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Ingoldsby

Civil parishes in LincolnshireSouth Kesteven DistrictUse British English from December 2013Villages in Lincolnshire
Saint Bartholomew's Church, Ingoldsby geograph.org.uk 87064
Saint Bartholomew's Church, Ingoldsby geograph.org.uk 87064

Ingoldsby is a small village in the South Kesteven district of Lincolnshire, England. It is situated 7 miles (11 km) south-east from the market town of Grantham, 32 miles (51 km) south of the county town of Lincoln, and 33 miles (53 km) east of the City of Nottingham. The village contains approximately 121 households. Ingoldsby is a civil parish and an ecclesiastical parish. The ecclesiastical parish is part of The North Beltisloe Group of parishes in the Deanery of Beltisloe. From 2006 to 2011 the incumbent was Rev Richard Ireson. The parish church is dedicated to St Bartholomew. Ingoldsby is situated midway between Grantham and Bourne. Adjacent villages include Great Humby, Lenton, Bitchfield and Boothby Pagnell. The population of the parish is 254. Close by to the east of the village is the Roman road King Street that ran from Bourne to near Ancaster.Adjacent to the village is the minor hamlet of Scotland, and Scotland House. They are connected by Scotland Lane.Ingoldsby forms the most southerly point of the Ropsley Triangle, which denotes the area between Ropsley, Boothby Pagnell and Ingoldsby.

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

Ingoldsby
Main Street, South Kesteven Ingoldsby

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Latitude Longitude
N 52.858715 ° E -0.50167 °
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Main Street

Main Street
NG33 4ER South Kesteven, Ingoldsby
England, United Kingdom
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Saint Bartholomew's Church, Ingoldsby geograph.org.uk 87064
Saint Bartholomew's Church, Ingoldsby geograph.org.uk 87064
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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.