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Charles Read Academy

Academies in LincolnshireEast Midlands school stubsLincolnshire building and structure stubsSecondary schools in LincolnshireUse British English from February 2023
The Charles Read Academy (geograph 3713734)
The Charles Read Academy (geograph 3713734)

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.

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

Charles Read Academy
Bourne Road, South Kesteven Corby Glen

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N 52.81054 ° E -0.51636 °
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Charles Read Academy

Bourne Road
NG33 4NT South Kesteven, Corby Glen
England, United Kingdom
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Phone number
The David Ross Education Trust

call+441476550333

Website
charlesreadacademy.co.uk

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The Charles Read Academy (geograph 3713734)
The Charles Read Academy (geograph 3713734)
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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.