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Belchalwell
Belchalwell is a small village and former civil parish, now in the parish of Okeford Fitzpaine in the Blackmore Vale, in the Dorset district, in the ceremonial county of Dorset, England. It lies south of Sturminster Newton and northwest of Blandford Forum. Belchalwell Street is sited on Upper Greensand, with Lower Belchalwell on the boundary of Gault and Kimmeridge Clay, both beneath the north slopes of Bell Hill, part of the Dorset Downs. In 1881 the parish had a population of 169. On 25 March 1885 the parish was abolished and merged with Okeford Fitzpaine and Fifehead Neville. Belchalwell is Saxon in origin, with a medieval church, St Aldhelm's Church, much renovated. The name of the village describes a cold well on a hillside. The village has approximately 30 properties with fewer than a hundred residents, and is much reduced in size from former times, largely due to reductions in agricultural employment, which has always been the primary industry. One former resident was ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
St Aldhelm's Church, Belchalwell
St Aldhelm's Church is a Grade II* listed Anglican church in the village of Belchalwell, Dorset. It is in the ecclesiastical parish of Belchalwell, which is part of the Benefice of Hazelbury Bryan and the Hillside Parishes. The church is situated on higher ground above Belchalwell village. The oldest parts of the church are of the 12th century; much of the building is of the 15th century. Saint Aldhelm There being no trace of the original dedication, after church records were lost in a fire in 1731, the church was dedicated in 1959 to Saint Aldhelm. Saint Aldhelm (c.639–709) was a notable scholar in Wessex in the time of King Ine; he was appointed the first Abbot of Malmesbury c.675, and became the first Bishop of Sherborne in 705. Athelstan Museum, Malmesbury, accessed 29 October 2017.
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Okeford Fitzpaine
Okeford Fitzpaine is a village and Civil parishes in England, civil parish in the English county of Dorset, situated in the Blackmore Vale south of the town of Sturminster Newton. It is sited on a thin strip of greensand under the escarpment, scarp face of the Dorset Downs. In the United Kingdom Census 2011, 2011 census the civil parishes in England, civil parish—which includes the village of Belchalwell to the west and most of the hamlet of Fiddleford to the north—had 404 dwellings, 380 households and a population of 913. History Prehistoric remains within the parish include three cross dykes and five round barrows on the chalk hills south of the village, and an Iron Age hill fort on Banbury Hill, towards Sturminster Newton. Banbury covers about and is of univallate (single rampart) construction, though its defences have been reduced by cultivation. In 1086 in the Domesday Book Okeford Fitzpaine was recorded as ''Adford''; it had 40 households, 16 ploughlands, of mead ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bell Hill, Dorset
At 258 metres, Bell Hill is one of the highest hills in the county of Dorset, England and a high point on the Wessex Ridgeway. Location Bell Hill lies about 5 miles west of Blandford Forum. The village of Ibberton nestles against its southwestern foot, whilst a little further to the northeast, below Okeford Hill on the same ridgeline, is the village of Okeford Fitzpaine.Ordnance Survey 1:50,000 Landranger series, no. 194 The summit itself lies on a ridge running from northeast to southwest. To the northwest its escarpment drops steeply in to the Blackmore Vale and Stour Valley, whilst to the southeast the woods of Turnworth Clump and Ringmoor are bracketed by two more ridges, Ibberton Long Down and Turnworth Down, forming a horseshoe with Bell Hill. Another spur runs east from Turnworth Down to Shillingstone Hill, site of a quarry and a popular cross-country race. A trig point on the Wessex Ridgeway marks this subsidiary summit. History There is evidence of prehistoric s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jack Hargreaves
John Herbert Hargreaves OBE (31 December 1911 – 15 March 1994) was an English television presenter and writer whose enduring interest was to comment without nostalgia or sentimentality on accelerating distortions in relations between the city and the countryside, seeking – in entertaining ways – to question and rebut metropolitan assumptions about its character and function. Hargreaves is remembered for appearing on ''How (TV series), How'', a children's programme which he also conceived, about how things worked or ought to work. It ran from 1966 on Southern Television (of which Hargreaves was a director) and networked on ITV Network, ITV until the demise of Southern in 1981. Hargreaves was the presenter of the weekly magazine programme ''Out of Town'', first broadcast in 1960 following the success of his series ''Gone Fishing'' the previous year. Broadcast on Friday evenings on Southern Television the programme was also taken up by many of the other ITV regions, usually i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Blackmore Vale
The Blackmore Vale (; less commonly spelt ''Blackmoor'') is a vale, or wide valley, in north Dorset, and to a lesser extent south Somerset and southwest Wiltshire in southern England. Geography The vale is part of the Stour valley and part of the natural region known as the Blackmoor Vale and Vale of Wardour. The southern periphery of the vale is in the Dorset National Landscape area. To the south and east, the vale is clearly delimited by the steep escarpments of two areas of higher chalk downland, the Dorset Downs to the south, and Cranborne Chase to the east. To the north and west, the definitions of the vale are more ambiguous, as the landscape changes more gradually around the upper reaches of the Stour and its tributaries. One definition places the boundary along the watershed between the Stour and neighbouring valleys of the Yeo to the west and Brue to the north. A narrower definition places the limits of the vale close to the county boundary and villages like Bou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fifehead Neville
