place

Grantham and Stamford (UK Parliament constituency)

Constituencies of the Parliament of the United Kingdom established in 1997Parliamentary constituencies in LincolnshirePolitics of GranthamSouth Kesteven District
GranthamStamford2007Constituency
GranthamStamford2007Constituency

Grantham and Stamford is a constituency in Lincolnshire represented in the House of Commons of the UK Parliament since 2019 by Gareth Davies, a Conservative.Under the 2023 Periodic Review of Westminster constituencies, the constituency will be subject to major boundary changes, with Stamford being included in the re-established Rutland and Stamford constituency. The seat will be renamed Grantham and Bourne, to be first contested at the next general election.

Excerpt from the Wikipedia article Grantham and Stamford (UK Parliament constituency) (License: CC BY-SA 3.0, Authors, Images).

Grantham and Stamford (UK Parliament constituency)
B1176, South Kesteven Swinstead

Geographical coordinates (GPS) Address Nearby Places
placeShow on map

Wikipedia: Grantham and Stamford (UK Parliament constituency)Continue reading on Wikipedia

Geographical coordinates (GPS)

Latitude Longitude
N 52.8 ° E -0.5 °
placeShow on map

Address

B1176
NG33 4PB South Kesteven, Swinstead
England, United Kingdom
mapOpen on Google Maps

GranthamStamford2007Constituency
GranthamStamford2007Constituency
Share experience

Nearby Places

Counthorpe
Counthorpe

Counthorpe is a hamlet in the civil parish of Counthorpe and Creeton in the South Kesteven district of Lincolnshire, England. It adjoins the hamlet of Creeton and lies 5 miles (8 km) south-west from Bourne and 3 miles (5 km) south from Corby Glen, and on the River Glen. In the Domesday account Counthorpe is written as "Cudetorp". Before the Conquest lordship was held by Earl Morcar; after, Drogo de la Beuvrière became Tenant-in-chief.Counthorpe shares the Grade I listed Anglican parish church at Creeton, dedicated to St Peter. The church is of late Decorated style. A restoration of 1851 discovered the arches and piers of a former Norman aisle. The church holds a chained bible from 1611. Two examples of Saxon crosses stand in the churchyard, with 20 stone coffins considered to mark the interment of Cistercian monks of Vallis Dei abbey in the neighbouring parish of Edenham.Counthorpe was formerly a hamlet of Castle Bytham and had, up to the 16th century, its own parochial chapel, but was annexed to Creeton in 1860.Counthorpe is recorded in the 1872 White's Directory as a small village in the parish of Castle Bytham, but which, for ecclesiastical purposes, became on 30 June 1860 united with Creeton. The village was 2 miles (3 km) from Little Bytham railway station. At this time Counthope was a township of 78 people in about 130 acres (0.5 km2) of land divided between three farms; a farmer of one of these, at Counthorpe Lodge, was also a grazier.

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.