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Teffont
Teffont is a civil parish in the south of Wiltshire, England, consisting of the villages of Teffont Magna and Teffont Evias. It is in the Nadder valley, north of the river, about west of Salisbury. The parish was created in 1934 by combining the two Teffonts. The population taken at the 2011 census was 248. Description Teffont has a parish council and is in the area of the Wiltshire Council unitary authority, which is responsible for almost all significant local government functions. The two former parishes each had a church, and both continue in use, although they are only about three-quarters of a mile apart; they are both Grade II* listed buildings. Until 1922 Teffont Magna was a chapelry of Dinton, and its modest church dates from the 13th century. The church at Teffont Evias was rebuilt in the 1820s, when an imposing tower was added. Part of Chilmark Quarries, a former stone quarry and now a Site of Special Scientific Interest, is in the far southwest of the pa ...
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Teffont Evias
Teffont Evias is a small village and former civil parish in the Nadder valley in the south of Wiltshire, England. Edric Holmes described the village as "most delightfully situated", and Maurice Hewlett included Teffont in his list of the half dozen most beautiful villages in England. The present buildings are mostly of local stone, and several are thatched. The civil parish was combined in 1934 with neighbouring Teffont Magna to form a united Teffont parish. Location Teffont Evias lies northeast of the large village of Tisbury and west of Wilton. The southern boundary of both the former Teffont Evias parish, and the modern Teffont parish, is the River Nadder. The village street follows a stream which rises at Teffont Magna and flows south to join the Nadder. Geology Purbeck limestone underlies almost all of the parish, with a ridge of Cretaceous Upper Greensand. Teffont Evias Quarry and Lane Cutting is protected as a geological Site of Special Scientific Interest, where ...
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Teffont Magna
Teffont Magna, sometimes called Upper Teffont, is a small village and former civil parish in the Nadder valley in the south of the county of Wiltshire, England. For most of its history Teffont Magna was a chapelry of neighbouring Dinton. In 1934 it was combined with the parish of Teffont Evias, just to the south, to form a united Teffont parish. Location Teffont Magna lies west of Dinton and west of Wilton. The parish extends north onto the chalk downs that separate the valleys of the Nadder and Wylye. The village is between Chilmark and Dinton on the B3089 Hindon to Barford St Martin road, in the valley of a stream which rises just to the north and flows south through Teffont Evias to join the Nadder. History The north boundary of the ancient parish, and hence also of the modern parish, is a prehistoric linear earthwork called Grim's Ditch. A hillfort of uncertain age known as Wick Ball Camp stands on a hilltop in the east of the parish, straddling the boundary with Di ...
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Dinton, Wiltshire
Dinton is a village, civil parish and former manor in Wiltshire, England, in the Nadder valley on the B3089 road about west of Salisbury. The parish population was 696 at the 2011 census, estimated at 733 in 2019. The civil parish includes the village of Baverstock, about east of Dinton village. History The northern bounds of the parish follow a prehistoric line known as Grim's Ditch, through downland overlooking the Wylye valley further north. Hanging Langford Camp, an Iron Age settlement, is just beyond the parish boundary. The hillfort known as Wick Ball Camp lies near the western boundary of the parish, partly within Dinton Park. A Roman road from the Mendip lead mines to Old Sarum passed east–west, just south of the ditch. The Domesday Book of 1086 recorded a settlement of 37 households at Dinton, held by Shaftesbury Abbey. After the Dissolution in 1540, much of Dinton's land was acquired by the Earls of Pembroke. Later other land was purchased by the Wyndham famil ...
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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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Æthelbald, King Of Wessex
Æthelbald (died 860) was King of Wessex from 855 or 858 to 860. He was the second of five sons of King Æthelwulf. In 850, Æthelbald's elder brother Æthelstan defeated the Vikings in the first recorded sea battle in English history, but he is not recorded afterwards and probably died in the early 850s. The next year Æthelwulf and Æthelbald inflicted another defeat on the Vikings at the Battle of Aclea. In 855 Æthelwulf went on pilgrimage to Rome and appointed Æthelbald King of Wessex, while Æthelberht, the next oldest son, became King of Kent, which had been conquered by Wessex thirty years earlier. On his way back from Rome, Æthelwulf stayed for several months with Charles the Bald, King of the Franks, whose twelve-year-old daughter Judith he married. When he returned to England in 856, Æthelbald refused to give up the crown. Most historians believe that Æthelbald continued to be king of Wessex while Æthelberht gave up Kent to his father, but some think that Wes ...
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Chilmark Quarries
Chilmark Quarries () is a 9.65 hectare biological and geological Site of Special Scientific Interest (SSSI), in the ravine south of the village of Chilmark in Wiltshire, England. The SSSI was first notified in 1977. Its importance as a home for bats led to the site being designated in 2005 (together with Fonthill Grottoes) as a European Special Area of Conservation. The western section of the site is in Chilmark civil parish, while the eastern section (separated by a minor road) is in Teffont parish. History Chilmark stone, a form of limestone, was mined here from medieval times and was used for buildings including Salisbury Cathedral. In 1936 the quarry and mines were bought by the Air Ministry and used as a storage area for RAF Chilmark, a munitions depot, until 1995. Stone extraction continued on a small scale until the quarry closed c. 2007. In March 2019 the quarry re-opened (by Chilmark Stone (Properties) Ltd) and extraction of Ashlar and Walling stone has once again s ...
