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Bitchfield

Former civil parishes in LincolnshireSouth Kesteven DistrictUse British English from October 2014Villages in Lincolnshire
St.Mary Magdalene's church, Bitchfield, Lincs. geograph.org.uk 212701
St.Mary Magdalene's church, Bitchfield, Lincs. geograph.org.uk 212701

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.

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

Bitchfield
Corby Road, South Kesteven Bitchfield and Bassingthorpe

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Geographical coordinates (GPS)

Latitude Longitude
N 52.84625 ° E -0.533655 °
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Corby Road

Corby Road
NG33 4DU South Kesteven, Bitchfield and Bassingthorpe
England, United Kingdom
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St.Mary Magdalene's church, Bitchfield, Lincs. geograph.org.uk 212701
St.Mary Magdalene's church, Bitchfield, Lincs. geograph.org.uk 212701
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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.