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Vale Of Wardour
The Vale of Wardour encompasses the valley of the River Nadder in the county of Wiltshire, England. Geography Topography The Vale of Wardour lies east of the town of Shaftesbury and is a relatively small but varied landscape. Named after the village of Wardour, its main river is the Nadder which flows from west to east through the vale. In the west the Nadder is fed by its main tributary, the Sem; in the east the valley ends around Wilton where the Nadder is joined by the Wylye. The largest village in the vale is Tisbury.''NCA Profile:133 Blackmore Vale and Vale of Wardour (NE539)''
at publications.naturalengland.org.uk. Retrieved 25 Feb 2018.


Natural region

The vale is a western tongue of
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River Nadder
The River Nadder is a tributary of the River Avon, flowing in south Wiltshire, England. Course The river flows north from Ludwell to West End where it is joined by the Ferne Brook, close to the Lower Coombe and Ferne Brook Meadows site of special scientific interest ( SSSI). At Wardour it is joined by the River Sem. The river then flows east through Tisbury, where it is joined by the Fonthill Brook, and then onto Barford St Martin and Burcombe before reaching Wilton. Near Quidhampton, the Wylye joins from the north. After passing Harnham, the Nadder joins the Avon near Salisbury Cathedral. Including its headwaters, the river's length is about . Water quality The Environment Agency measures the water quality of the river systems in England. Each is given an overall ecological status, which may be one of five levels: high, good, moderate, poor and bad. There are several components that are used to determine this, including biological status, which looks at the quantity an ...
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Salisbury Plain
Salisbury Plain is a chalk plateau in the south western part of central southern England covering . It is part of a system of chalk downlands throughout eastern and southern England formed by the rocks of the Chalk Group and largely lies within the county of Wiltshire, but stretches into Hampshire. The plain is famous for its rich archaeology, including Stonehenge, one of England's best known landmarks. Large areas are given over to military training and thus the sparsely populated plain is the biggest remaining area of calcareous grassland in northwest Europe. Additionally the plain has arable land, and a few small areas of beech trees and coniferous woodland. Its highest point is Easton Hill. Physical geography The boundaries of Salisbury Plain have never been truly defined, and there is some difference of opinion as to its exact area. The river valleys surrounding it, and other downs and plains beyond them loosely define its boundaries. To the north the scarp of the ...
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Old Wardour Castle
Wardour Castle is a ruined 14th-century castle at Wardour, on the boundaries of the civil parishes of Tisbury and Donhead St Andrew in the English county of Wiltshire, about west of Salisbury. The castle was built in the 1390s, came into the ownership of the Arundells in the 16th century and was rendered uninhabitable in 1643 and 1644 during the English Civil War. A Grade I listed building, it is managed by English Heritage and open to the public. History Construction and design In the 1300s, the land on which the castle was built was owned by the St Martin family until Sir Lawrence de St Martin died in 1385. Later in that year the land was acquired by John, the fifth Baron Lovell. In 1392 or 1393 Baron Lovell was granted permission by King Richard II to build a castle on the site. It was constructed using locally quarried Tisbury greensand, and the master mason was William Wynford. The design was inspired by the hexagonal (6-sided) castles then in fashion in parts ...
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Fovant Badges
The Fovant Badges are a set of regimental badges cut into a chalk hill, Fovant Down, near Fovant, in southwest Wiltshire, England. They are located between Salisbury and Shaftesbury on the A30 road in the Nadder valley; or approximately southeast of Fovant. They were created by soldiers garrisoned nearby, and waiting to go to France, during the First World War; the first in 1916. They are clearly visible from the A30 road which runs through the village. Nine of the original twenty remain, and are scheduled ancient monuments and recognised by the Imperial War Museum as war memorials. Further badges have been added more recently. The Fovant Badge Society holds an annual Drumhead Service which is attended by the Australian High Commissioner, local mayors and members of parliament. These services fund the upkeep of the badges. Construction After the outlines were cut into the grass-covered hillsides, they were refilled with chalk brought from a nearby slope, up to 50 tons pe ...
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Castle Ditches
