John Billingsley (agriculturist)
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John Billingsley (agriculturist)
John Billingsley (1747–1811) was an agricultural pioneer in 18th century Somerset, England. The writer of the 1794 Survey of Somerset, Billingsley was a leading agriculturalist who was one of the founders of the Bath and West Society, known today as the Royal Bath and West of England Society. He lived all his life at Ashwick Grove. Family life He was born in 1747, the grandson of Nicholas Billingsley, a Presbyterian dissenter who was minister at Ashwick from 1699 to 1729. Little is known about his early life but by 1782, he was listed as Brewer along with Ryan Gosling of the Oakhill Brewery in the neighbouring village of Oakhill, and may have been involved in the wool trade before that. He was described as a leading member of the Presbyterian church although at some stage he was reconciled with the Church of England. ''General View of the Agriculture of the County of Somerset'' The 18th century was largely one of peace in Somerset, but the Industrial Revolution in th ...
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Ashwick
Ashwick is a village in the Mendip district of Somerset, England, about three miles north of Shepton Mallet and seven miles east from Wells. It has also been a civil parish since 1826. The parish had a population of 1,352 according to the 2011 census, and apart from Ashwick village also includes Gurney Slade and Oakhill. History The area around Ashwick has evidence of occupation since the Iron Age, being in close proximity to Maesbury Castle. In Roman Britain, Fosse Way was constructed, which passes to the east of the parish. Although Oakhill is the larger village today, Ashwick is the older settlement, dating back to Anglo-Saxon times. It appears in the Domesday book as a settlement called Escewiche, which translates as 'the hamlet or farmstead by the ash trees'. The parish of Ashwick was part of the Hundred of Kilmersdon. The village is the site of Ashwick Court, a country house dating from the late 17th century and Grade II* listed. Anthony Newley's short-lived 1960 ATV ...
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River Brue
The River Brue originates in the parish of Brewham in Somerset, England, and reaches the sea some west at Burnham-on-Sea. It originally took a different route from Glastonbury to the sea, but this was changed by Glastonbury Abbey in the twelfth century. The river provides an important drainage route for water from a low-lying area which is prone to flooding which man has tried to manage through rhynes, canals, artificial rivers and sluices for centuries. The Brue Valley Living Landscape is an ecological conservation project based on the Somerset Levels and Moors and managed by the Somerset Wildlife Trust. The valley includes several Sites of Special Scientific Interest including Westhay Moor, Shapwick Heath and Shapwick Moor. Much of the area has been at the centre of peat extraction on the Somerset Levels. The Brue Valley Living Landscape project commenced in January 2009 to restore and reconnect habitat that will support wildlife. The aim is to be able to sustain itself in ...
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Compton Martin
Compton Martin is a small village and civil parish within the Chew Valley in Somerset and in the Bath and North East Somerset unitary authority in England. The parish has a population of 508. It lies between Chew Valley Lake and Blagdon Lake, north of the Mendip Hills, approximately south of Bristol on the A368 road Weston-super-Mare to Bath, between Blagdon and West Harptree. A spring rises near the church and feeds the village duck pond, which used to power a paper mill, and ultimately becomes the River Yeo. The Big Green Gathering takes place at Fernhill Farm above the village. History There is evidence of habitation of the area from prehistoric times and the Romans mined lead in the local hill. According to Robinson it is listed in the 1086 Domesday Book as ''Comtona''. The Manor of Compton was given by William the Conqueror to Serlo de Burci. In the reign of Henry I of England it passed to his grandson, Robert fitz Martin, who gave the village the latter half of its ...
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Mendip Hills
The Mendip Hills (commonly called the Mendips) is a range of limestone hills to the south of Bristol and Bath in Somerset, England. Running from Weston-super-Mare and the Bristol Channel in the west to the Frome valley in the east, the hills overlook the Somerset Levels to the south and the Chew Valley and other tributaries of the Avon to the north. The hills give their name to the local government district of Mendip, which administers most of the area. The higher, western part of the hills, covering has been designated an Area of Outstanding Natural Beauty (AONB), which gives it a level of protection comparable to a national park. The hills are largely formed from Carboniferous Limestone, which is quarried at several sites. Ash–maple woodland, calcareous grassland and mesotrophic grassland which can be found across the Mendip Hills provide nationally important semi-natural habitats. With their temperate climate these support a range of flora and fauna including birds, but ...
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Sir Benjamin Hobhouse, 1st Baronet
Sir Benjamin Hobhouse, 1st Baronet (1757–1831) was an English politician. Life The son of John Hobhouse, a slave trader and merchant at Bristol (and nephew to Isaac Hobhouse), he received his education at Bristol grammar school and Brasenose College, Oxford, where he graduated B.A. in 1778. In 1781 he proceeded M.A., and was called to the bar at the Middle Temple. At the general election of 1796 Hobhouse stood for parliament at Bristol without success, but in February 1797 he was elected M.P. for Bletchingley in Surrey, in 1802 for Grampound in Cornwall, and in 1806 for Hindon in Wiltshire. He then represented Hindon till he withdrew from political life in 1818. In 1803 he took office under Henry Addington as secretary to the board of control. He resigned this post in May 1804, and in 1805 was appointed chairman of the committees for supplies. He was also first commissioner for investigating the debts of the nabobs of the Carnatic. Hobhouse was made a baronet on 22 Dec ...
