“…Where studied, the areas of the GSR, between Shetland and to Iceland Ridge have revealed a complex pattern of channel pathways controlled by the seabed topography (Dom and Werner, 1993;Kuijpers et al, 1998;Kenyon et al, 2003), bedforms (Masson et al, 2004) as well as sandy, channel-related sediment drifts (Kenyon et al, 2003).…”