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Careby Aunby And Holywell
Careby Aunby and Holywell is a civil parish in the district of South Kesteven, south-west Lincolnshire, in England. It stretches from the county border with Rutland in the west to the River West Glen in the east. The B1176 road from Corby Glen passes through Careby and on past Aunby toward Stamford. The main London to Scotland railway line passes through the parish, the line upon which ''Mallard'' took the speed record for the LNER. The total population in the 2001 census was 146, falling marginally to 143 at the 2011 census. The population in 1801 was 65, and had risen to 133 by 1911 The centre of the parish is near Places in the parish Settlements *Careby *Aunby *Holywell Other Locations *Castle Dyke Earthen banks forming the remains of a small moated medieval structure in the woods between Aunby and Holywell. *Lincolnshire Gate At the western boundary with Rutland there is a small but important Nature Reserve called Robert's Field at Lincolnshire Gate. *Stant ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
England
England is a country that is part of the United Kingdom. It shares land borders with Wales to its west and Scotland to its north. The Irish Sea lies northwest and the Celtic Sea to the southwest. It is separated from continental Europe by the North Sea to the east and the English Channel to the south. The country covers five-eighths of the island of Great Britain, which lies in the North Atlantic, and includes over 100 smaller islands, such as the Isles of Scilly and the Isle of Wight. The area now called England was first inhabited by modern humans during the Upper Paleolithic period, but takes its name from the Angles, a Germanic tribe deriving its name from the Anglia peninsula, who settled during the 5th and 6th centuries. England became a unified state in the 10th century and has had a significant cultural and legal impact on the wider world since the Age of Discovery, which began during the 15th century. The English language, the Anglican Church, and Engli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lincolnshire Gate
Lincolnshire Gate is the name given to a corner in the road between Holywell, Lincolnshire and Pickworth, Rutland to the south-west of Castle Bytham, in Lincolnshire, England. It is situated approximately north from Stamford. It describes a point where this small country road crosses the county border between Lincolnshire and Rutland, to pass between Newell Wood and Howitts Gorse. On either side are the remains of small quarries, worked from the Middle Ages till the early 20th century for building and road stone for nearby use. Robert's Field, a calcareous grassland nature reserve and Site of Special Scientific Interest A Site of Special Scientific Interest (SSSI) in Great Britain or an Area of Special Scientific Interest (ASSI) in the Isle of Man and Northern Ireland is a conservation designation denoting a protected area in the United Kingdom and Isle of ... (SSSI), is to the north. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South Kesteven District Council
South is one of the cardinal directions or Points of the compass, compass points. The direction is the opposite of north and is perpendicular to both east and west. Etymology The word ''south'' comes from Old English ''sūþ'', from earlier Proto-Germanic language, Proto-Germanic ''*sunþaz'' ("south"), possibly related to the same Proto-Indo-European language, Proto-Indo-European root that the word ''sun'' derived from. Some languages describe south in the same way, from the fact that it is the direction of the sun at noon (in the Northern Hemisphere), like Latin meridies 'noon, south' (from medius 'middle' + dies 'day', cf English meridional), while others describe south as the right-hand side of the rising sun, like Biblical Hebrew תֵּימָן teiman 'south' from יָמִין yamin 'right', Aramaic תַּימנַא taymna from יָמִין yamin 'right' and Syriac ܬܰܝܡܢܳܐ taymna from ܝܰܡܝܺܢܳܐ yamina (hence the name of Yemen, the land to the south/right of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kesteven
The Parts of Kesteven ( or ) are a traditional division of Lincolnshire, England. This division had long had a separate county administration (quarter sessions), along with the two other Parts of Lincolnshire, Lindsey and Holland. Etymology The word ''Kesteven'' is supposed to have derived from two root words: the Celtic ' meaning wood (compare Modern Welsh ') and the Old Norse ', a meeting place. The earliest record of the place-name is c1000 and was spelt , developing into by 1185. Administrative areas Wapentakes and Sokes Historically, Lincolnshire was divided into wapentakes, hundreds and sokes. The following made up Kesteven: * Aswardburn Wapentake * Aveland Wapentake * Beltisloe Wapentake * Boothby Graffo Wapentake * Flaxwell Wapentake * Langoe Wapentake * Lovedon Wapentake * Ness Wapentake * Winnibriggs and Threo Wapentake * Borough and Soke of Grantham * Stamford Borough Local Government Act 1888 The three parts were given separate elected county councils ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wapentake
A hundred is an administrative division that is geographically part of a larger region. It was formerly used in England, Wales, some parts of the United States, Denmark, Southern Schleswig, Sweden, Finland, Norway, the Bishopric of Ösel–Wiek, Curonia, the Ukrainian state of the Cossack Hetmanate and in Cumberland County in the British Colony of New South Wales. It is still used in other places, including in Australia (in South Australia and the Northern Territory). Other terms for the hundred in English and other languages include ''wapentake'', ''herred'' (Danish and Bokmål Norwegian), ''herad'' ( Nynorsk Norwegian), ''hérað'' (Icelandic), ''härad'' or ''hundare'' (Swedish), ''Harde'' (German), ''hiird'' ( North Frisian), ''satakunta'' or ''kihlakunta'' (Finnish), ''kihelkond'' (Estonian), ''kiligunda'' (Livonian), ''cantref'' (Welsh) and ''sotnia'' (Slavic). In Ireland, a similar subdivision of counties is referred to as a barony, and a hundred is a subdivision of a part ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Diocese Of Lincoln
