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coal measures

 
Dictionary: coal measures

pl.n. Geology
  1. Coal Measures A stratigraphic unit equivalent to the Pennsylvanian or Upper Carboniferous Periods.
  2. Strata of the Carboniferous Period usually containing coal deposits.

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Major division of Upper Carboniferous (323 – 290 million years ago) rocks and time in Great Britain. The Coal Measures account for much of England's coal production. The deposits consist largely of bituminous coal, though anthracite coals occur in southern Wales. Though local variation in the coal seams occurs, great uniformity is evident on a regional scale, and some coal beds can be identified throughout Great Britain and even on the European continent.

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Wikipedia: Coal measure
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British coalfields in the nineteenth century.

The Coal Measures is a lithostratigraphical term for the coal-bearing part of the Upper Carboniferous System. It represents the remains of fluvio-deltaic sediment, and 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..[1][2]

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).

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.[3]

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.

See also

References

  1. ^ Rayner, D H; Hemingway, J E, The Geology and Mineral Resources Of Yorkshire, Leeds: Yorkshire Geological Society (published 1974) 
  2. ^ Edwards, W; Trotter, F M, The Pennines and Adjacent Areas, British Regional Geology (Third ed.), London: HMSO. Natural Environment Research Council (published 1954) 
  3. ^ Strategraphy 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.

Further reading

  • CJ Cleal and BA Thomas, Plants of the British Coal Measures, The Palaeontological Association, 1994.
  • CJ Cleal and BA Thomas, British Upper Carboniferous stratigraphy, Chapman & Hall, London, 1995.



 
 

 

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Dictionary. The American Heritage® Dictionary of the English Language, Fourth Edition Copyright © 2007, 2000 by Houghton Mifflin Company. Updated in 2009. Published by Houghton Mifflin Company. All rights reserved.  Read more
Britannica Concise Encyclopedia. Britannica Concise Encyclopedia. © 2006 Encyclopædia Britannica, Inc. All rights reserved.  Read more
Wikipedia. This article is licensed under the Creative Commons Attribution/Share-Alike License. It uses material from the Wikipedia article "Coal measure" Read more