Winford

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.

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.

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."

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.

Barrow Gurney is a village and civil parish in Somerset, England, situated in the unitary authority of North Somerset on the B3130, midway between the A38 and A370 near the Long Ashton bypass and Bristol Airport, 5 miles (8.0 km) south west of Bristol city centre. The civil parish includes Barrow Common, and has a population of 349.It is close to Barrow Gurney Reservoirs, which supply drinking water for Bristol, and feed the Land Yeo which runs alongside the B3130 through the village. It was also the site of Barrow Hospital.

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.

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.

Barrow Gurney Reservoirs (grid reference ST5468) (also known as Barrow Gurney Tanks or Barrow Tanks) are three artificial reservoirs for drinking water near the village of Barrow Gurney, which lies southwest of Bristol, England. They are known by their numbers rather than names. They are fed by several springs including one which becomes the Land Yeo. Some of the outfall is also used to feed the river which flows to the Bristol Channel. There are three reservoirs in total, one (Tank number three, 60 acres (24 ha) to the north of the A38 and two (Tank number one, 25 acres (10 ha) and number two, 40 acres (16 ha) to the south. The reservoirs are operated by Bristol Water. The first opened in 1852 to store the water from the newly finished "Line of Works", but within two years it developed a leak and had to be drained for repair, causing serious disruption to Bristol's water supply. Over the following decades, work was undertaken to improve the water quality. First with sand filters and in 1935 with chlorinationDuring 1962 maximum output was increased from 26 million imperial gallons (120,000 m3) to 31 million imperial gallons (140,000 m3) a day by lowering the outlet of the filtered tank and duplicating inlets to the seven filters which received microstrained water. The stony banks on all the tanks provide a habitat for sedges. Fishing (under permit) is generally for rainbow (Oncorhynchus mykiss, formerly Salmo iridia) and Brown trout (Salmo trutta morpha fario and S. trutta morpha lacustris).

Barrow Gurney Nunnery (also called Minchin Barrow) was established around 1200 in Barrow Gurney Somerset, England. The Benedictine convent was founded by one of the Fitz-Hardinges (or Fitzhardinge), and in 1212, was left 10 marks in the will of Hugh de Wells. The nunnery also received a pension on the church of Twerton by the time of the Taxatio in 1291. Several other donations of money and land had been received by the Valor of 1535 when the property was assessed as worth £29 6s. 8½d. on which there were charges of £5 12s. 4¾d., leaving a clear value of £23 14s. 3¾d.The nunnery was still poor and by 1398 had transferred from the Diocese of Wells to the Diocese of Llandaff.At the dissolution of the monasteries in 1536 its value was £31. The area and buildings were granted by Henry VIII to John Drew, of Bristol, who converted it into a private mansion, renamed Barrow Court.

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.

Barrow Hospital (sometimes referred to as Barrow Gurney Hospital, or Barrow Gurney Psychiatric Institution) was a psychiatric hospital in Barrow Gurney, Somerset, United Kingdom.

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.