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St John the Evangelist's Church, Corby Glen

14th-century church buildings in EnglandChurch of England church buildings in LincolnshireEnglish Gothic architecture in LincolnshireGrade I listed churches in LincolnshireOpenDomesday
South Kesteven DistrictUse British English from July 2013
Corby Glen St John's from the south east
Corby Glen St John's from the south east

The Church of St John the Evangelist is a Grade I listed Church of England parish church dedicated to John the Evangelist, in Corby Glen, Lincolnshire, England. The church is 9 miles (14 km) south-east of Grantham, and in the South Kesteven Lincolnshire Vales. It is noted in particular for its 14th- and 15th-century medieval wall paintings. St John's is in the ecclesiastical parish of Corby Glen, and is part of the Corby Glen Group of Parishes in the Deanery of Beltisloe, and the Diocese of Lincoln. Other churches within the group are St Andrew's at Irnham, St Nicholas' at Swayfield, St Thomas a Becket at Bassingthorpe, St Mary Magdalene at Bitchfield and St Thomas of Canterbury at Burton Coggles.

Excerpt from the Wikipedia article St John the Evangelist's Church, Corby Glen (License: CC BY-SA 3.0, Authors, Images).

St John the Evangelist's Church, Corby Glen
Church Street, South Kesteven Corby Glen

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Wikipedia: St John the Evangelist's Church, Corby GlenContinue reading on Wikipedia

Geographical coordinates (GPS)

Latitude Longitude
N 52.8132 ° E -0.515708 °
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Church Street
NG33 4NJ South Kesteven, Corby Glen
England, United Kingdom
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Corby Glen St John's from the south east
Corby Glen St John's from the south east
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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.