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Beltisloe

Wapentakes of Kesteven
Burton Coggles, Lincolnshire, from the west
Burton Coggles, Lincolnshire, from the west

Beltisloe is a Deanery of the Diocese of Lincoln in England, and a former Wapentake.The Wapentake of Beltisloe was established as an ancient administrative division of the English county of Lincolnshire before the Norman Conquest of 1066. In England a wapentake was the division of a shire for administrative, military and judicial purposes under the common law. The term wapentake is of Scandinavian origin and meant the taking of weapons; it later signified the clash of arms by which the people assembled in a local court expressed assent. Danish influence was strong in those English counties where wapentakes existed.The Wapentake of Beltisloe was bounded on the north by Winnibriggs and Threo Wapentake; on the east by Aveland Wapentake; on the south by Ness Wapentake and Rutland and on the west by Grantham soke and Leicestershire. This wapentake contained a number of now abandoned settlements, and in the 19th century contained the market town of Corby Glen and the villages of Basingthorpe, Bitchfield, Burton Coggles, Castle Bytham, Little Bytham, Careby, Creeton, Edenham, Gunby, Irnham, Lavington, Skillington, Stainby, Swayfield, Swinstead, Witham on the Hill, North Witham and South Witham.

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

Beltisloe
Bourne Road, South Kesteven Corby Glen

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Wikipedia: BeltisloeContinue reading on Wikipedia

Geographical coordinates (GPS)

Latitude Longitude
N 52.81 ° E -0.55 °
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Address

Bourne Road

Bourne Road
NG33 4LD South Kesteven, Corby Glen
England, United Kingdom
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Burton Coggles, Lincolnshire, from the west
Burton Coggles, Lincolnshire, from the west
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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.