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Wiltshire Council
Wiltshire Council is a council for the unitary authority of Wiltshire (excluding the separate unitary authority of Swindon) in South West England, created in 2009. It is the successor authority to Wiltshire County Council (1889–2009) and the four district councils of Kennet, North Wiltshire, Salisbury, and West Wiltshire, all of which were created in 1974 and abolished in 2009. Establishment of the unitary authority The ceremonial county of Wiltshire consists of two unitary authority areas, Wiltshire and Swindon, administered respectively by Wiltshire Council and Swindon Borough Council. Before 2009, Wiltshire was administered as a non-metropolitan county by Wiltshire County Council, with four districts, Kennet, North Wiltshire, Salisbury, and West Wiltshire. Swindon, in the north of the county, had been a separate unitary authority since 1997, and on 5 December 2007 the Government announced that the rest of Wiltshire would move to unitary status. This was later put in ...
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Belgae
The Belgae () were a large confederation of tribes living in northern Gaul, between the English Channel, the west bank of the Rhine, and the northern bank of the river Seine, from at least the third century BC. They were discussed in depth by Julius Caesar in his account of his wars in Gaul. Some peoples in Britain were also called Belgae, and O'Rahilly equated them with the Fir Bolg in Ireland. The Belgae gave their name to the Roman province of Gallia Belgica and, much later, to the modern country of Belgium; today "Belgae" is also Latin for "Belgians". Etymology The consensus among linguists is that the ethnic name ''Belgae'' comes from the Proto-Celtic root ''*belg-'' or ''*bolg-'' meaning "to swell (particularly with anger/battle fury/etc.)", cognate with the Dutch adjective ''gebelgd'' "very angry" (weak perfect participle of the verb ''belgen'' "to become angry") and ''verbolgen'' "being angry" (strong perfect participle of obsolete ''verbelgen'' "to make angry"), as well ...
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Common Brittonic
Common Brittonic ( cy, Brythoneg; kw, Brythonek; br, Predeneg), also known as British, Common Brythonic, or Proto-Brittonic, was a Celtic language spoken in Britain and Brittany. It is a form of Insular Celtic, descended from Proto-Celtic, a theorized parent tongue that, by the first half of the first millennium BC, was diverging into separate dialects or languages. Pictish is linked, likely as a sister language or a descendant branch. Evidence from early and modern Welsh shows that Common Brittonic took a significant amount of influence from Latin during the Roman period, especially in terms related to the church and Christianity. By the sixth century AD, the tongues of the Celtic Britons were more rapidly splitting into Neo-Brittonic: Welsh, Cumbric, Cornish, Breton, and possibly the Pictish language. Over the next three centuries it was replaced in most of Scotland by Scottish Gaelic and by Old English (from which descend Modern English and Scots) throughout most o ...
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Durotriges
The Durotriges were one of the Celtic tribes living in Britain prior to the Roman invasion. The tribe lived in modern Dorset, south Wiltshire, south Somerset and Devon east of the River Axe and the discovery of an Iron Age hoard in 2009 at Shalfleet, Isle of Wight gives evidence that they may also have lived in the western half of the island. After the Roman conquest, their main ''civitates'', or settlement-centred administrative units, were Durnovaria (modern Dorchester, "the probable original capital") and Lindinis (modern Ilchester, "whose former, unknown status was thereby enhanced"). Their territory was bordered to the west by the Dumnonii; and to the east by the Belgae.__NOTOC__ Name The tribe's name is known from Ptolemy's ''Geography'' and from two inscriptions on Hadrian's Wall, both dating from after the Roman conquest of Britain. It is not known if anyone referred to them as the Durotriges before they arrived in the area now known as Dorset. The name can probably be ...
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Roman Britain
Roman Britain was the period in classical antiquity when large parts of the island of Great Britain were under occupation by the Roman Empire. The occupation lasted from AD 43 to AD 410. During that time, the territory conquered was raised to the status of a Roman province. Julius Caesar invaded Britain in 55 and 54 BC as part of his Gallic Wars. According to Caesar, the Britons had been overrun or culturally assimilated by other Celtic tribes during the British Iron Age and had been aiding Caesar's enemies. He received tribute, installed the friendly king Mandubracius over the Trinovantes, and returned to Gaul. Planned invasions under Augustus were called off in 34, 27, and 25 BC. In 40 AD, Caligula assembled 200,000 men at the Channel on the continent, only to have them gather seashells ('' musculi'') according to Suetonius, perhaps as a symbolic gesture to proclaim Caligula's victory over the sea. Three years later, Claudius directed four legi ...
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Upper Greensand Formation
The Upper Greensand Formation is a Cretaceous formation of Albian to Cenomanian in age, found within the Wessex Basin and parts of the Weald Basin in southern England. It overlies the Gault Clay and underlies the Chalk Group. It varies in thickness from zero to 75 m. It is predominantly a glauconitic fine-grained sandstone, locally becoming silty. Fragmentary dinosaur remains, such as those assigned to ''Iuticosaurus'', have been recovered from this formation. It has been quarried as a building stone from Roman times, and used in London and the area of its outcrop from Devon to East Sussex. Use Sandstones from the Upper Greensand have been used as building stone since at least Roman times. Reigate Stone was mined from the Upper Greensand in north east Surrey throughout the middle ages and early modern period, forming the most important source of freestone in Medieval London. In Dorset, the Shaftesbury Sandstone was quarried between Shaftesbury and Okeford Fitzpaine and used i ...
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