|
Cassington Canal
The Cassington Canal (also known as the Cassington Cut or the Evenlode Cut) was an early 19th-century canal near Eynsham, Oxfordshire. The canal was built by the 4th Duke of Marlborough to provide a link between the River Thames and Cassington Mill; it later provided alternative wharfage to that at Eynsham. The canal was in operation for less than 70 years, its use declining with the advent of rail transport. The canal's primary use was to connect the Duke's salt works with the network of canals, rivers, and other inland waterways, as well as connecting the Oxford Canal and the Thames and Severn Canal. History Built between 1800 and 1802, the canal initially provided an connection between Cassington Mill and the recently constructed Cassington– Eynsham road. An early mention of the canal was in 1800, where the canal was described as "made by and belonging to" the Duke of Marlborough, and that its purpose was to convey goods between Cassington Mill and a wharf. A wid ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eynsham
Eynsham is a village and civil parish in the West Oxfordshire district, in Oxfordshire, England, about north-west of Oxford and east of Witney. The 2011 Census recorded a parish population of 4,648. It was estimated at 5,087 in 2020. Etymology Eynsham's name is first attested in the ''Anglo-Saxon Chronicle'', which took its present form in the later ninth century, as ''Egonesham''. (The ''Chronicle'' portrays the settlement as one of four captured by a West Saxon named Cuthwulf in 571 CE following the Battle of Bedcanford. The historicity of the battle is, however, in doubt.) The name is thought to derive from the Old English personal name ''Ægen'', in its genitive form ''Ægenes'', combined with the word ("river-meadow"). Thus the name once meant "Ægen's river-meadow". History Eynsham grew up near the historically important ford of Swinford on the River Thames flood plain. Excavations have shown that the site was used in the Bronze Age (3000–300 BCE) for a rectilinea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palace Of Westminster
The Palace of Westminster is the meeting place of the Parliament of the United Kingdom and is located in London, England. It is commonly called the Houses of Parliament after the House of Commons and the House of Lords, the two legislative chambers which occupy the building. The palace is one of the centres of political life in the United Kingdom; "Westminster" has become a metonym for the UK Parliament and the British Government, and the Westminster system of government commemorates the name of the palace. The Elizabeth Tower of the palace, nicknamed Big Ben, is a landmark of London and the United Kingdom in general. The palace has been a Grade I listed building since 1970 and part of a UNESCO World Heritage Site since 1987. The building was originally constructed in the eleventh century as a royal palace and was the primary residence of the kings of England until 1512, when a fire destroyed the royal apartments. The monarch moved to the adjacent Palace of Whitehall, bu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taynton Limestone Formation
The Taynton LimestoneWeishampel, David B; et al. (2004). "Dinosaur distribution (Middle Jurassic, Europe)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 538–541. . is a geological Formation (geology), formation in Oxfordshire in the United Kingdom. It dates to the Middle Jurassic, mid-Bathonian stage.Benson, R.B.J. (2009). "An assessment of variability in theropod dinosaur remains from the Bathonian (Middle Jurassic) of Stonesfield and New Park Quarry, UK and taxonomic implications for ''Megalosaurus bucklandii'' and ''Iliosuchus incognitus''." ''Palaeontology'', It predominantly consists of Oolite, ooidal grainstone. The term "Stonesfield Slate" refers to slaty limestone horizons within the formation that during the 18th and 19th centuries were extensively quarried for use in roof tiling within the vicinity of Stonesfield, Oxfordshire. Previously these were thought to belong to the Shar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 canal lock, locks. From Midford an arm also ran via Writhlington to Radstock, with a tunnel at Wellow, Somerset, Wellow. A feature of the canal was Combe Hay Locks, 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 canal lock, locks. The Radstock arm was never commercially success ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 Navigability, 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, Somerset, Bath the waterway follows the natural course of the River Avon, Bristol, River Avon before the canal links it to the River Kennet at Newbury, Berkshire, Newbury, and from there to Reading, Berkshire, Reading on the River Thames. In all, the waterway incorporates 105 Lock (water transport), 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wilts And Berks Canal
