Treeton Colliery
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Treeton Colliery
Treeton Colliery was a coal mine situated in the village of Treeton, near Rotherham, South Yorkshire, England. Work on the sinking of Treeton Colliery commenced, with all due ceremony, in October 1875. Trade, at the time, was in a poor state and the company was short of capital so work was suspended three years later not being resumed until March, 1882. The colliery was owned by the Rother Vale Collieries Limited which was founded in the same year, bringing together the new workings with collieries at Fence and Orgreave. This became part of the United Steel Companies Limited following the end of World War I. From its beginnings until 1965 Treeton worked the Barnsley seam and the High Hazels seam until the following year. After nationalisation it was decided to increase the output of the Wathwood seam and to reopen the Swallow Wood seam which had fallen into disuse in 1947. This came on stream in 1972 and lasted until the colliery closed on 7 December 1990. These two seams p ...
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Coal Mine
Coal mining is the process of extracting coal from the ground. Coal is valued for its energy content and since the 1880s has been widely used to generate electricity. Steel and cement industries use coal as a fuel for extraction of iron from iron ore and for cement production. In the United Kingdom and South Africa, a coal mine and its structures are a colliery, a coal mine is called a 'pit', and the above-ground structures are a 'pit head'. In Australia, "colliery" generally refers to an underground coal mine. Coal mining has had many developments in recent years, from the early days of men tunneling, digging and manually extracting the coal on carts to large open-cut and longwall mines. Mining at this scale requires the use of draglines, trucks, conveyors, hydraulic jacks and shearers. The coal mining industry has a long history of significant negative environmental impacts on local ecosystems, health impacts on local communities and workers, and contributes heavily to th ...
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Swallow Wood Seam
The coal seams worked in the South Yorkshire Coalfield lie mainly in the middle coal measures within what is now formally referred to as the Pennine Coal Measures Group. These are a series of mudstones, shales, sandstones, and coal seams laid down towards the end of the Carboniferous period between about 320 and 300 million years ago. The total depth of the strata is about . The list of coal seams that follows starts at the shallowest seam and proceeds downwards with the outcrops occurring progressively further west until the deepest coal seam, the Silkstone Seam which outcropped at the western edge of the coalfield. The thicknesses and depths of each seam are not given as they vary across the coalfield. Seams Sources * * Further reading * * External links Yorkshire Coalfield Geology- with depths of the seams at Kiveton, and a map showing the depth of the Barnsley Seam across the coalfield; see also depths of the seams at Dinningtonbr>and Thurcroft Thurcroft ...
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Coal Mines In Rotherham
Coal is a combustible black or brownish-black sedimentary rock, formed as rock strata called coal seams. Coal is mostly carbon with variable amounts of other elements, chiefly hydrogen, sulfur, oxygen, and nitrogen. Coal is formed when dead plant matter decays into peat and is converted into coal by the heat and pressure of deep burial over millions of years. Vast deposits of coal originate in former wetlands called coal forests that covered much of the Earth's tropical land areas during the late Carboniferous ( Pennsylvanian) and Permian times. Many significant coal deposits are younger than this and originate from the Mesozoic and Cenozoic eras. Coal is used primarily as a fuel. While coal has been known and used for thousands of years, its usage was limited until the Industrial Revolution. With the invention of the steam engine, coal consumption increased. In 2020, coal supplied about a quarter of the world's primary energy and over a third of its electricity. Some ...
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Orgreave Paddy Mail Accident
The Orgreave Train Collision occurred on 13 December 1926 near Orgreave Colliery signal box on the Great Central Railway line about east of Sheffield. A goods train had collided with a preceding goods train on the same line, and the wreckage had obstructed the adjacent passenger line. A workmen's train, known as a paddy mail, ran into the wreckage; paddy mails were workmen's trains operated in connection with all three shift changes at the collieries. These were hauled from Sheffield Victoria, as far as Orgreaves Colliery Sidings by the main line company, using whatever locomotive was available. At this point the colliery's own locomotives took over and in connection with this operation 'Rothervale No.6' was fitted with vacuum brakes. The train then ran to Orgreave Colliery platform and Treeton Colliery. Circumstances The line at Orgreaves CollieryThe signal box was named ''Orgreaves Colliery'', with an 's' being added to the name, in error, however the railway company never ...
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Darnall Railway Station
Darnall railway station is on the Sheffield to Lincoln Line and was built in 1849 to serve Darnall, a community about from the centre of Sheffield, South Yorkshire, England, and which later became a suburb of the city. As of March 2020, Darnall is the least used railway station in the county of South Yorkshire. History The station was built by the Manchester, Sheffield and Lincolnshire Railway (M.S.& L.R.) with two platforms flanking the main lines. The main station building, on the Cleethorpes-bound side, contained the usual facilities, and was situated at the top of Station Road; a waiting shelter on the Sheffield-bound platform gave passengers some comfort. Widening took place in the area just before the First World War and two goods lines were laid around the back of the platforms. This was to increase capacity of the line and aid the movement of coal traffic towards Immingham Docks, opened in 1912. This work required the removal of Darnall tunnel about to the east of th ...
