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South Yorkshire Coalfield

Coalfield in Yorkshire, England

  • 11 min read
  • 5 chapters

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Geography and geology

The coalfield stretches from Halifax in the north west, to the north of Bradford and Leeds in the north east, Huddersfield and Sheffield in the west, and Doncaster in the east. The major towns of Wakefield, Barnsley and Rotherham are within its boundaries. It is part of the larger Nottinghamshire, Derbyshire and Yorkshire Coalfield. Its western boundary is defined by the outcropping of coal seams in the foothills of the Pennines and in the east by the descent of the coal-bearing strata under overlying rocks as they approach the North Sea. Since the creation of the county of South Yorkshire in 1974, the name can be misleading as the coalfield stretches beyond the Wakefield district and other parts of West Yorkshire as far as Keighley and Kellingley Colliery and the Selby Coalfield are in North Yorkshire. It is separate from the Ingleton Coalfield in North Yorkshire, and a small number of mines around Todmorden are part of the Lancashire Coalfield.

The coal bearing rock strata or coal measures that make up the coalfield outcrop in the foothills of the Pennines and dip gently downwards from west to east. This area is known as the exposed coalfield. The coal measures are Carboniferous rocks deposited between 290 and 354 million years ago. West and east of Doncaster the coal measures are overlain by younger rocks, Permian limestone, where the area is referred to as the concealed coal field.

The northernmost extent of the South Yorkshire Coalfield is marked by the change of its richest and highest grade coal seam, the Barnsley Seam or Bed, to a thin seam of inferior coal which occurs to the north of Barnsley. The southern limit was marked by the Barnsley Bed losing its coking qualities.

The structure of the coal field is not significantly affected by faults except along the River Don between Sheffield and Mexborough. These faults give rise to the Frickley and Maltby troughs where the coal measures are thrown down and lie deeper than in other parts of the coalfield.

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