The stratigraphy arising from this deposition of sediments is not simple. Various features of the sediments
The base of the Langsettian is defined as the base of the Subcrenatum (Pot Clay) Marine Band and is followed by a series of shales and sandstones with a few coals. The base of the Duckmantian is defined by the Vanderbeckei (Clay Cross) Marine Band. Most of the important ironstones and worked coals are found from the middle of the Langsettian to the middle of the Duckmantian. The base of the Bolsovian is at the Aegiranum (Mansfield) Marine Band, and in our area about 350 m of mudrocks, with relatively fewer coals, extend to the eroded top of the Westphalian succession. In Staffordshire sediments from the younger Westphalian D are found. These are red beds, indicating drier soils and oxidising conditions, and implying uplift, and similar reddening in Westphalian C sediments also occurs near Rotherham.
Detailed work (Hallsworth & Chisholm, 2000) on the lowest sandstones indicate they were brought in from the north, like the underlying Namurian sandstones they resemble (Fig 2). Their heavy mineral content show that in the catchments to these rivers were granites and granulite metasediments suggesting the older roots of the earlier Caledonian orogenic belt were being eroded.
About 200 m up from the base of the Westphalian a series of sandstones derived from the west overlaps the northerly series and continues from the Greenmoor sandstone up to the Abdy Rock. These river catchments produced a heavy mineral suite which suggested that mature sediments, with occasional ophiolite (ancient seafloor, obducted by plate movements) were being weathered to supply the sediment. The source of these rivers is probably along the Variscan mountain front, well into Laurentia.
The Woolley Edge Rock is probably the first of a series of sandstones that continue well into the Bolsovian, where the heavy mineral content suggests the sediment source was along the rising front of the Variscan orogenic belt to the east. The heavy minerals contained in these sandstones suggest a wide variety of orogenic-belt rock types including both low and high grade meta-sediments, granites and ophiolites were being weathered in the catchments.