Glastonbury Canal
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Glastonbury Canal
The Glastonbury Canal ran for approximately through two locks from Glastonbury to Highbridge in Somerset, England, where it entered the River Parrett and from there the Bristol Channel. The canal was authorised by Parliament in 1827 and opened in 1834. It was operated by The Glastonbury Navigation & Canal Company. Most of it was abandoned as a navigation in 1854, when a railway was built along the towpath. An earlier canal had been built in the Middle Ages to supply Glastonbury Abbey and the town with stone and produce. In the early 19th century a new canal was proposed to improve commerce in Glastonbury and help with drainage of the surrounding area of the Somerset Levels. Several alternative routes were considered and costed before obtaining an Act of Parliament and issuing a prospectus to raise funds for the building of the canal. Construction commenced in the 1820s; however it was more expensive than envisaged and further funds had to be raised. It finally opened in 183 ...
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John Rennie The Younger
Sir John Rennie FRSA (30 August 1794 – 3 September 1874) was the second son of engineer John Rennie the Elder, and brother of George Rennie. Early life John Rennie was born at 27 Stamford Street, Blackfriars Road, London, on 30 August 1794. He was educated by Dr. Greenlaw at Isleworth, and afterwards by Dr. Charles Burney at Greenwich. He subsequently entered his father's manufactory in Holland Street, Blackfriars Road, where he acquired a practical knowledge of his profession, and in 1813 he was placed under Mr. Hollingsworth, resident engineer of Waterloo Bridge, the foundations of which he personally superintended. In 1815 he assisted his father in the erection of Southwark Bridge, and in 1819 he went abroad for the purpose of studying the great engineering works on the continent. J. & G. Rennie On the death of his father in 1821, John remained in partnership with his brother George, the civil engineering portion of the business being carried on by him, whereas the ...
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Saxons
The Saxons ( la, Saxones, german: Sachsen, ang, Seaxan, osx, Sahson, nds, Sassen, nl, Saksen) were a group of Germanic * * * * peoples whose name was given in the early Middle Ages to a large country (Old Saxony, la, Saxonia) near the North Sea coast of northern Germania, in what is now Germany. In the late Roman Empire, the name was used to refer to Germanic coastal raiders, and as a name similar to the later "Viking". Their origins are believed to be in or near the German North Sea coast where they appear later, in Carolingian times. In Merovingian times, continental Saxons had been associated with the activity and settlements on the coast of what later became Normandy. Their precise origins are uncertain, and they are sometimes described as fighting inland, coming into conflict with the Franks and Thuringians. There is possibly a single classical reference to a smaller homeland of an early Saxon tribe, but its interpretation is disputed. According to this proposal, the S ...
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Act Of Parliament
Acts of Parliament, sometimes referred to as primary legislation, are texts of law passed by the Legislature, legislative body of a jurisdiction (often a parliament or council). In most countries with a parliamentary system of government, acts of parliament begin as a Bill (law), bill, which the legislature votes on. Depending on the structure of government, this text may then be subject to assent or approval from the Executive (government), executive branch. Bills A draft act of parliament is known as a Bill (proposed law), bill. In other words, a bill is a proposed law that needs to be discussed in the parliament before it can become a law. In territories with a Westminster system, most bills that have any possibility of becoming law are introduced into parliament by the government. This will usually happen following the publication of a "white paper", setting out the issues and the way in which the proposed new law is intended to deal with them. A bill may also be introduced in ...
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Heathland
A heath () is a shrubland habitat found mainly on free-draining infertile, acidic soils and characterised by open, low-growing woody vegetation. Moorland is generally related to high-ground heaths with—especially in Great Britain—a cooler and damper climate. Heaths are widespread worldwide but are fast disappearing and considered a rare habitat in Europe. They form extensive and highly diverse communities across Australia in humid and sub-humid areas where fire regimes with recurring burning are required for the maintenance of the heathlands.Specht, R.L. 'Heathlands' in 'Australian Vegetation' R.H. Groves ed. Cambridge University Press 1988 Even more diverse though less widespread heath communities occur in Southern Africa. Extensive heath communities can also be found in the Texas chaparral, New Caledonia, central Chile, and along the shores of the Mediterranean Sea. In addition to these extensive heath areas, the vegetation type is also found in scattered locations acro ...
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Street, Somerset
Street is a large village and civil parish in Somerset, England, with a population of 11,805 in 2011. On a dry spot in the Somerset Levels, at the end of the Polden Hills, it is south-west of Glastonbury. There is evidence of Roman occupation. Much of the history of the village is dominated by Glastonbury Abbey, and a 12th-century causeway from Glastonbury built to transport local Blue Lias stone to it. The Society of Friends was established there by the mid-17th century. One Quaker family, the Clarks, started a business in sheepskin rugs, woollen slippers and, later, boots and shoes. This became C&J Clark which still has its headquarters in Street. In 1993, redundant factory buildings were converted to form Clarks Village, the first purpose-built factory outlet in the United Kingdom. The Shoe Museum provides information about the history of Clarks and footwear manufacture in general. The Clark family's former mansion and its estate at the edge of the village are now owned ...
