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Bassingthorpe

Former civil parishes in LincolnshireGrade I listed buildings in LincolnshireOpenDomesdaySouth Kesteven DistrictUse British English from October 2014
Villages in Lincolnshire
St.Thomas' church, Bassingthorpe, Lincs. geograph.org.uk 90736
St.Thomas' church, Bassingthorpe, Lincs. geograph.org.uk 90736

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.

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

Bassingthorpe
Bassingthorpe Road, South Kesteven Bitchfield and Bassingthorpe

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Geographical coordinates (GPS)

Latitude Longitude
N 52.845911 ° E -0.565966 °
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Address

Bassingthorpe Road

Bassingthorpe Road
NG33 4EB South Kesteven, Bitchfield and Bassingthorpe
England, United Kingdom
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St.Thomas' church, Bassingthorpe, Lincs. geograph.org.uk 90736
St.Thomas' church, Bassingthorpe, Lincs. geograph.org.uk 90736
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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.