Littleton gunpowder works

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.

Winford is a village and civil parish within the Chew Valley, Somerset, England. It is within the unitary authority of North Somerset about 8 miles (12.9 km) south of Bristol. The parish has a population of 2,153.The parish includes the village of Felton which is close to the A38, Bristol International Airport and Hartcliff Rocks Quarry and Lulsgate Quarry Sites of Special Scientific Interest. On Felton Common, between the village and the airport, is the church of St Katharine and the Noble Army of Martyrs, which was built around 1868, and the remains of a windmill which has been converted into a private house. The small village of Regil also falls within the parish, although it has its own small church dedicated to St James, one pub, a village hall and several farms. Winford village lies on the route of the Monarch's Way long-distance footpath and has one pub, a village post office and several farms in the surrounding area.

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 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.

Dundry is a village and civil parish, situated on Dundry Hill in the northern part of the Mendip Hills, between Bristol and the Chew Valley Lake, in the English county of Somerset. The parish includes the hamlets of Maiden Head and East Dundry. The parish had a 2011 population of 829.The village lies on the route of the Monarch's Way long-distance footpath. It is a popular destination for the people of Bristol as it is known for its panoramic views of the city.

Dundry Hill is immediately south of Bristol, England: it includes farmland, a small number of houses and a church. It stretches east–west for some two miles. Most of the hill is within the district of North Somerset. At the hill's eastern end the southern slopes are within Bath and North East Somerset, and the northern slopes are within the city and county of Bristol, including the highest point in that county.The village of Dundry, with its prominent church, is near the summit. At the eastern end is Maes Knoll, near Norton Malreward, an Iron Age hillfort and the start of Wansdyke. To the South lies the Chew Valley. On the western side of the hill is a spring which becomes the Land Yeo. Dundry Main Road South Quarry is a 0.7 hectare geological Site of Special Scientific Interest near the village of East Dundry, because of the number of fossils in the inferior oolite. 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.

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.

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 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.

Hartcliff Rocks Quarry (grid reference ST534662) is a 1.6 hectare (3.9 acre) Site of Special Scientific Interest (SSSI) near Felton, Somerset notified in 1991. According to the citation, the site "provides exposures of Triassic Dolomitic Conglomerate unconformably overlying Carboniferous Limestone."

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 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.