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Sheffield Victoria Railway Station
Sheffield Victoria was the main railway station in Sheffield, Yorkshire, England, on the Great Central Railway, between Chesterfield and Penistone. History Early history Engineered by Joseph Locke, the Sheffield, Ashton-under-Lyne and Manchester Railway linking Manchester and Sheffield opened in 1845. Originally, this line terminated at the Bridgehouses station, which was about to the west of the future Victoria station. In 1847, the Sheffield, Ashton-under-Lyne and Manchester Railway merged with two other railway companies to form the Manchester, Sheffield and Lincolnshire Railway. The station at Bridgehouses had been outgrown, so an extension and new station were planned. John Fowler, who later gained fame for co-designing the Forth Railway Bridge in Scotland, was employed to engineer the extension and station. Fowler's design included a viaduct over the Wicker that was high, long and two island platforms long. The extension was completed in 1847–1848 and the new Vic ...
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Paddy Mails
Paddy mails, generally considered as being workmen's trains, were operated by, or for many companies to transport their workers to their place of work or between their sites of work. Originally they were operated by railway contractors, on temporary tracks laid to remove spoil from their workings, to transport workers from their "shanty villages" to the work site. Many of these navvies as they were known were of Irish origin, hence the name given to the trains (see: Paddy). Once the main line was built the name passed to the workmen's specials, which in many cases, were operated along the main line railways and sometimes operated by the main line companies to an exchange point where the trains were taken over by the industrial company. In a time before the provision of pit-head baths it was illegal to travel in a normal service train in working clothes, so special trains were provided, usually of the railway company's most ancient coaches. There is a preserved example of such ...
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Manchester, Sheffield And Lincolnshire Railway
The Manchester, Sheffield and Lincolnshire Railway (MS&LR) was formed in 1847 when the Sheffield, Ashton-under-Lyne and Manchester Railway joined with authorised but unbuilt railway companies, forming a proposed network from Manchester to Grimsby. It pursued a policy of expanding its area of influence, especially in reaching west to Liverpool, which it ultimately did through the medium of the Cheshire Lines Committee network in joint partnership with the Great Northern Railway and the Midland Railway. Its dominant traffic was minerals, chiefly coal, and the main market was in London and the south of England. It was dependent on other lines to convey traffic southward. The London and North Western Railway was an exceptionally hostile partner, and in later years the MS&LR allied itself with the Great Northern Railway. Passenger traffic, especially around Manchester, was also an important business area, and well-patronised express trains to London were run in collaboration with th ...
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North Midland Railway
The North Midland Railway was a British railway company, which opened its line from Derby to Rotherham (Masbrough) and Leeds in 1840. At Derby, it connected with the Birmingham and Derby Junction Railway and the Midland Counties Railway at what became known as the Tri-Junct Station. In 1844, the three companies merged to form the Midland Railway. Origin The East Midlands had for some years been at the centre of plans to link the major cities throughout the country. In Yorkshire, George Hudson was the Chairman of the York and North Midland Railway, a proposed line from York towards the industrial markets of Manchester and Liverpool. The new line would connect it, and the Manchester and Leeds Railway as part of a trunk route from the South and London to Yorkshire and the North East of England. Meanwhile, financiers in Birmingham, were looking to expand their system northwards. George Carr Glyn was the first Chairman of the new company, with George Stephenson appointed as engi ...
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Wathwood Seam
The coal seams worked in the South Yorkshire Coalfield lie mainly in the middle coal measures within what is now formally referred to as the Pennine Coal Measures Group. These are a series of mudstones, shales, sandstones, and coal seams laid down towards the end of the Carboniferous period between about 320 and 300 million years ago. The total depth of the strata is about . The list of coal seams that follows starts at the shallowest seam and proceeds downwards with the outcrops occurring progressively further west until the deepest coal seam, the Silkstone Seam which outcropped at the western edge of the coalfield. The thicknesses and depths of each seam are not given as they vary across the coalfield. Seams Sources * * Further reading * * External links Yorkshire Coalfield Geology- with depths of the seams at Kiveton, and a map showing the depth of the Barnsley Seam across the coalfield; see also depths of the seams at Dinningtonbr>and Thurcroft Thurcroft is ...
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Treeton
Treeton is a village and civil parish of the Metropolitan Borough of Rotherham in South Yorkshire, England. It is located about south of the town of Rotherham and east of Sheffield City Centre. History There is evidence of Mesolithic and Neolithic settlement in this area. In 1954 a Neolithic polished stone axe was found at Gregory Hill Field, and in 1957 Mesolithic flint cores were found in Treeton Wood. There was a Roman fort at Templeborough, about north west of Treeton, and remnants of the Roman road called Icknield Street (sometimes Ryknild or Riknild Street) have been found in nearby Brinsworth. The name ''Treeton'' is Old English in origin and may mean 'tree farmstead' or 'farmstead built with posts'. The earliest known written record of Treeton is the ''Domesday book'' of 1086, in which it is referred to as ''Trectone'' or ''Tretone''. The ''Domesday Book'' also mentions that the village had two mills and a church. The present parish church the Church of St Helen wa ...
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High Hazels Seam
The coal seams worked in the South Yorkshire Coalfield lie mainly in the middle coal measures within what is now formally referred to as the Pennine Coal Measures Group. These are a series of mudstones, shales, sandstones, and coal seams laid down towards the end of the Carboniferous period between about 320 and 300 million years ago. The total depth of the strata is about . The list of coal seams that follows starts at the shallowest seam and proceeds downwards with the outcrops occurring progressively further west until the deepest coal seam, the Silkstone Seam which outcropped at the western edge of the coalfield. The thicknesses and depths of each seam are not given as they vary across the coalfield. Seams Sources * * Further reading * * External links Yorkshire Coalfield Geology- with depths of the seams at Kiveton, and a map showing the depth of the Barnsley Seam across the coalfield; see also depths of the seams at Dinningtonbr>and Thurcroft Thurcroft is ...
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