The Wilts & Berks Canal is a canal in the historic counties of Wiltshire and Berkshire, England, linking the Kennet and Avon Canal at Semington near Melksham, to the River Thames at Abingdon. The North Wilts Canal merged with it to become a branch to the Thames and Severn Canal at Latton near Cricklade. Among professional trades boatmen, the canal was nicknamed the Ippey Cut, possibly short for Chippenham. The canal was opened in 1810, but abandoned in 1914 – a fate hastened by a breach at Stanley aqueduct in 1901. Much of the canal subsequently became unnavigable: many of the structures were deliberately damaged by army demolition exercises; parts of the route were filled in and in some cases built over. In 1977 the Wilts & Berks Canal Amenity Group was formed with a view to full restoration of the canal. Several locks and bridges have since been restored, and over of the canal have been rewatered. Name The official name of the canal is the "Wilts & Berks Canal" a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thames And Severn Canal
The Thames and Severn Canal is a canal in Gloucestershire in the south-west of England, which was completed in 1789. It was conceived as part of a cargo route from Bristol and the Midlands to London, linking England's two largest rivers for better trade. The route climbs the steep Cotswold escarpment through the Golden Valley, tunnels underneath the summit of the Cotswold Edge, and emerges near the source of the Thames. At its eastern end, it connects to the top of the navigable Thames at Inglesham Lock near Lechlade, while at its western end, it connects to the Stroudwater Navigation at Wallbridge near Stroud, and thence to the River Severn. It had one short arm (branch), from Siddington to the town of Cirencester. It includes Sapperton Tunnel, which when built was the longest canal tunnel in Britain, and remains the second-longest complete tunnel. There were always problems with water supply, as no reservoirs were built, while the summit section near the tunnel ran throu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Somerset Coalfield
The Somerset Coalfield in northern Somerset, England is an area where coal was mined from the 15th century until 1973. It is part of a larger coalfield which stretched into southern Gloucestershire. The Somerset coalfield stretched from Cromhall in the north to the Mendip Hills in the south, and from Bath in the east to Nailsea in the west, a total area of about . Most of the pits on the coalfield were concentrated in the Cam Brook, Wellow Brook and Nettlebridge Valleys and around Radstock and Farrington Gurney. The pits were grouped geographically, with clusters of pits close together working the same coal seams often under the same ownership. Many pits shared the trackways and tramways which connected them to the Somerset Coal Canal or railways for distribution. The early pits were adits where coal outcropped or bell pits where coal was close to the surface. These methods were abandoned when deep seams were mined. The deepest shaft on the coalfield was at the Strap ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waterways In The United Kingdom
Water transport played a vital role in the UK's industrial development. The beginning of the 19th century saw a move from roads to waterways, (i.e. canals, rivers, firths, and estuaries). Rivers in the United Kingdom Major navigable rivers include the Humber, Mersey, Yorkshire Ouse, Severn, Thames and Trent. Some minor navigable rivers may be classified as canals. Others include the Warwickshire Avon, the Bristol Avon. There are also the subterranean rivers of London, and the Jubilee River, which, although man-made, was designed to look and act like a natural river rather than a canal. Canals in the United Kingdom The canals of the United Kingdom are a major part of the network of inland waterways. They are used for irrigation and transport and were a key part of the Industrial Revolution. Today, they are also used for recreational boating. Statistics See also * British Waterways Waterscape *Canal & River Trust The Canal & River Trust (CRT), branded a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lime Kiln
A lime kiln is a kiln used for the calcination of limestone (calcium carbonate) to produce the form of lime called ''quicklime'' (calcium oxide). The chemical equation for this reaction is: CaCO3 + heat → CaO + CO2 This reaction can take place at anywhere above , but is generally considered to occur at (at which temperature the partial pressure of CO2 is 1 atmosphere), but a temperature around (at which temperature the partial pressure of CO2 is 3.8 atmospheres) is usually used to make the reaction proceed quickly.Parkes, G.D. and Mellor, J.W. (1939). ''Mellor's Modern Inorganic Chemistry'' London: Longmans, Green and Co. Excessive temperature is avoided because it produces unreactive, "dead-burned" lime. Slaked lime (calcium hydroxide) can be formed by mixing quicklime with water. History Pre-pottery Neolithic In plaster, proto-pottery, and mortar Because it is so readily made by heating limestone, lime must have been known from the earliest times, and all th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
