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South Kesteven

Local government districts of the East MidlandsNon-metropolitan districts of LincolnshireSouth Kesteven DistrictUse British English from December 2012
Grantham Town (cropped)
Grantham Town (cropped)

South Kesteven is a local government district in Lincolnshire, England, forming part of the traditional Kesteven division of the county. Its council is based in Grantham. The district also includes the towns of Bourne, Market Deeping and Stamford, along with numerous villages and surrounding rural areas. The neighbouring districts are North Kesteven, South Holland, Peterborough, North Northamptonshire, Rutland, Melton and Newark and Sherwood.

Excerpt from the Wikipedia article South Kesteven (License: CC BY-SA 3.0, Authors, Images).

Geographical coordinates (GPS)

Latitude Longitude
N 52.8 ° E -0.5 °
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08902
New Jersey, Vereinigte Staaten von Amerika
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Grantham Town (cropped)
Grantham Town (cropped)
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Counthorpe
Counthorpe

Counthorpe is a hamlet in the civil parish of Counthorpe and Creeton in the South Kesteven district of Lincolnshire, England. It adjoins the hamlet of Creeton and lies 5 miles (8 km) south-west from Bourne and 3 miles (5 km) south from Corby Glen, and on the River Glen. In the Domesday account Counthorpe is written as "Cudetorp". Before the Conquest lordship was held by Earl Morcar; after, Drogo de la Beuvrière became Tenant-in-chief.Counthorpe shares the Grade I listed Anglican parish church at Creeton, dedicated to St Peter. The church is of late Decorated style. A restoration of 1851 discovered the arches and piers of a former Norman aisle. The church holds a chained bible from 1611. Two examples of Saxon crosses stand in the churchyard, with 20 stone coffins considered to mark the interment of Cistercian monks of Vallis Dei abbey in the neighbouring parish of Edenham.Counthorpe was formerly a hamlet of Castle Bytham and had, up to the 16th century, its own parochial chapel, but was annexed to Creeton in 1860.Counthorpe is recorded in the 1872 White's Directory as a small village in the parish of Castle Bytham, but which, for ecclesiastical purposes, became on 30 June 1860 united with Creeton. The village was 2 miles (3 km) from Little Bytham railway station. At this time Counthope was a township of 78 people in about 130 acres (0.5 km2) of land divided between three farms; a farmer of one of these, at Counthorpe Lodge, was also a grazier.

Northampton Sand Formation
Northampton Sand Formation

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.