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FIELD TRIP OBJECTIVES Over three days, this excursion will offer participants the opportunity to visit spectacular Carboniferous outcrops of palaeontologic, sedimentologic and structural interest in southern New Brunswick. The Norton fossil forest (Fig. 1) contains upright tree trunks smaller, but considerably older than at Joggins. Near Sussex, soft-sediment deformation (slumping) of shale and oil shale is visible over several magnitudes, with these strata overlain by coarsening upward lake shoreface sandstone. At Albert Mines, solid bitumen (Albertite) is abundant adjacent to abandoned mine shafts and fossil fish may be excavated with a bit of luck. Thick beds of often imbricate alluvial fan conglomerate form the ‘flower pots’ at Hopewell Cape (Fig. 2). Salt diapirism (Fig. 3) has folded and faulted over a kilometre thickness of nonmarine strata on the Maringouin peninsula.

Sedimentological, Structural and Paleontological Highlights of the Carboniferous Maritimes Basin in Southern New Brunswick