Burton Coggles

Beltisloe is a Deanery of the Diocese of Lincoln in England, and a former Wapentake.The Wapentake of Beltisloe was established as an ancient administrative division of the English county of Lincolnshire before the Norman Conquest of 1066. In England a wapentake was the division of a shire for administrative, military and judicial purposes under the common law. The term wapentake is of Scandinavian origin and meant the taking of weapons; it later signified the clash of arms by which the people assembled in a local court expressed assent. Danish influence was strong in those English counties where wapentakes existed.The Wapentake of Beltisloe was bounded on the north by Winnibriggs and Threo Wapentake; on the east by Aveland Wapentake; on the south by Ness Wapentake and Rutland and on the west by Grantham soke and Leicestershire. This wapentake contained a number of now abandoned settlements, and in the 19th century contained the market town of Corby Glen and the villages of Basingthorpe, Bitchfield, Burton Coggles, Castle Bytham, Little Bytham, Careby, Creeton, Edenham, Gunby, Irnham, Lavington, Skillington, Stainby, Swayfield, Swinstead, Witham on the Hill, North Witham and South Witham.

Corby Glen railway station was a station on the Great Northern Railway main line serving Corby Glen, Lincolnshire. It was west of the village on the Melton Mowbray road, and was originally named just Corby, but was renamed to avoid confusion with Corby station on the Midland Railway in Northamptonshire. The station closed in 1959.

Westby is a hamlet in the civil parish of Bitchfield and Bassingthorpe, in the South Kesteven district of Lincolnshire, England. It is situated approximately 6 miles (9.7 km) south-east from the town of Grantham. Westby is considered a shrunken medieval village and at the time of Domesday Book of 1086 it consisted of eleven households.

Bitchfield is a village in the civil parish of Bitchfield and Bassingthorpe, in the South Kesteven district of Lincolnshire, England. It consists of two groups of buildings connected by Dark Lane, known as Bitchfield and Lower Bitchfield, collectively called Bitchfield. The village is situated approximately 6 miles (10 km) south-east from Grantham, and on the B1176 road, running east and parallel to the A1. In 1921 the parish had a population of 95. On 1 April 1931 the parish was abolished and merged with Bassingthorpe to form "Bitchfield and Bassingthorpe".Bitchfield is mentioned in the Domesday Book as "Billesfelt". Both Bitchfield and Lower Bitchfield are sometimes described as "shrunken" rather than deserted medieval villages. There are signs that both were more extensive at one time. In Bitchfield there is an earthwork known as Camp Field.The ecclesiastical parish covers just Bitchfield. It is part of the North Beltisloe Group of parishes in the Deanery of Beltisloe, in the Diocese of Lincoln. The parish church, in Lower Bitchfield, is dedicated to St Mary Magdalene. From 2006 to 2011 the incumbent was Rev Richard Ireson. The church is substantially unaltered, with features of both Norman and Perpendicular architecture.

Bitchfield and Bassingthorpe is a civil parish which includes Boothby Pagnell and Burton Coggles in the South Kesteven district of Lincolnshire, England. According to the 2001 census it had a population of 154 across 59 homes. By the 2011 census there were 157 households, made of 366 people.The civil parish includes the villages of Bitchfield and Bassingthorpe, and the hamlet of Westby. There are no major roads through the parish, though the London-Edinburgh railway line passes through the extreme western edge. The parish is crossed by the B1176 Corby Glen to Grantham road. Several small streams rise in the western half of the parish, and flow eastwards into the West Glen River which flows through the parish from North to South. Bassingthorpe manor is probably the highest spot in the parish, with a spot height of 106m. The terrain slopes down eastward to the shallow valley of the glen, which lies between two 70m contours. Toward the eastern boundary the land rises again to about 90m.Busses on route 4 from Grantham to Stamford pass through the parish.Local democracy takes the form of a parish meeting.

Corby Glen is a village and civil parish in the South Kesteven district of Lincolnshire, England. It is approximately 9 miles (14 km) south-east of the market town of Grantham and 8 miles (13 km) north west of Bourne.

Bassingthorpe is a small village in the civil parish of Bitchfield and Bassingthorpe, in the South Kesteven district of Lincolnshire, England. It is 5 miles (8 km) south from Grantham, and on a C class road between the B6403 to the west and the B1176 to the east. In 1921 the parish had a population of 78. On 1 April 1931 the parish was abolished and merged with Bitchfield to form "Bitchfield and Bassingthorpe".The village contains 4 houses and a Grade I listed church dedicated to St Thomas. The ecclesiastical parish is part of The North Beltisloe Group of parishes, of the Deanery of Beltisloe in the Diocese of Lincoln. From 2006 to 2011 the incumbent was Rev Richard Ireson.

