Caption:
Oblique aerial view southward toward the Smallwood Reservoir where the confluence of three eskers is bounded by ribbed moraine to the west (at right), and streamlined landforms to the east (at left). This confluence of eskers is part of a large trunk esker system that begins northwest of Giasson Lake and terminates just north of Churchill Falls. In the foreground, strandlines of glacial Lake Low occur up to 8 metres above the present maximum level of the Smallwood Reservoir