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The Sydney Basin is situated in northeastern Cape Breton Island, Nova Scotia (Fig. 1), and extends a long way offshore. The Carboniferous strata of the basin include some 600 m thickness of productive coal measures within the Morien Group, which ranges in age from Westphalian C to Stephanian (Hacquebard 1972, Zodrow and Gastaldo 1982). The coal measures consist of alternations of coarse and fine sandstones and grey shales with seatearths and coals. Certain intervals are characterized by red and green mudstones while bituminous shales, commonly accompanied by thin limestone beds, are noticeable within the roof shales of some of the coal seams. Sandstone and small-pebble conglomerate infill paleochannels in the sequence. Although the fauna of the bituminous shales and limestones is regarded as non-marine, Hacquebard and Donaldson (1969) considered the coals (and the sequences in general) to be more typical of a paralic rather than a limnic type of coal basin.

Upper Pennsylvanian sediment dispersal and paleochannel orientation in the western part of the Sydney Coalfield, Cape Breton, Nova Scotia