place

Bitchfield and Bassingthorpe

Civil parishes in LincolnshireSouth Kesteven District
Footpath to Boothby Pagnell geograph.org.uk 212708
Footpath to Boothby Pagnell geograph.org.uk 212708

Bitchfield and Bassingthorpe is a civil parish which includes Boothby Pagnell and Burton Coggles in the South Kesteven district of Lincolnshire, England. According to the 2001 census it had a population of 154 across 59 homes. By the 2011 census there were 157 households, made of 366 people.The civil parish includes the villages of Bitchfield and Bassingthorpe, and the hamlet of Westby. There are no major roads through the parish, though the London-Edinburgh railway line passes through the extreme western edge. The parish is crossed by the B1176 Corby Glen to Grantham road. Several small streams rise in the western half of the parish, and flow eastwards into the West Glen River which flows through the parish from North to South. Bassingthorpe manor is probably the highest spot in the parish, with a spot height of 106m. The terrain slopes down eastward to the shallow valley of the glen, which lies between two 70m contours. Toward the eastern boundary the land rises again to about 90m.Busses on route 4 from Grantham to Stamford pass through the parish.Local democracy takes the form of a parish meeting.

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

Bitchfield and Bassingthorpe
Bassingthorpe Road, South Kesteven Bitchfield and Bassingthorpe

Geographical coordinates (GPS) Address Nearby Places
placeShow on map

Wikipedia: Bitchfield and BassingthorpeContinue reading on Wikipedia

Geographical coordinates (GPS)

Latitude Longitude
N 52.85 ° E -0.55 °
placeShow on map

Address

Bassingthorpe Road

Bassingthorpe Road
NG33 4EB South Kesteven, Bitchfield and Bassingthorpe
England, United Kingdom
mapOpen on Google Maps

Footpath to Boothby Pagnell geograph.org.uk 212708
Footpath to Boothby Pagnell geograph.org.uk 212708
Share experience

Nearby Places

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.