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A satellite picture covering the deltaic plain of the Baram River (Fig. 1) has been interpreted in terms of sedimentary environments (Fig. 2). The upper deltaic plain is characterised by the extensive development offreshwater swamps, mainly covered by peat deposits. The lower deltaic plain is restricted to a narrow fringe of salt-tolerant vegetation which develops on both side of the distributaries. The abandoned river network canbedelineated. Reconstruction of the paleomeandering belts clearly shows the interconnection between the modem Baram, Belait andMiri rivers.

New insight into the recent evolution of the Baram Delta from satellite imagery