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Peat Extraction On The Somerset Levels
Peat extraction on the Somerset Levels, in South West England has occurred since the area was first drained by the Romans, and continues today on an area of less than 0.5% of the total geography. The modern system in recycling land back to farm use and conservation has resulted in the creation of numerous Sites of Special Scientific Interest. History Large areas of peat were laid down on the Somerset Levels, particularly in the River Brue Valley, during the Quaternary period after the ice sheets melted. Extraction The extraction of peat from the Moors is known to have taken place during Roman times, and has been carried out since the Levels were first drained. After the Romans left Britain, from this period forward, peat extraction was undertaken by hand by the owning or tenanted farmers. By the late Victorian period, the Eclipse Peat Company was the main commercial extractor of peat, operating initially across Shapwick Heath. In June 1961, on opening a new areas for p ...
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Galton's Canal
Galton's Canal was a 1-mile 3 furlong (2.2 km) canal with one canal lock, lock, crossing Westhay Moor in Somerset, England, and connecting the River Brue to the North Drain. It was operational by 1822, and ceased to be used after the 1850s. History Few details of the canal have survived, and the main source of information about it comes from a paper submitted to the Journal of the Royal Agricultural Society of England by Erasmus Galton, and published in 1845. The journal was chosen because the main purpose of the canal was the improvement of a peat bog, to provide agricultural land. In 1811, Samuel Galton Jr., a financier from Duddeston, in Birmingham, owned of peat bog in the parish of Meare, which formed part of Westhay Moor. The moor had been split up into tenements by an Act of Parliament in 1790, but most of it remained unimproved, and was only suitable for the cutting of turf, which was used as a fuel. Samuel Galton set out to improve his holding, and the project wa ...
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Moorland
Moorland or moor is a type of habitat found in upland areas in temperate grasslands, savannas, and shrublands and montane grasslands and shrublands biomes, characterised by low-growing vegetation on acidic soils. Moorland, nowadays, generally means uncultivated hill land (such as Dartmoor in South West England), but also includes low-lying wetlands (such as Sedgemoor, also South West England). It is closely related to heath, although experts disagree on what precisely distinguishes these types of vegetation. Generally, moor refers to highland and high rainfall zones, whereas heath refers to lowland zones which are more likely to be the result of human activity. Moorland habitats mostly occur in tropical Africa, northern and western Europe, and neotropical South America. Most of the world's moorlands are diverse ecosystems. In the extensive moorlands of the tropics, biodiversity can be extremely high. Moorland also bears a relationship to tundra (where the subsoil is permafros ...
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Peat
Peat (), also known as turf (), is an accumulation of partially decayed vegetation or organic matter. It is unique to natural areas called peatlands, bogs, mires, moors, or muskegs. The peatland ecosystem covers and is the most efficient carbon sink on the planet, because peatland plants capture carbon dioxide (CO2) naturally released from the peat, maintaining an equilibrium. In natural peatlands, the "annual rate of biomass production is greater than the rate of decomposition", but it takes "thousands of years for peatlands to develop the deposits of , which is the average depth of the boreal orthernpeatlands", which store around 415 gigatonnes (Gt) of carbon (about 46 times 2019 global CO2 emissions). Globally, peat stores up to 550 Gt of carbon, 42% of all soil carbon, which exceeds the carbon stored in all other vegetation types, including the world's forests, although it covers just 3% of the land's surface. ''Sphagnum'' moss, also called peat moss, is one of th ...
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South Drain (river)
The South Drain flows in a generally north-westerly direction from Actis Tunnel to Gold Corner, where it moves on to the Huntspill River, in Somerset ( en, All The People of Somerset) , locator_map = , coordinates = , region = South West England , established_date = Ancient , established_by = , preceded_by = , origin = , lord_lieutenant_office =Lord Lieutenant of Somerset , lord_ ..., England. It flows through the Shapwick Heath Nature Reserve. It was constructed between 1802 and 1806 as a result of the 1801 Brue Drainage Act. References Rivers of Somerset Somerset Levels {{England-river-stub ...
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North Drain
The North Drain flows westerly from Hurn Sluice on the River Sheppey to the North Drain Pumping Station at the River Brue, in Somerset ( en, All The People of Somerset) , locator_map = , coordinates = , region = South West England , established_date = Ancient , established_by = , preceded_by = , origin = , lord_lieutenant_office =Lord Lieutenant of Somerset , lord_ ..., England. References Rivers of Somerset Somerset Levels {{England-river-stub ...
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East Huntspill
East Huntspill is a village and civil parish on the Huntspill Level, near Highbridge, Somerset, England. The civil parish includes Cote, Hackness and Bason Bridge. The parish of East Huntspill has a population of 1,146. History Huntspill was listed in the Domesday Book of 1086 as ''Honspil'', meaning 'Huna's creek' possibly from the Old English personal name ''Huna'' and from the Celtic ''pwll''. The parish of Huntspill was part of the Huntspill and Puriton Hundred. Three 18th century farmhouses in East Huntspill, Hackney, New Road and Phippins, have all been designated as Grade II listed buildings. In 1949 the civil parish of Huntspill was abolished and divided into Huntspill All Saints and West Huntspill along the line of the Bristol and Exeter Railway. The parish of Huntspill All Saints was renamed East Hunstspill in 1972. Governance The village falls within the Non-metropolitan district of Sedgemoor, which was formed on 1 April 1974 under the Local Government Act 1 ...
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