Uffington and Barnack railway station

Pilsgate is a hamlet and former civil parish, now in the parish of Barnack, in the Peterborough district, in the ceremonial county of Cambridgeshire, England. Pilsgate is close to the county boundary and 3 miles (5 km) south-east of Stamford, Lincolnshire. In 1881 the parish had a population of 125.

Uffington is a village and civil parish in the South Kesteven district of Lincolnshire, England. The population of the civil parish at the 2011 census was 686. It is in the valley of the River Welland, between Stamford and The Deepings.

Barnack is a village and civil parish in the Peterborough unitary authority of the ceremonial county of Cambridgeshire, England and the historic county of Northamptonshire. Barnack is in the north-west of the unitary authority, 3.5 miles (5.6 km) south-east of Stamford, Lincolnshire. The parish includes the hamlet of Pilsgate about 1 mile (1.6 km) northwest of Barnack. Both Barnack and Pilsgate are on the B1443 road. The 2011 Census recorded a parish population of 931.Barnack is historically part of the Soke of Peterborough, which was associated with Northamptonshire but had its own County Council from 1888 until 1965. From 1894 until 1965 there was a Barnack Rural District that was a subdivision of the Soke, and which formed part of Huntingdon and Peterborough until 1974.Barnack is notable for its former limestone industry, its Anglo-Saxon parish church and an unusual early Bronze Age burial. Hills and Holes, an area of Roman and later quarrying, is now a nature reserve.

The Church of St John the Baptist, Barnack is a Church of England parish church in the village of Barnack, now in the City of Peterborough unitary authority area of the ceremonial county of Cambridgeshire, England. Barnack was part of the Soke of Peterborough, an historic area that was traditionally part of Northamptonshire. Barnack is 3.5 miles (6 km) south-east of Stamford in Lincolnshire. The church is a Grade I listed building.The church, dedicated to John the Baptist, is noted in particular for its Anglo-Saxon tower to which was added a spire of circa 1200, possibly one of the earliest spires in England.In the north aisle is a large Romanesque sculpture of a seated Christ in Majesty that was discovered under the floor in 1931. Estimates of the date of the Christ vary widely, from the latter part of the 10th century to circa 1200; the Corpus of Romanesque Sculpture in Britain and Ireland settles on the late 12th century.Simon Jenkins gives the church four stars in his England's Thousand Best Churches (1999) and highlights as features the tower, the stiff-leaf font and the Christ in Majesty. The height of the surviving Saxon work in the tower is 55 feet (17 metres), topped by an octagon and spire of 59 feet high (18 metres), giving a total height to the base of the weathervane of 114 feet (35 metres).

Barnack Hills & Holes is a 23.3-hectare (58-acre) biological Site of Special Scientific Interest in Barnack in Cambridgeshire. It is also a national nature reserve. It is a Nature Conservation Review site, Grade I. In 2002 it was designated as a Special Area of Conservation, to protect the orchid-rich grassland as part of the Natura 2000 network of sites throughout the European Union.Arising from the rubble of a medieval quarry, the Hills and Holes is one of Britain’s most important wildlife sites. Covering an area of just 50 acres (22 ha), the grassy slopes are home to a profusion of wild flowers. This type of meadowland is now all too rare; half of the surviving limestone grassland in Cambridgeshire is found here. In 2002 it was designated as a Special Area of Conservation, to protect the orchid-rich grassland as part of the Natura 2000 network of sites throughout the European Union.The hummocky landscape was created by quarrying for limestone. Barnack stone, was a valuable building stone first exploited by the Romans over 1,500 years ago. Stone from Barnack was used to build Peterborough and Ely Cathedrals. By the year 1500 however, all the useful stone had been removed and the bare heaps of limestone rubble gradually became covered by the rich carpet of wild flowers that can be seen today. The limestone was originally formed in Jurassic times. It is made from the remains of billions of tiny sea-creatures which lived in a warm shallow sea that covered the area 150 million years ago.Barnack’s rich flora supports a wide variety of wildlife, especially insects, and a number of nationally scarce species are found. Limestone grasslands are traditionally grazed with sheep and at Barnack, grazing is carried out in autumn by up to 300 sheep. These remove the summer growth and build-up of leaves, stalks and grass tussocks that would otherwise die back to form a dead layer, or litter, on the ground. Without grazing, the build-up of coarse grasses and litter would rapidly choke the rarer lime-loving plants.

Barnack railway station was a station in the Soke of Peterborough (now Cambridgeshire) serving the village of Barnack. Despite being located adjacent to the village, the more remote Uffington & Barnack station on the Midland Railway Leicester to Peterborough line was more convenient for many journeys. Barnack station was opened by the Stamford and Essendine Railway (S&ER) on 9 August 1867; it was on the S&ER's branch from Stamford to Wansford. The S&ER was leased to the Great Northern Railway at the end of 1892. The line never really recovered from the 1926 general strike, and the station closed with the line on 1 July 1929. In 2014 the building survives as a private house.

Walcot Hall is a Grade I listed Carolean country house in the hamlet of Southorpe. It lies 2 km (1 mile) south of the village of Barnack, Cambridgeshire, UK. The house is now within the boundary of the Peterborough unitary authority area of the ceremonial county of Cambridgeshire but it was part of the Soke of Peterborough, an historic area that was traditionally associated with Northamptonshire. It is constructed of limestone ashlar in 2 storeys with attic with a rectangular floor plan of 9 by 5 bays and a Collyweston stone roof. It stands in some 120 acres of wooded parkland as part of a 1400-acre agricultural estate.

Uffington was a rural district in Lincolnshire, Parts of Kesteven from 1894 to 1931. It was created in 1894 from that part of the Stamford rural sanitary district which was in Kesteven (the rest forming part of either Ketton Rural District in Rutland, Easton on the Hill Rural District in Northamptonshire, or Barnack Rural District in the Soke of Peterborough). It covered the following parishes: Barholm Braceborough Greatford Stowe Tallington Uffington West Deeping WilsthorpeIt was abolished by a County Review Order in 1931, and went to form part of the South Kesteven Rural District.

Ufford Bridge railway station was a station serving the villages of Ufford and Southorpe in the Soke of Peterborough (now part of Cambridgeshire). The station was situated where the road from Ufford crosses the railway, at the point where it meets the Barnack to Southorpe road. The platform was under and to the north of the bridge and the goods siding to the south. A waiting room was built utilising the road bridge as its roof. The train guard combined the duties of station master, porter, booking clerk and ticket collector at Ufford Bridge. The station was on the Stamford and Essendine Railway line from Stamford to Wansford line which never really recovered from the 1926 general strike, and the station closed with the line on 1 July 1929.

Bainton Gate railway station was a short lived railway "station" in the Soke of Peterborough (now in Cambridgeshire) on the Syston and Peterborough Railway serving the village of Bainton. It was located at the level crossing on the Bainton to Tallington road. The crossing keeper's cottage survives and is now a private house. According to The Syston and Peterborough website, this cottage doubled as the station building. The station closed on 1 August 1856.

Southorpe Roughs is a 9.8-hectare (24-acre) Site of Special Scientific Interest west of Southorpe in Cambridgeshire.This is a disused quarry which has grassland on Jurassic limestone. The main grasses are tor-grass and sheep's fescue, and there are the nationally rare plants spotted cat's ear and pasque flower.The site is private land with no public access.

The River Gwash, occasionally Guash, a tributary of the River Welland, flows through the English counties of Leicestershire, Rutland and Lincolnshire. It rises just outside the village of Knossington in Leicestershire, near the western edge of Rutland. It is about 39 kilometres (24 mi) long.