cooperage for the powder mill. The clock tower which was part of the works was originally attached to a chapel or office.

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.

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.

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.

Barns Batch Spinney (grid reference ST557659) is a 0.06-hectare geological Site of Special Scientific Interest near the village of Dundry, North Somerset, notified in 1987. The English Nature citation says that Barns Batch Spinney is important because of the exposures which it provides of the lower part of the classic Inferior Oolite limestone sequence of the Dundry area. It shows rocks lying stratigraphically below the Middle and Upper Inferior Oolite Limestones seen at Dundry Main Road South Quarry.The geology at this site provides a section spanning the division of the Middle Jurassic known as the Aalenian and Bajocian Stages and a sequence of rocks placed in the subdivision known as the discites zone, named after the characteristic fossil ammonite Hyperlioceras discites. This is one of the thickest sequences in Britain and may be used as the basis for defining these new subzones.

The Anglican Church of St. Mary and St. Peter in Winford, Somerset, England, dates from the 15th Century. It has been designated as a Grade II* listed building.The main body of the original church was rebuilt in 1796 however the tower, which was built around 1437, survives.The church consists of a nave, chancel and north and south aisles along with the four-stage west tower which is supported by set back buttresses and has a small polygonal stair turret from the roof. Around the tower is a trefoil-headed parapet with corner crocketted pinnacles and gargoyles on the corners. The tower has six bells. These were re-tuned in 2006.The interior holds a font and wooden pulpit. There is some stained glass which is decorated with heraldic shields and a canvas coat of arms beneath the tower. An unidentified monument and a Shire Monument dating from around 1764 in the churchyard are also listed.The parish is part of the benefice of Winford with Felton Common within the Diocese of Bath and Wells.

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.