has subdued magnetic relief indicating basement (basalt) depth of at least 400m. On the eastern part of the shelf there occur pronounced edge anomalies, apparently due to a basement step of at least 1 km mean thickness and mean width 3-4 km. The distance from the upper edge of this basement step to the bathymetric shelf edge increases from 5-8 kmat 19 W to 12-14 km at 14’30’W. The basement has alternating magnetic polarities. Linear magnetic anomalies are indistinct or absent in the surveyed region. It is speculated that the sharp basement step represents the trace of the maximum southerly extent of the eastern volcanic zone of Iceland.