The Diocese of Lincoln forms part of the Province of Canterbury in England. The present diocese covers the ceremonial county of Lincolnshire. History The diocese traces its roots in an unbroken line to the Pre-Reformation Diocese of Leicester, founded in 679. The see of Leicester was translated to Dorchester in the late 9th century, before taking in the territory of the Diocese of Lindsey and being translated to Lincoln. The diocese was then the largest in England, extending from the River Thames to the Humber Estuary. In 1072, Remigius de Fécamp, bishop under William the Conqueror, moved the see to Lincoln, although the Bishops of Lincoln retained significant landholdings within Oxfordshire. Because of this historic link, for a long time Banbury remained a peculiar of the Bishop of Lincoln. The modern diocese remains notoriously extensive, having been reportedly referred to by Bob Hardy, Bishop of Lincoln, as "2,000 square miles of bugger all" in 2002. The dioceses of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Deanery
A deanery (or decanate) is an ecclesiastical entity in the Roman Catholic Church, the Eastern Orthodox Church, the Anglican Communion, the Evangelical Church in Germany, and the Church of Norway. A deanery is either the jurisdiction or residence of a dean. Catholic usage In the Catholic Church, Can.374 §2 of the Code of Canon Law grants to bishops the possibility to join together several neighbouring parishes into special groups, such as ''vicariates forane'', or deaneries. Each deanery is headed by a vicar forane, also called a dean or archpriest, who is—according to the definition provided in canon 553—a priest appointed by the bishop after consultation with the priests exercising ministry in the deanery. Canon 555 defines the duties of a dean as:Vicars Forane (Cann. 553–555) from the |
Beltisloe
Beltisloe is a Deanery of the Diocese of Lincoln in England, and a former Wapentake. The Wapentake of Beltisloe was established as ancient administrative division of the English county of Lincolnshire before the Norman Conquest of 1066.Open Domesday: Wapentake of Beltisloe in 1066 and 1086 accessed 9 May 2020.Allen.History of the County of Lincoln. p.277 In a wapentake was the division of a for administrative, military and judicial purposes under the |
Lincolnshire Limestone
The Lincolnshire Limestone Formation is a geological formation in England, part of the Inferior Oolite Group of the (Bajocian) Middle Jurassic strata of eastern England. It was formed around 165 million years ago, in a shallow, warm sea on the margin of the London Platform and has estuarine beds above and below it. The maximum known thickness is 40.2 metres, at around TF9730, while four kilometres further west it is 18.3 metres thick at its outcrop in the upper Witham valley. It fades out in the south, around Kettering in Northamptonshire. There are two sub-divisions, the Upper and Lower Lincolnshire Limestone Members respectively. The dividing marker is the 'Crossi' bed which is distinguished by the fossils of ''Acanthothris crossi'' it contains. The Crossi bed forms the top of the Lower Lincolnshire limestone. The bottom of the Lower Lincolnshire limestone has some of the characteristics of the underlying Lower Estuarine Series, in that it tends to contain more than usual amoun ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Blisworth Limestone
The Blisworth Limestone Formation is a geological formation primarily consisting of limestone deposited during the Bathonian stage of the Middle Jurassic, found in the Jurassic ridge which extends north and south through England. It was laid down in the shallows of the Jurassic sea and is part of the more widely defined Great Oolite Group. It was previously known as the Great Oolite Limestone, White Limestone and the Snitterby Limestone Formation. It is the lateral equivalent of the White Limestone Formation From the Jurassic ridge it extends eastwards below the later deposits and in the North Sea terminology, it is part of the West Sole Group. (Cameron p. 74) Formation The Blisworth limestone lies above the Upper Estuarine Series of strata. The latter was formed close to the coast where rivers flowed from the London-Brabant Island. The land sank a little in relation to the sea so the site lay a little further offshore. In the hot, shallow sea, the water partially evaporated s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cornbrash
The Cornbrash Formation is a Middle Jurassic geological formation in England. It ranges in age from Bathonian to Callovian, the uppermost part of the Middle Jurassic. Dinosaur remains are among the fossils that have been recovered from the formation, although none have yet been referred to a specific genus.Weishampel, et al. (2004). "Dinosaur distribution." Pp. 517-607. The name Cornbrash is an old English agricultural name applied in Wiltshire to a variety of loose rubble or brash which, in that part of the country, forms a good soil for growing corn. The name was adopted by William Smith for a thin band of shelly limestone which, in the south of England, breaks up in the manner indicated. Although only a thin group of rocks (10–25 feet c. 3–7 m), it is remarkably persistent; it may be traced from Weymouth to the Yorkshire coast, but in north Lincolnshire it is very thin, and probably dies out in the neighborhood of the Humber. It appears again, however, as a thin bed in Gr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kellaways Formation
The Kellaways Formation is a geological formation of the Callovian Series from the Jurassic. It is found in the British Isles, immediately above the Great Oolite Series: below the Oxford Clay Formation and above the Cornbrash. It consists of two layers, the Kellaways Sand, a light green-grey clayish silt and sand with layers of sand concretions, overlying the Kellaways Clay, a dark grey plastic fissile clay. They were laid down during the Callovian, offshore from the London-Brabant Island, between 165 and 160 million years ago, in the latitude of the modern Mediterranean Sea, when the structure of Britain was still taking shape. At this stage, the coal swamps of the north-western shore of the island had subsided below the sea so that the Kellaways clay was formed in fairly deep water and the Kellaways sand was blown and washed from what had become the hot desert land. The holotype of the indeterminate eusauropod ''"Ornithopsis" leedsii'' has been recovered from this formation.N ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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