Ashmore
Ashmore is a village and civil parish in the North Dorset district of Dorset, England, southwest of Salisbury. The village is centred on a circular pond and has a church and several stone cottages and farms, many with thatched roofs. It is the highest village in the county with the contour passing close to the village church (although the north side of the town of Shaftesbury, Dorset, is slightly higher at ). The pond or "mere" gave the village its original name of "Ash-mere".North Dorset District Council,''North Dorset Official District Guide'', Home Publishing Co. Ltd.,c.1983. p30 In the 2011 census the parish had a population of 188. History Three round barrows have been found in the parish: two barrows south of the village near Well Bottom, and one west of the village near the boundary with the village of Fontmell Magna; this latter barrow was excavated in the 19th century and bones were recovered. Ashmore may have been the site of a Neolithic market place or settlem ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Ashmore St Nicholas Church
Ashmore is a village and civil parish in the North Dorset district of Dorset, England, southwest of Salisbury. The village is centred on a circular pond and has a church and several stone cottages and farms, many with thatched roofs. It is the highest village in the county with the contour passing close to the village church (although the north side of the town of Shaftesbury, Dorset, is slightly higher at ). The pond or "mere" gave the village its original name of "Ash-mere".North Dorset District Council,''North Dorset Official District Guide'', Home Publishing Co. Ltd.,c.1983. p30 In the 2011 census the parish had a population of 188. History Three round barrows have been found in the parish: two barrows south of the village near Well Bottom, and one west of the village near the boundary with the village of Fontmell Magna; this latter barrow was excavated in the 19th century and bones were recovered. Ashmore may have been the site of a Neolithic market place or settlem ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Cranborne Chase
Cranborne Chase () is an area of central southern England, straddling the counties Dorset, Hampshire and Wiltshire. It is part of the Cranborne Chase and West Wiltshire Downs Area of Outstanding Natural Beauty (AONB). The area is dominated by, and often considered to be synonymous with, a chalk downland plateau. Part of the English Chalk Formation, it is adjacent to Salisbury Plain and the West Wiltshire Downs in the north, and the Dorset Downs to the south west. The highest point is Win Green Down, in Wiltshire, at . Historically a medieval hunting forest, the area is also noted for its Neolithic and Bronze age archaeology and its rural agricultural character. Definitions As an informally defined region, the boundaries of Cranborne Chase vary depending on usage. When defined as the chalk plateau, it is clearly bounded by escarpments which face the valleys of the Blackmore Vale to the west, the Vale of Wardour to the north, and the Hampshire Avon to the east. To the south th ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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North Dorset
North Dorset was a local government district in Dorset, England. It was largely rural, but included the towns of Blandford Forum, Gillingham, Shaftesbury, Stalbridge and Sturminster Newton. Much of North Dorset was in the River Stour valley and is called the Blackmore Vale. The economy of North Dorset was largely dairy agriculture based. The district was formed on 1 April 1974, under the Local Government Act 1972, from the municipal boroughs of Blandford Forum, Shaftesbury, Blandford Rural District, Shaftesbury Rural District and Sturminster Rural District. The district and its council were abolished on 1 April 2019 and, together with the other 4 districts outside the greater Bournemouth area, incorporated into a Dorset unitary authority. At the 2001 UK census North Dorset had a population of 61,905, a rise of 8,300 from 1991, with 25,248 households. North Dorset is home to North Dorset Rugby Football Club. Settlements :''Towns with a population over 2,500 are in b ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Cranborne Hundred
Cranborne Hundred was a hundred in the county of Dorset, England, containing the following parishes: *Ashmore * Belchalwell (divided between Okeford Fitzpaine and Fifehead Neville 1884) *Cranborne (part) * East Woodyates (created 1858) * Edmondsham (part) * Farnham *Hampreston (part; entire from the 1860s, when the other part was transferred from Hampshire) *Pentridge * Shillingstone * Tarrant Gunville * Tarrant Rushton *Tollard Royal (divided between Dorset and Wiltshire until the 1880s, when the Dorset part was transferred to Wiltshire) *Turnworth *West Parley *Witchampton :(''Alderholt and Verwood were created from Cranborne in 1894'') See also *List of hundreds in Dorset This is a list of hundreds in the county of Dorset, England. Between the Anglo-Saxon period and the Local Government Act (1888), the county of Dorset was divided into hundreds and boroughs (and from the mediaeval period, liberties as well). Th ... Sources *Boswell, Edward, 1833: ''The Civil Division of ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Ploughland
The carucate or carrucate ( lat-med, carrūcāta or ) was a medieval unit of land area approximating the land a plough team of eight oxen could till in a single annual season. It was known by different regional names and fell under different forms of tax assessment. England The carucate was named for the carruca heavy plough that began to appear in England in the late 9th century, it may have been introduced during the Viking invasions of England.White Jr., Lynn, The Life of the Silent Majority, pg. 88 of Life and Thought in the Early Middle Ages, ed. Robert S. Hoyt, University of Minnesota Press, Minneapolis. 1967 It was also known as a ploughland or plough ( ang, plōgesland, "plough's land") in the Danelaw and usually, but not always, excluded the land's suitability for winter vegetables and desirability to remain fallow in crop rotation. The tax levied on each carucate came to be known as " carucage". Though a carucate might nominally be regarded as an area of 120 acres (49 hec ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Bournemouth International Airport
