Niceic Electrician Dukinfield

 

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Local Niceic electricians in Dukinfield.

Niceic electrician Dukinfield are your local Niceic electricians, we can cover all your reports and paperwork. We can also carry out electrical maintenance to existing buildings, this includes Niceic inspection & testing (periodic inspection reports). Niceic electricians Dukinfield will carry out an electrical survey, known as a periodic inspection report (PIR) which will reveal if electrical circuits are overloaded, find potential hazards in the installation, identify defective work, highlight any lack of earthling or bonding and carry out tests on the fixed wiring of the installation. The report will establish the overall condition of all the electrics and state whether it is satisfactory for continued use, and should detail any work that might need to be done.

Niceic electrician Dukinfield offer discounted rates for o,a,p .

Niceic electrician Dukinfield, Manchester Electrician Ltd carry out all work to the highest standards, to each individual customers requirements and at highly competitive and affordable rates.

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Niceic electrician Dukinfield deliver prompt service at reasonable rates, 24 hours daily.

Our Niceic electrician Dukinfield have 30 years experience in the Dukinfield area.

We have more than 30 years experience as professional and reputable Niceic electricians in and around Dukinfield and the greater manchester areas, Niceic electrician Dukinfield have also generated an envious reputation due to the quality of our work, coupled with our at highly competitive and affordable rates.

 

Manchester Electrician Dukinfield - Services.

Niceic electrician Dukinfield services range from temporary distribution for construction sites, 110 volt power & lighting installation, inspection & testing, periodic inspection reports as listed below.

 

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Niceic electrician Dukinfield commercial installations

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Niceic electrician Dukinfield cctv systems

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Niceic mains distribution 400-230v Dukinfield,

 

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Niceic power distribution 400v & 230v Dukinfield,

 

Niceic electrician Dukinfield cable management systems

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Niceic electrician Dukinfield lighting systems and controls

Niceic lighting systems and controls Dukinfield,

 

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Niceic electrician Dukinfield More information

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Dukinfield - Geography & history

Population 18,885 (2001 Census)
OS grid reference SJ945975 - London 160 mi (257 km) SSE
Metropolitan borough Tameside
Metropolitan county Greater Manchester
Region North West
Country England
Sovereign state United Kingdom
Post town DUKINFIELD
Postcode district SK16
Dialling code 0161
Police Greater Manchester
Fire Greater Manchester
Ambulance North West
EU Parliament North West England
UK Parliament Denton and Reddish

 

Dukinfield is a small town within the Metropolitan Borough of Tameside, in Greater Manchester, England. It lies in central Tameside on the south bank of the River Tame, opposite Ashton-under-Lyne, and is 6.3 miles (10.1 km) east of the city of Manchester. At the time of the 2001 census it had a population of 18,885.

Historically a part of Cheshire, the town is a product of the Industrial Revolution when its development was accelerated by the growth of coal mining and the cotton industry

 

History

The earliest evidence of human activity around Dukinfield comes from a collection of four flints from the late Neolithic/early Bronze Age. The artefacts were discovered on the site of Dukinfield Hall and has been taken as evidence of a prehistoric settlement on the site. There is no further evidence of activity in the area until the Roman period. A 3rd-century bronze Roman coin, from the reign of Emperor Tetricus I was discovered in the town.

 

Dukinfield means "open land of the ducks" and derives from the Old English duce and feld. After the Norman conquest of England the area became part of two Norman estates and in the 12th century the presiding family took the name "De Dokenfeld".

 

During the English Civil War, Colonel Robert Duckenfield of Dukinfield Hall was a noted commander in the New Model Army. His son was a Dukinfield Baronet in 1665.

 

Industrialisation - particularly the cotton trade - helped shape the town, but its rapid development destroyed its former pasture and meadow land. Most of the cotton mills have now been demolished, but some have been preserved and have been converted into apartments.

 

Coal pits were also a major part of Dukinfield's industrial history, one pithead was located on Birch Lane, now the site of All Saints' Catholic College, with another near the northern border with Ashton-under-Lyne. One, the Astley Deep pit mine, was just off King's Street opposite the bottom of Brownlea Avenue. This mine was reported to be the deepest coal mine in the world, at 2100 feet (640 metres) and had three main shafts. These shafts were filled in and left to stand for many years before being built on. It is now the site of a development of houses comprising Angel Close, Oval Drive & Silver Close.

On 14 April 1874, a large underground gas explosion occurred in the Astley Deep Pit coal mine, known locally as Astley Deep Pit Disaster. 54 men were killed.

 

There are four major historical characters in Dukinfield's history - Robert Duckenfield, John Astley, Samuel Robinson and Daniel Adamson.

 

John Astley, born in 1724 was a coal, iron and cotton industrialist who built Dukinfield Lodge.

Robinson, who was a Unitarian, industrialist and scholar founded the village library in 1833 and was dubbed the "foremost promoter of education in the district" before his death in 1884.

 

Adamson was a mechanical engineer who also became the first chairman of the world-renowned Manchester Ship Canal Company. He died on 13 January 1890. The Adamson Military Band, (which received support from Daniel Adamson and is named after him) set up for the workers, is based in Dukinfield.

 

Dukinfield and its surrounding towns were major centres of civil revolt during the Nineteenth Century and briefly the area was a hotbed of Chartism, the popular movement calling for universal suffrage via a "People's Charter". The famous Chartist leader Reverend Joseph Rayner Stephens is buried in St John's Church cemetery in the town.

 

Dukinfield Geography

At 53°28′40.14″N 02°05′33.3″W / 53.4778167°N 2.092583°W / 53.4778167; -2.092583 (53.477818° -2.092584°), and 159 miles (256 km) north-northwest of London, Dukinfield's borders are defined to the north and west by the River Tame.

 

The town is situated at the edge of the Cheshire Plain where it meets the Pennines, and Dukinfield is the first town on the hill. The park is situated approximately a quarter of a mile from the Town Hall along King Street towards Longdendale in the South. Because of the quite steep rise out of the plain, the park is terraced and is over 90 feet higher at the top. The hill flattens out slightly before rising steeply again towards the East, where the library is situated. The Town Hall is also at the base of the same hill with Astley Street rising steeply along its shorter Southern side before climbing some 120 feet to the crest of the ridge.

 

There are coal measures around the town, which run north–south through Tameside. The local soil is mainly clayey with some alluvial deposits. The reason for Dukinfield having so many mines in such a small area is simply that the hill that these buildings are on is a folded granite, dropping down at a steep angle into the earth where it meets the plain. This gives a definite end of the plain in Dukinfield, and as such it is the ancient side of a vast lake or swamp that would have run out from the park and Town Hall through Dukinfield and into Manchester itself.

 

This ancient lake is the reason coal is found in the area. The layers of shale and coal are laid on top of each other in quite thin bands, only 20 or 30 feet thick, but they are folded in such a way as to allow the miners to track the coal seams quite easily downwards. The coal deposits fall away at a 20 degree or so angle, and runs some 8 or 9 miles from the base of the hill out under the plain. The coal deposits are known as the Dukinfield Marine Band and form a V shape running out from here towards Stockport in the South and Ashton Moss in the North East. Because there are so many folds coming to this point, Dukinfield had at least three mines of which Astley Deep Pit had the best coal. There are many types of coal found here, but Dukinfield coal was of extremely good quality and was known to be the best for heating and steam generation. Only a mile to the south along Longdendale road is another large mine, the Dewsnap Colliery, which was of a lower quality and so was not in as much demand. The Dukinfield Marine Band rises out of the earth at Dukinfield, and continues up the hill towards the top of the ridge, some 140 feet above the level of the plain where it flattens out for a while, and it is here that the third mine was situated. Because Astley Deep and Dewsnap Colliery are at the base of the Hill, their advantage is prodigious.

 

Dukinfield Geography

At 53°29′38″N 2°6′11″W / 53.49389°N 2.10306°W / 53.49389; -2.10306 (53.4941°, −2.1032°), and 160 miles (257 km) north-northwest of London, Dukinfield stands on the north bank of the River Tame, about 35 feet (11 m) above the river. Described in Samuel Lewis's A Topographical Dictionary of England (1848) as situated on "on a gentle declivity", Dukinfield lies on undulating ground by the Pennines, reaching a maximum elevation of about 1,000 feet (305 m) above sea level. It is 6.2 miles (10.0 km) east of Manchester city centre, and is bound on all sides by other towns: Dukinfield, Droylsden, Dukinfield, Mossley, Oldham and Stalybridge, with little or no green space between them. Ashton experiences a temperate maritime climate, like much of the British Isles, with relatively cool summers and mild winters.

Dukinfield and neighbouring Oldham viewed from Werneth LowGenerally the bedrock of the west of the town consists of coal measures, which were exploited by the coal mining industry, while the east is mainly millstone grit. Overlying the bedrock are deposits of glacial sand and gravel, clay, and some alluvial deposits. Ashton Moss, a peat bog, lies to the west of the town and was originally much larger. The River Tame forms part of the southern boundary, dividing the town from Stalybridge and Dukinfield, and the River Medlock runs to the west. The Peak Forest Canal terminates at Dukinfield Junction on the Ashton Canal, which passes through the town.

 

Ashton's built environment is similar to the urban structure of most towns in England, consisting of residential dwellings centred around a market square and high street in the town centre, which is the local centre of commerce. There is a mixture of low-density urban areas, suburbs, semi-rural and rural locations in Dukinfield, but overwhelmingly the land use in the town is residential; industrial areas and terraced houses give way to suburbs and rural greenery as the land rises out of the town in the east. The older streets are narrow and irregular, but those built more recently are spacious, lined by "substantial and handsome houses". Areas and suburbs of Dukinfield include Ashton Moss, Cockbrook, Hartshead, Hazelhurst, Heys, Hurst, Limehurst, Luzley, Park Bridge, Ryecroft, Taunton, and Waterloo.

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