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Irnham

Civil parishes in LincolnshireSouth Kesteven DistrictUse British English from February 2014Villages in Lincolnshire
Griffin Inn Irnham by Tim Heaton
Griffin Inn Irnham by Tim Heaton

Irnham is a village and civil parish in South Kesteven, Lincolnshire, England. It is situated approximately 10 miles (16 km) south-east from Grantham. To the north is Ingoldsby and to the south-west, Corby Glen. The village is on a high limestone ridge that forms part of the Kesteven Uplands. The civil parish of Irnham includes the hamlets of Bulby and Hawthorpe. The similar extent ecclesiastical parish is Irnham, part of the Beltisloe rural deanery in the Diocese of Lincoln, and part of a Group which includes Corby Glen and Swayfield, sharing a single priest. The parish church is dedicated to St Andrew.

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

Irnham
South Kesteven Irnham

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Wikipedia: IrnhamContinue reading on Wikipedia

Geographical coordinates (GPS)

Latitude Longitude
N 52.829 ° E -0.481 °
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Address


NG33 4JG South Kesteven, Irnham
England, United Kingdom
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Griffin Inn Irnham by Tim Heaton
Griffin Inn Irnham by Tim Heaton
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Hawthorpe, Lincolnshire
Hawthorpe, Lincolnshire

Hawthorpe is a hamlet in the South Kesteven district of Lincolnshire, England, and the civil parish of Irnham, Bulby and Hawthorpe. It is west from the A15, east from the A1, and 5 miles (8.0 km) north-west from the town of Bourne. Hawthorpe is mentioned in the Domesday Book as "Awartorp", in the Beltisloe Hundred of Kesteven. It comprised 2 households, 2 villagers and 4 freemen, with 2.9 ploughlands, a meadow of 8 acres (0.032 km2) and woodland of 320 acres (1.3 km2). In 1066 the Lord was Healfdene; after 1086 Lordship was given to Alfred of Lincoln.In the 1872 White's Directory the two hamlets of Bulby and Hawthorpe were grouped as Bulby-cum-Hawthorpe forming the eastern side of Irnham parish, being a joint township with a population of 180 in 1,767 acres (7.2 km2) "of fertile land". About 1,000 acres (4.0 km2) of Bulby-cum-Hawthorpe land was purchased by Rev. William Watson Smith in about 1840, who built on it the Elizabethan-style Bulby House and grounds. By 1872, Bulby House and 1,100 acres (4.5 km2) of township land was owned by Gilbert Heathcote-Drummond-Willoughby, 1st Earl of Ancaster (Lord Aveland), who was lord of the manor. A moated area evident at the time was said to be the site of Bulby Hall which is "supposed to have been burnt down in the Barons' wars".In the 1885 Kelly's Directory Hawthorpe is written as having an 1881 population of 70, and as a joint township with the hamlet of Bulby for the support of the poor. Hawthorpe belonged principally to Lord Aveland, who lived at Bulby House.Listed buildings in the hamlet centre on Hawthorpe Farm, including a 17th-century farmhouse, 19th-century cottages, and 17th- to 19th-century barns and stables, all Grade II.

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.