Swayfield 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 316. It is situated just over 3 miles (5 km) east from the A1 road, 9 miles (14 km) south-east from Grantham and 10 miles (16 km) north from Stamford. It has approximately 138 houses.

The Northampton Sand Formation, sometimes called the Northamptonshire Sand, is a Middle Jurassic geological formation which is placed within the Inferior Oolite Group. It was formerly worked extensively in Northamptonshire for its ironstone. The Northampton Sand Formation constitutes the lowest part of the Inferior Oolite Group and lies on the upper Lias clay. It attains a maximum thickness of up to 21 metres (69 ft) to the north and west of Northampton where it lies in a subterranean basin. In the south, it fades out around Towcester. Northward from the edge of the basin in the upper Lias, under Northampton, it lies progressively lower beneath the Jurassic Lincolnshire limestones. A little to the north of Corby Glen (grid reference TF0027) it is at about 50 metres (160 ft) from the surface. It fades out under north Lincolnshire as the strata rise towards the Market Weighton Axis. The formation to dates to the Aalenian, and predominantly consists of sandy ironstone, which when freshly exposed is greenish-grey in colour, which weathers to limonitic brown sandstone. It formed in an extensive, shallow sea on the northwestern margin of the London-Brabant Massif. Dinosaur remains are among the fossils that have been recovered from the formation, although none have yet been referred to a specific genus. A species of horseshoe crab, Mesolimulus woodwardi has been described from the formation.The formation is a signficiant emitter of radon gas.

The Church of St John the Evangelist is a Grade I listed Church of England parish church dedicated to John the Evangelist, in Corby Glen, Lincolnshire, England. The church is 9 miles (14 km) south-east of Grantham, and in the South Kesteven Lincolnshire Vales. It is noted in particular for its 14th- and 15th-century medieval wall paintings. St John's is in the ecclesiastical parish of Corby Glen, and is part of the Corby Glen Group of Parishes in the Deanery of Beltisloe, and the Diocese of Lincoln. Other churches within the group are St Andrew's at Irnham, St Nicholas' at Swayfield, St Thomas a Becket at Bassingthorpe, St Mary Magdalene at Bitchfield and St Thomas of Canterbury at Burton Coggles.

Charles Read Academy is a co-educational secondary school located in Corby Glen, Lincolnshire, England. It serves the villages between Stamford, Bourne and Grantham. The current school was built as a comprehensive in 1963, and in 1999 it was renamed the Charles Read High School to perpetuate the tradition of the former grammar school founded in 1669 by the bequest of Charles Read (1604–1669), who became a wealthy shipper in Hull. Read also founded Read School at Drax in Yorkshire and a grammar school at Tuxford in Notts. Reads Grammar School in Corby Glen closed in 1909.The original grammar school building is now the Willoughby Memorial Library and Art Gallery. The building was restored in 1965 by the Willoughby Memorial Trust which was founded by James Heathcote-Drummond-Willoughby, 3rd Earl of Ancaster in memory of his son Timothy, Lord Willoughby de Eresby, who died in 1963. Charles Read High School converted to an academy in January 2011. In January 2013 the West Grantham Academies Trust announced the Academy would close by September 2014 but subsequently the David Ross Education Trust took responsibility for maintaining the school.

Stoke Bank is an inclined stretch of the East Coast Main Line (ECML) between Peterborough and Grantham. It is named after the village of Stoke Rochford, close to Stoke Summit, which at 345 feet (105 m) above sea level is the highest point of the ECML between London King's Cross and Berwick-upon-Tweed. It is not however, the highest point of the entire ECML, which is Grantshouse Summit between Berwick and Edinburgh at 400 feet (120 m).The climb up the bank begins roughly 15 miles (24 km) north of Peterborough, which is close to sea level, and ascends to Stoke Summit over a distance of approximately 10 miles (16 km) with gradients of up to 1 in 178. Shortly after the summit, the line runs through the 880 yards (800 m) Stoke Tunnel. It then descends for around 5 miles at 1 in 200 before reaching Grantham station, and then continues on a more gradual descent for around 15 miles, until reaching Newark North Gate, which is also near sea level.