Monkton Combe School

Monkton Combe is a village and civil parish in north Somerset, England, 3 miles (4.8 km) south of Bath. The parish, which includes the hamlet of Tucking Mill, had a population of 554 in 2013. It was formerly known as Combe, owing to its geography, while it was also known as Monckton Combe and Combe Monckton until last century.

Monkton Combe Halt railway station was a railway station in Monkton Combe, Somerset, UK. It was built by the Great Western Railway in 1910, on the Camerton branch of the Bristol and North Somerset Railway line.

St Michael's Church is the Church of England parish church of Monkton Combe, Somerset, England. It was also the parish church of Combe Down until the 1850s when the communities separated. It is a Grade II listed building.

Ralph Allen School in Combe Down, Bath, England, is a co-educational, comprehensive secondary school with academy status. Located on the south-eastern edge of Bath, the school educates 11 to 18-year-olds from Bath and the surrounding area.

Tucking Mill is a small hamlet within the parish of Monkton Combe, Somerset, England. It lies on Midford Brook and was a key point on the now disused Somerset Coal Canal. It is at the southern end of the Two Tunnels Greenway which follows the disused railway trackbed of the Somerset and Dorset Joint Railway from East Twerton through the Bath suburb of Oldfield Park to the Devonshire Tunnel, emerging into Lyncombe Vale before entering the Combe Down Tunnel, and then coming out to cross Tucking Mill Viaduct into Midford.There is also a small reservoir, which is now a fishery for the disabled.

Midford Valley Woods (grid reference ST769611) is a 60-acre (24.6-hectare) biological Site of Special Scientific Interest between Midford and Limpley Stoke in Wiltshire, England, notified in 1975.

Combe Down Tunnel is on the now-closed Somerset and Dorset Joint Railway main line, between Midford and Bath Green Park railway station, below high ground and the southern suburbs of Bath, England, emerging below the southern slopes of Combe Down village. Opened in 1874, this 1,829-yard (1,672 m) long disused railway tunnel was once the UK's longest without intermediate ventilation. The tunnel now forms part of the £1.8 million Two Tunnels Greenway walking and cycling path opened on 6 April 2013 and is the longest cycling tunnel in Britain. Its custodian is Wessex Water.

Limpley Stoke is a village and civil parish in Wiltshire, England. It lies in the Avon valley between Bath and Freshford, and is both above and below the A36 road. The parish is surrounded to the north, west and south by the Bath and North East Somerset district and includes the outskirts of the Somerset villages of Freshford and Midford. The Avon forms the eastern boundary of the parish, and its tributary the Midford Brook is the boundary in the north and west.

Limpley Stoke railway station is a former railway station in Limpley Stoke, Wiltshire, England, UK. The station was originally started by the Wilts, Somerset and Weymouth Railway, which was bought by the Great Western Railway before service started. The station served as a loading point for limestone from nearby quarries until 1960. Two camping coaches were positioned here by the Western Region from 1956 to 1957. The station closed in 1966, and the building is now in private hands. The line remains open, and has regular passenger service.

Combe Down is a village on the outskirts of Bath, England in the Bath and North East Somerset unitary authority within the ceremonial county of Somerset. Combe Down village consists predominantly of 18th and 19th century Bath stone-built villas, terraces and workers' cottages; the post World War II Foxhill estate of former and present council housing; a range of Georgian, Victorian and 20th century properties along both sides of North Road and Bradford Road and the 21st century Mulberry Park development on the site of the former Ministry of Defence offices.

Dundas Aqueduct (grid reference ST785625) carries the Kennet and Avon Canal over the River Avon (the Somerset / Wiltshire border) and the Wessex Main Line railway from Bath to Westbury. The aqueduct is near Monkton Combe, Somerset, and is about 2+1⁄2 miles (4 km) southeast of the city of Bath. It was designed by John Rennie and chief engineer John Thomas between 1797 and 1801, and completed in 1805. James McIlquham was appointed contractor. It is named after Charles Dundas, the first chairman of the Kennet and Avon Canal Company. The aqueduct is 150 yards (137.2 m) long with three arches built of Bath Stone, with Doric pilasters, and balustrades at each end. The central semi-circular arch spans 64 feet (19.5 m); the two oval side arches span 20 feet (6.1 m).The canal crosses back across the Avon and the railway on another aqueduct at Avoncliff. This diversion onto the right bank of the Avon avoids the steep sides of the river valley at Limpley Stoke, and the need to cross the Midford Brook and River Frome. It is a Grade I listed building, and was the first canal structure to be designated as a Scheduled Ancient Monument in 1951. Over many years, leaks had developed and the aqueduct was closed in 1954. For a while in the 1960s and 1970s, the canal was dry and it was possible to walk along the bed on each side of the river, as well as through the aqueduct itself. The aqueduct was relined with polythene and concrete and restored, reopening in 1984. Care was taken not to disturb a colony of bats living under the aqueduct. The aqueduct is also the junction between the Kennet and Avon Canal and the largely derelict Somerset Coal Canal. The short stretch of the Somerset Coal Canal still in water forms Brassknocker Basin, used for boat moorings, cycle hire and a cafe, and is next to Dundas Wharf where the small tollhouse, warehouse and crane still stand. The stretch of river below and above the aqueduct is used by Monkton Combe School Boat Club (Monkton Bluefriars) up to six days a week, since at least the 1960s. At the opposite (Wiltshire) end of the aqueduct a wharf was constructed serving the Conkwell stone quarries.Between 2002 and 2004 further restoration was undertaken, which included replacing engineering bricks used by GWR with Bath Stone to match the original work. In 2015, the railway below the aqueduct was lowered to allow the route to be used as a diversionary route for freight trains in the future. Network Rail published a time-lapse video of the work.

Midford Brook is a small river in Somerset, England. It is formed by the convergence of the Wellow Brook and Cam Brook at Midford. It passes Tucking Mill and joins the River Avon close to the Dundas Aqueduct and the remains of the Somerset Coal Canal. For its entire length it defines the boundary between Bath & North East Somerset and Wiltshire.Although the Midford Brook is named on Ordnance Survey maps, the Environment Agency does not recognise it, instead identifying the Wellow Brook as continuing to the Avon.The Midford Brook has a catchment area of 147.4 km2 which is largely over impermeable Lias. The deep steep-sided valley means that it responds rapidly to rainfall.