Fifehead Neville is a village and Civil parishes in England, civil parish in the county of Dorset in southern England, situated in the Blackmore Vale about southwest of the town of Sturminster Newton. In the United Kingdom Census 2011, 2011 census the population of the parish was 147. Toponymy The first part of the name Fifehead Neville derives from the Old English ''fīf'' and ''hīd'', meaning '(estate of) five Hide (unit), hides of land'. It was recorded as ''Fifhide'' in the Domesday Book of 1086. The second part derives from the de Neville family who were here in the 13th century; in 1287 the name ''Fyfhud Neuyle'' was recorded. This differentiated this Fifehead from other Dorset manorial holdings called Fifehead (Fifehead St Quintin and Fifehead St Magdalen). History In a field bordering the River Divelish the remains of two wings of a Roman villa were found in 1880 and 1903. Floor mosaics and part of a hypocaust system were uncovered. The archaeological findings are on ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anglo-Saxons
The Anglo-Saxons, in some contexts simply called Saxons or the English, were a Cultural identity, cultural group who spoke Old English and inhabited much of what is now England and south-eastern Scotland in the Early Middle Ages. They traced their origins to Germanic peoples, Germanic settlers who became one of the most important cultural groups in Britain by the 5th century. The Anglo-Saxon period in Britain is considered to have started by about 450 and ended in 1066, with the Norman conquest of England, Norman Conquest. Although the details of Anglo-Saxon settlement of Britain, their early settlement and History of Anglo-Saxon England, political development are not clear, by the 8th century an Anglo-Saxon cultural identity which was generally called had developed out of the interaction of these settlers with the existing Romano-British culture. By 1066, most of the people of what is now England spoke Old English, and were considered English. Viking and Norman invasions chang ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
A Vision Of Britain Through Time
The Great Britain Historical GIS (or GBHGIS) is a spatially enabled database that documents and visualises the changing human geography of the British Isles, although is primarily focussed on the subdivisions of the United Kingdom mainly over the 200 years since the first census in 1801. The project is currently based at the University of Portsmouth, and is the provider of the website ''A Vision of Britain through Time''. NB: A "GIS" is a geographic information system, which combines map information with statistical data to produce a visual picture of the iterations or popularity of a particular set of statistics, overlaid on a map of the geographic area of interest. Original GB Historical GIS (1994–99) The first version of the GB Historical GIS was developed at Queen Mary, University of London between 1994 and 1999, although it was originally conceived simply as a mapping extension to the existing Labour Markets Database (LMDB). The system included digital boundaries for ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dorset Downs
The Dorset Downs are an area of chalk downland in the centre of the county Dorset in south west England. The downs are the most western part of a larger chalk formation which also includes (from west to east) Cranborne Chase, Salisbury Plain, Hampshire Downs, Chiltern Hills, North Downs and South Downs.''Uplift, Erosion and Stability: Perspectives on Long-term Landscape Development'' ed. by Smith, Bernard J., Whalley Wilfred B. and Warke Patricia A. (1999), Geological Society Special Publication No. 162, Bath. Accessed on 3 Apr 2013. Physical geography The Dorset Downs are bounded on the north, along the steep scarp face, by the[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kimmeridge Clay
The Kimmeridge Clay is a sedimentary rock, sedimentary deposit of fossiliferous marine clay which is of Late Jurassic to lowermost Cretaceous age and occurs in southern and eastern England and in the North Sea. This rock formation (geology), formation is the major source rock for North Sea oil. The fossil fauna of the Kimmeridge Clay includes turtles, crocodiles, Sauropoda, sauropods, Plesiosauria, plesiosaurs, Pliosauroidea, pliosaurs and ichthyosaurs, as well as a number of invertebrate species. Description Kimmeridge Clay is named after the village of Kimmeridge on the Dorset coast of England, where it is well exposed and forms part of the Jurassic Coast World Heritage Site. Onshore, it is of Late Jurassic (Kimmeridgian) age and outcrops across England, in a band stretching from Dorset in the south-west, north-east to North Yorkshire. Offshore, it extends into the Lower Cretaceous (Berriasian Stage) and it is found throughout the Southern, Central and Northern North Sea. Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dorset (district)
Dorset is a unitary authority area, existing since 1 April 2019, in the ceremonial county of Dorset, England. It covers all of the ceremonial county except for Bournemouth, Christchurch and Poole. The council of the district is Dorset Council, which is in effect Dorset County Council re-constituted so as to be vested with the powers and duties of five district councils which were abolished, and shedding its partial responsibility for and powers in Christchurch. History and statutory process Statutory instruments for re-organisation of Dorset (as to local government) were made in May 2018. These implemented the Future Dorset plan to see all councils then existing within the county abolished and replaced by two new unitary authorities on 1 April 2019. * The unitary authorities of Bournemouth and Poole merged with the non-metropolitan district of Christchurch to create a single unitary authority called Bournemouth, Christchurch and Poole Council, which has since created a BCP abb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gault
The Gault Formation is a geological formation of stiff blue clay deposited in a calm, fairly deep-water marine environment during the Lower Cretaceous Period (Upper and Middle Albian). It is well exposed in the coastal cliffs at Copt Point in Folkestone, Kent, England, where it overlays the Lower Greensand formation, and underlies the Upper Greensand Formation. These represent different facies, with the sandier parts probably being deposited close to the shore and the clay in quieter water further from the source of sediment; both are believed to be shallow-water deposits. The etymology of the name is uncertain and probably of local origin. Distribution It is found in exposure on the south side of the North Downs and the north side of the South Downs. It is also to be found beneath the scarp of the Berkshire Downs, in the Vale of White Horse, in Oxfordshire, England, and on the Isle of Wight where it is known as Blue Slipper. Gault underlies the chalk beneath the London Ba ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
