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Coal measures
The Coal Measures is a lithostratigraphical term for the coal-bearing part of the Upper Carboniferous System. The Coal Measures Group consists of the Upper Coal Measures Formation, the Middle Coal Measures Formation and the Lower Coal Measures Formation. The group records the deposition of fluvio-deltaic sediments which consists mainly of clastic rocks (claystones, shales, siltstones, sandstones, conglomerates) interstratified with the beds of coal. In most places, the Coal Measures are underlain by coarser clastic sequences known as Millstone Grit, of Namurian age. The top of the Coal Measures may be marked by an unconformity, the overlying rocks being Permian or later in age. In some parts of Britain, however, the Coal Measures grade up into mainly coal-barren red beds of late Westphalian and possibly Stephanian age. Within the Pennine Basin these barren measures are now referred to as the Warwickshire Group, from the district where they achieve their thickest development.〔Powell, J.H. et al. 2000. ''Stratigraphical framework for Westphalian to early Permian red-bed successions of the Pennine Basin'', British Geological Survey Research Report, RR/00/01〕
The Coal Measures formed during Westphalian and earliest Stephanian times in the European ('Heerlen') chronostratigraphical scheme (which is approximately equivalent to the Middle Pennsylvanian Series of the IUGS global chronostratigraphical scheme).
==Informal usage for other coal-bearing strata==
In the eastern United States the term coal measures has been applied to the Pennsylvanian coal fields. Generally, the Pittsburgh coal seam is considered the base of the upper coal measures, exposed along the Monongahela River, while the lower coal measures are exposed along the Allegheny River.〔Stratigraphy of the Bituminous Coal Field in Pennsylvania, Ohio and West Virginia, (Bulletin of the United States Geological Survey No. 65 ), Washington, Government Printing Office, 1891. See Chapter III and V.〕
The term coal measures has also historically been used in other parts of the world for coal-bearing successions of various ages, e.g. the Permian coal measures of Australia and the late Cretaceous and early Tertiary coal measures found in New Zealand. However, these usages are mostly informal.
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