Castle Ditches is the site of an Iron Age trivallate hillfort in the southeast of Tisbury parish in Wiltshire, England. It is probable that its ancient name was ''Spelsbury''; it was referred to as ''Willburge'' in Tisbury's charter of 984 A.D. Its shape is roughly triangular, and follows the contours of the small hill upon which it sits. The earthworks comprise a triple row of ramparts and ditches, now covered on three sides by woodland. There is a large entrance towards the southeast, where there is the shallowest incline of the hill; but there is also a narrow slit on the opposite side. The area within the site encompasses nearly , and the greatest height of the ramparts is about . Castle Ditches was recorded as a Scheduled Monument in 1932. Location The site is at , about southeast of Tisbury village. The hill has a summit of 193m AOD and overlooks the valley of the River Nadder to the north. Public footpaths surround the site, but the land is privately owned. See also ...
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Castle Rings, Wiltshire
Castle Rings is a univallate hill fort in the parish of Donhead St Mary in Wiltshire in England.Wiltshire and Swindon History Centre 2011. The fort is a Scheduled Ancient Monument, with a list entry identification number of 1005698.Historic England. Castle Rings has been dated to the Iron Age and is situated at an altitude of upon Upper Greensand sandstone beds. The main bulk of the fort enclosure lies within the boundaries of Donhead St Mary parish but some of the outlying earthworks are situated in the neighbouring Sedgehill and Semley parish. In the mid-1980s a metal detectorist unearthed a hoard of stater coins of the Durotriges tribe within the hill fort. Lady Theodora Grosvenor described the fort in her 1867 book ''Motcombe, Past and Present'': Physical characteristics The rampart of the fort stands high with a deep ditch; the ditch is set between double earth banks. The ditch averages wide and varies in depth to a maximum of . The inner rampart has an average wid ...
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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 Basin, ...
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Barford St Martin
Barford St Martin is a village and civil parish in Wiltshire, England, about west of Wilton, around the junction of the A30 and the B3089. Barford is known as one of the Nadder Valley villages, named for the River Nadder which flows through the parish. Grovely Wood forms the northern section of the parish. History Prehistoric sites in the parish include the earthworks known as Ebsbury, an Iron Age settlement, field system and possible hillfort, and a Romano-British enclosed settlement, on a hilltop in the north of the parish which overlooks the Wylye valley. Grovely Ditch or Grim's Ditch, a pre-Roman earthwork, runs through Grovely Wood a little further south. A small settlement called ''Bereford'', with nine households, was recorded in the Domesday Book compiled in 1085–1086. The St Martin suffix, from the dedication of the church, was added by 1304 to distinguish it from Barford manor in Downton parish. Amesbury Priory acquired 78 acres in 1197, and continued to hold th ...
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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 ...
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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
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West Wiltshire Downs
The West Wiltshire Downs is an area of downland in the west of the county of Wiltshire, England. The West Wiltshire Downs are geologically the same unit as Salisbury Plain to the north and Cranborne Chase to the south. The West Wiltshire Downs are split between two of the National Character Areas designated by Natural England: No. 134, Dorset Downs and Cranborne Chase; and No. 132, Salisbury Plain Salisbury Plain is a chalk plateau in the south western part of central southern England covering . It is part of a system of chalk downlands throughout eastern and southern England formed by the rocks of the Chalk Group and largely lies wi ... and West Wiltshire Downs.''Dorset Downs and Cranborne Chase''
at www.naturalengland.org.uk. Retrieved 25 Feb 2018.

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Natural England
Natural England is a non-departmental public body in the United Kingdom sponsored by the Department for Environment, Food and Rural Affairs. It is responsible for ensuring that England's natural environment, including its land, flora and fauna, freshwater and marine environments, geology and soils, are protected and improved. It also has a responsibility to help people enjoy, understand and access the natural environment. Natural England focuses its activities and resources on four strategic outcomes: * a healthy natural environment * enjoyment of the natural environment * sustainable use of the natural environment * a secure environmental future Roles and responsibilities As a non-departmental public body (NDPB), Natural England is independent of government. However, the Secretary of State for Environment, Food & Rural Affairs has the legal power to issue guidance to Natural England on various matters, a constraint that was not placed on its predecessor NDPBs. Its powers inc ...
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