|
East Farndon
East Farndon is a small linear village and civil parishes in England, civil parish about one mile south of Market Harborough in West Northamptonshire, England. The village is close to the border with Leicestershire, and has a Leicestershire post code and telephone dialling code. At the time of the United Kingdom Census 2001, 2001 census, the parish's population was 258 people, increasing to 307 at the 2011 census. The villages name means 'Ferny hill'. The village is mentioned in the Domesday Book of 1086. In a field on the west side of the parish is the Judith Stone. This is a glacial erratic, brought from probably hundreds of miles away during an ice age. It is thought to take its name from the Judith of Lens, Countess Judith, niece of William I of England, William the Conqueror. She is recorded in the Domesday Book as holding land in the parish, so perhaps the stone marked a Boundary marker, boundary of some kind. The church stands at the top of a hill and the village street ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
West Northamptonshire
West Northamptonshire is a unitary authority area covering part of the ceremonial county of Northamptonshire, England, created in 2021. By far the largest settlement in West Northamptonshire is the county town of Northampton. Its other significant towns are Daventry, Brackley and Towcester; the rest of the area is predominantly agricultural villages though it has many lakes and small woodlands and is passed through by the West Coast Main Line and the M1 and M40 motorways, thus hosting a relatively high number of hospitality attractions as well as distribution centres as these are key English transport routes. Close to these is the leisure-use Grand Union Canal. The district has remains of a Roman town Bannaventa, with relics and finds in the main town museums, and its most notable landscape and the mansion is Althorp. History West Northamptonshire was formed on 1 April 2021 through the merger of the three non-metropolitan districts of Daventry, Northampton, and South North ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacial Erratic
A glacial erratic is glacially deposited rock differing from the type of rock native to the area in which it rests. Erratics, which take their name from the Latin word ' ("to wander"), are carried by glacial ice, often over distances of hundreds of kilometres. Erratics can range in size from pebbles to large boulders such as Big Rock () in Alberta. Geologists identify erratics by studying the rocks surrounding the position of the erratic and the composition of the erratic itself. Erratics are significant because: *They can be transported by glaciers, and they are thereby one of a series of indicators which mark the path of prehistoric glacier movement. Their lithographic origin can be traced to the parent bedrock, allowing for confirmation of the ice flow route. *They can be transported by ice rafting. This allows quantification of the extent of glacial flooding resulting from ice dam failure which release the waters stored in proglacial lakes such as Lake Missoula. Erratics ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
