Titlebook: British Upper Carboniferous Stratigraphy; C. J. Cleal,B. A. Thomas Book 1996 Springer Science+Business Media Dordrecht 1996 Carboniferous.

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South Wales,xtends from Pontypool in the east to near Kidwelly in the west. Carmarthen Bay separates this from a smaller area of outcrop in Pembrokeshire. With the exception of the Iberian Peninsula (Lemos de Sousa and Oliviera; 1983, Martinez Diaz, 1983), South Wales provides by far the best exposed sequences

Cupping

Forest of Dean and Severn coalfields,rly exposed and is not dealt with further here (the Newent Coalfield — see Cleal, 1987 and Worssam ., 1989, for brief accounts of this coalfield). The Severn Coalfield has never been worked commercially, but the Forest of Dean was, until about 20 years ago, still commercially active. According to Bo

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Bravado

North Wales,e Dee Estuary and Oswestry. This includes the Flint-Derbyshire Coalfield which, until relatively recently, was still being actively mined. The Westphalian also outcrops in the Vale of Clwyd (between Dyserth and Ruthin), near Caernarvon, and on Anglesey.

Hay-Fever

Millstone Grit of the Central Province,rth (Figure 9.1). It is the thickest development of Millstone Grit in Britain, with a maximum thickness of over 180 m near Burnley and Skipton, and outcrops over an area of more than 4000 m. Much of the strata is relatively resistant to erosion, resulting in rugged scenery most typically represented

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Coal Measures of the Pennine Basin,and most fully developed coalfields north of the Wales-Brabant Barrier, with up to 2000 m of Westphalian strata being present. They have also yielded abundant and diverse assemblages of non-marine bivalves (e.g. Eagar, 1946, 1947, 1951, 1952b, 1956), marine band faunas (e.g. Calver, 1968) and plant

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Northern England,berland, Durham and Cumbria, although (despite the name generally given to the area) it also extends into the southernmost parts of Scotland. It is in effect a northern continuation of the Central Province/Pennine Basin, and some authors do not distinguish between them. However, there are a number o

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