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Dorset And Somerset Canal
The Dorset and Somerset Canal was a proposed canal in southwestern England. The main line was intended to link Poole, Dorset with the Kennet and Avon Canal near Bradford on Avon, Wiltshire. A branch was to go from the main line at Frome to the southern reaches of the Somerset coalfield at Nettlebridge. Construction of the branch started in 1786, using boat lifts rather than locks to cope with changes of level, but the company ran out of money and the canal was abandoned in 1803, never to be completed. Proposals Plans for a major canal to link Bristol and Poole, and therefore to make travel from the Bristol Channel to the English Channel easier and safer, were proposed in 1792. The suggested route passed through Wareham, Sturminster Newton, Wincanton and Frome, joining the River Avon at Bath. Collieries in the Mendips near Nettlebridge were to be served by a branch canal, while the main trade was seen as coal travelling southwards and clay travelling northwards. A public me ...
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Somerset Coal Canal
The Somerset Coal Canal (originally known as the Somersetshire Coal Canal) was a narrow canal in England, built around 1800. Its route began in basins at Paulton and Timsbury, ran to nearby Camerton, over two aqueducts at Dunkerton, through a tunnel at Combe Hay, then via Midford and Monkton Combe to Limpley Stoke where it joined the Kennet and Avon Canal. This link gave the Somerset coalfield (which at its peak contained 80 collieries) access east toward London. The longest arm was long with 23 locks. From Midford an arm also ran via Writhlington to Radstock, with a tunnel at Wellow. A feature of the canal was the variety of methods used at Combe Hay to overcome height differences between the upper and lower reaches: initially by the use of caisson locks; when this method failed an inclined plane trackway; and finally a flight of 22 conventional locks. The Radstock arm was never commercially successful and was replaced first with a tramway in 1815 and later in ...
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Kennet And Avon Canal
The Kennet and Avon Canal is a waterway in southern England with an overall length of , made up of two lengths of navigable river linked by a canal. The name is used to refer to the entire length of the navigation rather than solely to the central canal section. From Bristol to Bath the waterway follows the natural course of the River Avon before the canal links it to the River Kennet at Newbury, and from there to Reading on the River Thames. In all, the waterway incorporates 105 locks. The two river stretches were made navigable in the early 18th century, and the canal section was constructed between 1794 and 1810. In the late 19th and early 20th centuries, the canal gradually fell into disuse after the opening of the Great Western Railway. In the latter half of the 20th century the canal was restored in stages, largely by volunteers. After decades of dereliction and much restoration work, it was fully reopened in 1990. The Kennet and Avon Canal has been developed as a pop ...
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Turnpike Trust
Turnpike trusts were bodies set up by individual Acts of Parliament in the United Kingdom, acts of Parliament, with powers to collect road toll road, tolls for maintaining the principal roads in Kingdom of Great Britain, Britain from the 17th but especially during the 18th and 19th centuries. At the peak, in the 1830s, over 1,000 trusts administered around of turnpike road in England and Wales, taking tolls at almost 8,000 toll-gates and side-bars. During the early 19th century the concept of the turnpike trust was adopted and adapted to manage roads within the British Empire (Ireland, Canada, Australia, New Zealand, India, and South Africa) and in the United States. Turnpikes declined with the Railway mania, coming of the railways and then the Local Government Act 1888 gave responsibility for maintaining main roads to county councils and county borough councils. Etymology The term "turnpike" originates from the similarity of the gate used to control access to the road, to ...
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Quantock Hills
The Quantock Hills west of Bridgwater in Somerset, England, consist of heathland, oak woodlands, ancient parklands and agricultural land. They were England's first Area of Outstanding Natural Beauty, designated in 1956. Natural England have designated the Quantock Hills as a national character area. They are entirely surrounded by another: the Vale of Taunton and Quantock Fringes. The hills run from the Vale of Taunton Deane in the south, for about to the north-west, ending at Kilve and West Quantoxhead on the coast of the Bristol Channel. They form the western border of Sedgemoor and the Somerset Levels. From the top of the hills on a clear day, it is possible to see Glastonbury Tor and the Mendips to the east, Wales as far as the Gower Peninsula to the north, the Brendon Hills and Exmoor to the west, and the Blackdown Hills to the south. The highest point on the Quantocks is Wills Neck, at . Soil types and weather combine to support the hills' plants and animals. In 1970, an ...
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Brendon Hills
The Brendon Hills are a range of hills in west Somerset, England. The hills merge level into the eastern side of Exmoor and are included within the Exmoor National Park. The highest point of the range is Lype Hill at above sea level with a secondary summit several kilometres to the southeast at . Both points are marked by Ordnance Survey trig points and are located within enclosed farmland. Early versions of the name include ''Brunedun'' and ''Brundon'' reflecting an original name of ''Bruna'' or ''Brune'', meaning 'brown one'. ''Dun'' is a common Old English word for a fairly flat and extensive hill. This name is not connected with the village of Brendon in Devon, the name of which has a different origin. The terrain is broken by a series of deeply incised streams and rivers running roughly southwards to meet the River Haddeo, a tributary of the River Exe. The hills are quite heavily cultivated unlike their neighbouring upland areas of Exmoor and the Quantock Hills. The Brendon ...
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Water-meadow
A water-meadow (also water meadow or watermeadow) is an area of grassland subject to controlled irrigation to increase agricultural productivity. Water-meadows were mainly used in Europe from the 16th to the early 20th centuries. Working water-meadows have now largely disappeared, but the field patterns and water channels of derelict water-meadows remain common in areas where they were used, such as parts of Northern Italy, Switzerland and England. Derelict water-meadows are often of importance as wetland wildlife habitats. Water-meadows should not be confused with flood-meadows, which are naturally covered in shallow water by seasonal flooding from a river. "Water-meadow" is sometimes used more loosely to mean any level grassland beside a river. Types Two main types of water-meadow were used. Catchwork water-meadow These were used for fields on slopes, and relatively little engineering skill was required to construct them. Water from a stream or spring was fed to the top o ...
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