Bournemouth Airport (previously known as Hurn Airport and Bournemouth International Airport) is an airport located north-northeast of Bournemouth, in southern England. The site opened as RAF Hurn in 1941, but was transferred to civil control in 1944. For a short period (between 1944 and 1946) Hurn served as London's international airport, until the opening of facilities at Heathrow. Commercial services resumed in the late 1950s, with Palmair commencing flights to Palma, Majorca in October 1958. Subsequently, Ryanair and TUI Airways based aircraft at the airport, with scheduled flights now frequently serving Western Europe and the Mediterranean area, with charter and seasonal services serving North Africa, North America, and the Caribbean. Passenger numbers peaked in 2007 when just over one million passed through the airport. In 2019, the passenger total was around 803,000. This dropped to around 176,000 in 2020 due to the COVID-19 Pandemic Ryanair and TUI Airways are ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Tisbury Railway Station
Tisbury railway station serves the village of Tisbury, Wiltshire, Tisbury in Wiltshire, England. It is currently managed by South Western Railway (train operating company), South Western Railway and is on the West of England Main Line, down the line from . History The Salisbury and Yeovil Railway (S&YR) opened Tisbury railway station with the first section of its line, from to Gillingham (Dorset) railway station, Gillingham, on 2 May 1859. At first only passengers were catered for, but goods traffic started on 1 September 1860. The main goods yard and warehouse was on the north side of the line at the west end of the station, but some sidings were also added on the opposite side of the line. Initially the railway had just a single track but a passing loop and two Railway platform, platforms were provided at Tisbury. The whole line was double track by 1870 and a signal box was opened here in 1875. The S&YR never operated any trains, instead they were provided by the London and ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Area Of Outstanding Natural Beauty
An Area of Outstanding Natural Beauty (AONB; , AHNE) is an area of countryside in England, Wales, and Northern Ireland, that has been designated for conservation due to its significant landscape value. Areas are designated in recognition of their national importance by the relevant public body: Natural England, Natural Resources Wales, and the Northern Ireland Environment Agency respectively. In place of AONB, Scotland uses the similar national scenic area (NSA) designation. Areas of Outstanding Natural Beauty enjoy levels of protection from development similar to those of UK national parks, but unlike national parks the responsible bodies do not have their own planning powers. They also differ from national parks in their more limited opportunities for extensive outdoor recreation. History The idea for what would eventually become the AONB designation was first put forward by John Dower in his 1945 ''Report to the Government on National Parks in England and Wales''. Dower ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Cranborne Chase And West Wiltshire Downs
Cranborne Chase and West Wiltshire Downs is an Area of Outstanding Natural Beauty (AONB) covering of Dorset, Hampshire, Somerset and Wiltshire. It is the sixth largest AONB in England. The area was designated as an AONB in 1981 and confirmed in October 1983. Since 2014, the AONB Partnership of local authorities has used the abbreviated name Cranborne Chase AONB in its promotion of the area. The AONB includes several distinct landscape areas, among them: * Cranborne Chase, an area of chalk downland in the south. * West Wiltshire Downs, an area of chalk downland in the north. * The Vale of Wardour, a wide clay valley between the two areas of downland. * The area around Stourhead and Longleat on the Somerset-Wiltshire border, which has a distinctive characteristic of upper greensand hills. Much of the landscape is farmed chalk downland. The people who populated the area thousands of years ago constructed Ackling Dyke and the Knowlton Circles. The area was later the scene of conf ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Dry Valley
A dry valley may develop on many kinds of permeable rock, such as limestone and chalk, or sandy terrains that do not regularly sustain surface water flow. Such valleys do not hold surface water because it sinks into the permeable bedrock. There are many examples of chalk dry valleys along the North and South Downs in Southern England. Notably the National Trust-owned Devil's Dyke near Brighton covers some of downland scarp, and includes the deepest dry valley in the world – created when melting water eroded the chalk downland to the permafrost layer after the last ice age. The three-quarter mile long curved dry valley is around in height and attracts tourists with its views of Sussex, Hampshire and Kent. Other examples include the Alkham Valley near Dover, and the Hartley Bottom and Fawkham valleys near Dartford in north Kent. There are many examples of limestone dry valleys in the Peak District and the Yorkshire Wolds. A notable example is the valley of the River Manifold ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Flint
Flint, occasionally flintstone, is a sedimentary cryptocrystalline form of the mineral quartz, categorized as the variety of chert that occurs in chalk or marly limestone. Flint was widely used historically to make stone tools and start fires. It occurs chiefly as nodules and masses in sedimentary rocks, such as chalks and limestones.''The Flints from Portsdown Hill'' Inside the nodule, flint is usually dark grey, black, green, white or brown in colour, and often has a glassy or waxy appearance. A thin layer on the outside of the nodules is usually different in colour, typically white and rough in texture. The nodules can often be found along s and [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Chalk
Chalk is a soft, white, porous, sedimentary carbonate rock. It is a form of limestone composed of the mineral calcite and originally formed deep under the sea by the compression of microscopic plankton that had settled to the sea floor. Chalk is common throughout Western Europe, where deposits underlie parts of France, and steep cliffs are often seen where they meet the sea in places such as the Dover cliffs on the Kent coast of the English Channel. Chalk is mined for use in industry, such as for quicklime, bricks and builder's putty, and in agriculture, for raising pH in soils with high acidity. It is also used for " blackboard chalk" for writing and drawing on various types of surfaces, although these can also be manufactured from other carbonate-based minerals, or gypsum. Description Chalk is a fine-textured, earthy type of limestone distinguished by its light color, softness, and high porosity. It is composed mostly of tiny fragments of the calcite shells or skeletons ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |