The Manchester Coalfield is part of the South Lancashire Coalfield, the coal seams of which were laid down in the Carboniferous Period. Some easily accessible seams were worked on a small scale from the Middle Ages, and extensively from the beginning of the Industrial Revolution in the early 19th century until the last quarter of the 20th century. The Coal Measures lie above a bed of Millstone Grit and are interspersed with sandstones, mudstones, shales, and fireclays. The Lower Coal Measures occupy the high ground of the West Pennine Moors above Bolton and are not worked in the Manchester Coalfield. [1] The most productive of the coal measures are the lower two thirds of the Middle Coal Measures where coal is mined from seams between the Worsley Four Foot and Arley mines. The deepest and most productive collieries were to the south of the coalfield. The coalfield is affected by the northwest to southeast aligned Pendleton Fault along the Irwell Valley and the Rossendale Valley anticline. The Coal Measures generally dip towards the south and west. Numerous other smaller faults affect the coalfield. [2] The Upper Coal Measures are not worked in the Manchester Coalfield.
The early coal pits were dug to the shallow seams where they outcropped, particularly in the Irwell Valley and in Atherton. The early collieries were adits or bell pits exploiting the Worsley Four Foot Mine. Deeper mines were sunk when steam engines were developed to pump water from the shafts. Most collieries to the east of the Pendleton Fault had closed before 1929. A group of independent companies formed Manchester Collieries in 1929, to work the reserves of the coalfield.
In this part of Lancashire a coal seam is referred to as a mine and the coal mine is a colliery or pit. The beds of coal in the Coal Measures are separated by layers of gritstones, sandstones, shales and mudstones of varying thicknesses. The mines were frequently named after their thickness – Yard, Three Quarters – or given local names in the areas in which they were first worked.
Seam | Alternative names [3] | Description |
---|---|---|
Worsley Four Foot mine | Pendleton Four Foot, Parker mine in central Manchester | As the shallowest coal seam west of the Pendleton Fault, it was exploited from the early days of mining from bell pits and was accessed at the Delph at Worsley by the Worsley Navigable Levels. It is from 3 feet (0.91 m) to 4 feet (1.2 m) in thickness and was used as steam coal. The mine was wet due to the permeable sandstone above it. [4] It was worked westwards from Worsley to Bedford Colliery. [5] This coal seam is known as the Parker mine in the central coalfield under Manchester where a series of coal seams, the Bradford Group, was worked above it. [6] |
Bin mine | Top Five Quarters (Radcliffe) | The Bin Mine has a maximum height of 3 feet 9 inches (1.14 m); its coal was mainly used by industry. [4] Above the Bin mine the sandstones contain a layer of ironstone. [7] |
Crombouke Mine | Crumbouke, Shuttle (Pendlebury), Albert (Pendleton), Top Yard (Radcliffe) Roger mine (central Manchester) | The Crombouke is a seam from 2 feet 6 inches to 4 feet 6 inches of good quality coal in the west and corresponds to the Roger mine in central Manchester. [3] The Crombouke mine at Worsley thins out and is known as the Albert at Pendleton, The Crombouke mine at Pendleton is found below the Albert. [8] |
Brassey mine | Brassey Bottoms, Little (Newtown) | The Brassey mine is thickest around Tyldesley at 4 feet (1.2 m) thick. [4] |
Rams mine | Seven Foot (Walkden), Six Foot (Tyldesley) | The Rams mine has a minimum thickness of 4 feet (1.2 m) and average thickness of 6 feet (1.8 m) west of the fault. To the east it is up to 9 feet (2.7 m) in thickness. The high quality coal was mined to considerable depths under Pendlebury and Salford. [4] At Atherton it formed good quality steam coal. [8] |
Black and White mine | Seven Foot (Tyldesley), Gingham mine (Black mine), Ten Foot (White mine) in (Bolton and Little Lever, east of fault), Great mine in Atherton | The Black and White mine is a double seam with 7 feet 5 inches (2.26 m) of workable coal. Top coal is the White mine and bottom coal is the Black mine. [9] It outcrops at the south east corner of Hulton Park and in Little Hulton [10] and across Gibfield and Chowbent in Atherton where it was mined in shallow ladder pits or drifts. [11] The seam measured 7 feet 10 inches (2.39 m) in Atherton town centre. [12] |
Doe mine | Dow, Yard (Tyldesley) | The Doe mine has two coals separated by a dirt parting. At Newtown the seam was liable to spontaneous combustion. The lower coals of this mine were worked around Tyldesley as the Yard mine, near Bolton the top coal was worked as the Bancroft mine. [13] The seam outcrops on either side of the River Irwell at Clifton where the seam was worked at the Ladyshore Colliery. [14] |
Five Quarters mine | Yard (Atherton) | This seam was worked extensively east of the Irwell Valley Fault around Radcliffe. The seam was split by a dirt band and the coal was used as steam and household coal. [13] |
Hell hole mine | Victoria, Foor Foot (Atherton) | This coal seam varies in thickness between 2 feet 6 inches (0.76 m) and 4 feet (1.2 m) and the coal was used for coking and gas making and household use. [13] |
Trencherbone mine | The Trencherbone mine was extensively worked throughout the coalfield and reputedly produced the best coal. It outcropped at Stoneclough in the Irwell Valley. [14] It had a thickness of 3 feet (0.91 m) to 4 feet (1.2 m) at Astley and Tyldesley and up to 8 feet (2.4 m) elsewhere. [15] The seam outcropped between Schofield Lane and Bag Lane in Atherton. [11] | |
Cannel mine | King and Cannel | The Cannel mine was on average less than one foot thick. Cannel coal burns easily with a bright light and leaves little ash. This was the lowest coal seam worked east of the Irwell Valley. Cannel was used to make coal gas. [15] |
Sapling mine | The Sapling mine is thickest in the west but reduces to 9 inches. The coal is poor quality but where mined was used for industrial steam raising. [16] | |
Plodder mine | Ravine (Atherton) | The Plodder mine contains seams of fireclay and shales. The coal seam was 2 feet 8 inches but thicker at Newtown. It was contaminated with iron pyrites. At Sandhole Colliery the seam was liable to spontaneously combust. It was poor quality but used as steam coal. [16] |
Yard mine | Haigh Yard | The Haigh Yard seam had a height of 5 feet (1.5 m) at Tyldesley. The coal seam was divided by a dirt parting of sandstone. [16] |
Half Yard mine | Bone | This is a thin seam of coking coal with a maximum height of 20 inches. [16] |
Three Quarters mine | Smith | The Three Quarters mine had a maximum height of 2 feet (0.61 m) and was worked, where the thickness of the seam allowed, to produce coking coal. [16] It was worked at Chew Moor, Deane Moor and Farnworth. [17] |
Arley mine | Dogshaw (Bury), Daubhill (Bolton) | The Arley mine is the deepest of the seams of the Middle Coal Measures. It outcropped at Red Moss near Blackrod where it was 2 feet (0.61 m) thick, and at Chew Moor, Westhoughton and Daubhill, Bolton. [17] Its average thickness was 3 feet (0.91 m) to 4 feet (1.2 m). It produced excellent quality coal for coking, house and steam coal. The Arley mine was worked throughout the coalfield and around Tyldesley was a hot mine. [16] |
The eastern part of the coalfield under Manchester is isolated from the rest. The sequence of coal seams corresponds more closely with that of the Oldham Coalfield than the rest of the Manchester Coalfield. Workable seams are close to the surface and coal from the deep Roger mine was considered to be of the highest quality. The Upper Coal Measures above the Worsley Four Foot mine, known as the Parker mine, are worked in this part of the coalfield and known as the Bradford Group, above which is the Ardwick Group. [6]
The coal seams of the Bradford Group are the Two Foot, Doctor, New, Yard, Bradford Foor Foot, Three Quarters and Charlotte mines, the Charlotte being closest to the surface. The Openshaw mine above the Charlotte was worked for fireclay. Below the Bradford Group and the Parker mine are the Top, Middle and Deep mines and 60 feet (18 m) below them, the Roger mine. The Top, Middle and Deep mines correspond to the Major, Bland and Ashton Great mines in the Oldham Coalfield. The Crumbouke mine in the western coalfield is the Roger mine in central Manchester. [18]
Wet Earth Colliery was a coal mine located on the Manchester Coalfield, in Clifton, Greater Manchester. The colliery site is now the location of Clifton Country Park. The colliery has a unique place in British coal mining history; apart from being one of the earliest pits in the country, it is the place where engineer James Brindley made water run uphill.
The Worsley Navigable Levels are an extensive series of coal mines in Worsley in the City of Salford in Greater Manchester, England. They were worked largely by the use of underground canals and boats called starvationers.
The South Yorkshire Coalfield is so named from its position within Yorkshire. It covers most of South Yorkshire, West Yorkshire and a small part of North Yorkshire. The exposed coalfield outcrops in the Pennine foothills and dips under Permian rocks in the east. Its most famous coal seam is the Barnsley Bed. Coal has been mined from shallow seams and outcrops since medieval times and possibly earlier.
The North Staffordshire Coalfield was a coalfield in Staffordshire, England, with an area of nearly 100 square miles (260 km2), virtually all of it within the city of Stoke on Trent and the borough of Newcastle-under-Lyme, apart from three smaller coalfields, Shaffalong and Goldsitch Moss Coalfields near Leek and the Cheadle Coalfield. Coal mining in North Staffordshire began early in the 13th century, but the industry grew during the Industrial Revolution when coal mined in North Staffordshire was used in the local Potteries ceramics and iron industry.
The Cheadle Coalfield is a coalfield in the United Kingdom. Centred on the town of Cheadle, Staffordshire and its outlying villages it lies to the east of Stoke-on-Trent and the much larger North Staffordshire Coalfield. The area has been mined for many years, with documentary evidence from Croxden Abbey citing coal mining in the 13th century.
The Lancashire Coalfield in North West England was an important British coalfield. Its coal seams were formed from the vegetation of tropical swampy forests in the Carboniferous period over 300 million years ago.
The Ingleton Coalfield is in North Yorkshire, close to its border with Lancashire in north-west England. Isolated from other coal-producing areas, it is one of the smallest coalfields in Great Britain.
The Coalbrookdale Coalfield is a coalfield in Shropshire in the English Midlands. It extends from Broseley in the south, northwards to the Boundary Fault which runs northeastwards from the vicinity of The Wrekin past Lilleshall. The former coalfield has been built on by the new town of Telford.
The Astley and Tyldesley Collieries Company formed in 1900 owned coal mines on the Lancashire Coalfield south of the railway in Astley and Tyldesley, then in the historic county of Lancashire, England. The company became part of Manchester Collieries in 1929 and some of its collieries were nationalised in 1947.
Bedford Colliery, also known as Wood End Pit, was a coal mine on the Manchester Coalfield in Bedford, Leigh, Lancashire, England. The colliery was owned by John Speakman, who started sinking two shafts on land at Wood End Farm in the northeast part of Bedford, south of the London and North Western Railway's Tyldesley Loopline in about 1874. Speakman's father owned Priestners, Bankfield, and Broadoak collieries in Westleigh. Bedford Colliery remained in the possession of the Speakman family until it was amalgamated with Manchester Collieries in 1929.
The Denbighshire Coalfield in the historic county of Denbighshire in north-east Wales is one of the smaller British coalfields. It extends from near Caergwrle in the north, southwards through Wrexham, Ruabon and Rhosllannerchrugog to Chirk in the south. A small part extends into Shropshire around Oswestry. Beyond Caergwrle the coal-bearing strata continue northwards as the Flintshire Coalfield. Together the two coalfields are known as the North Wales Coalfield.
Bridgewater Collieries originated from the coal mines on the Manchester Coalfield in Worsley in the historic county of Lancashire owned by Francis Egerton, 3rd Duke of Bridgewater in the second half of the 18th century. After the Duke's death in 1803 his estate was managed by the Bridgewater Trustees until the 3rd Earl of Ellesmere inherited the estates in 1903. Bridgewater Collieries was formed in 1921 by the 4th Earl. The company merged with other prominent mining companies to form Manchester Collieries in 1929.
Astley Green Colliery was a coal mine in Astley, Greater Manchester, then in the historic county of Lancashire, England. It was the last colliery to be sunk in Astley. Sinking commenced in 1908 by the Pilkington Colliery Company, a subsidiary of the Clifton and Kersley Coal Company, at the southern edge of the Manchester Coalfield, working the Middle Coal Measures where they dipped under the Permian age rocks under Chat Moss. The colliery was north of the Bridgewater Canal. In 1929 it became part of Manchester Collieries, and in 1947 was nationalised and integrated into the National Coal Board. It closed in 1970, and is now Astley Green Colliery Museum.
Chanters Colliery was a coal mine which was part of the Fletcher, Burrows and Company's collieries at Hindsford in Atherton, Greater Manchester, then in the historic county of Lancashire, England.
Cleworth Hall Colliery was a coal mine operating on the Manchester Coalfield after 1874 in Tyldesley, Greater Manchester, then in the historic county of Lancashire, England.
Bradford Colliery was a coal mine in Bradford, Manchester, England. Although part of the Manchester Coalfield, the seams of the Bradford Coalfield correspond more closely to those of the Oldham Coalfield. The Bradford Coalfield is crossed by a number of fault lines, principally the Bradford Fault, which was reactivated by mining activity in the mid-1960s.
The Pendleton Fault, sometimes called the Irwell Valley Fault, stretches for about 20 miles (32 km) from Bolton in Greater Manchester along the Irwell Valley through Pendleton to Poynton in Cheshire, running northwest–southeast. The fault throws the beds of the Middle Coal Measures of the Manchester Coalfield by 1,000 feet (300 m) on its western side. The fault is active, and movement has caused earthquakes. An earthquake of intensity 6 on the Richter scale that occurred on 10 February 1889 was felt over an area of 2,500 square miles (6,500 km2). Lesser shocks were recorded in the early 20th century, in 1931 and 1944. Coal mining in the Irwell Valley between Bolton and Pendleton may account for small movements, although all mines in the area closed in 1929 and no coal has been mined since.
The Oldham Coalfield is the most easterly part of the South Lancashire Coalfield. Its coal seams were laid down in the Carboniferous period and some easily accessible seams were worked on a small scale from the Middle Ages and extensively from the beginning of the Industrial Revolution in the early 19th century until the middle of the 20th century.
The geology of Merseyside in northwest England largely consists of a faulted sequence of Carboniferous Coal Measures rocks overlain in the west by younger Triassic and Permian age sandstones and mudstones. Glaciation during the present Quaternary Period has left widespread glacial till as well as erosional landforms. Other post-glacial superficial deposits such as river and estuarine alluvium, peat and blown sand are abundant.