The Maldives is an archipelago located on the Chagos-Laccadives ridge, a prominent feature of the mid Indian Ocean basin, which runs from 9°S to 14°N of the equator. The Maldives archipelago runs from 0°41′48"S 7°06′30"N, occupying the central and largest part of the ridge (Fürstenau et al., 2010). The central location of the Maldives in the Indian ocean, equidistant from the East African and South East Asian reefs, gives rise to a high diversity of ecological species in the archipelago, with high affinities to both regions, within the larger "Chagos stricture" (Kench, 2011). The Maldives is widely recognized as a marine ecological hotspot, part of the world's most extensive atoll formation and the seventh largest reef system in the world, containing over 5% of the world's coral reefs and supporting over 1000 fish, 300 coral and 350 crustacean species (Emerton et al., 2009). Available sources indicate that little has been done to study the bathymetry of the country over large geographic scales since the development of Admiralty charts over a century ago (Kench, 2011). The first largescale bathymetric survey of the Maldives was carried out by Commander James Moresby from 1835 -1883(Gardiner, 1902. These charts still form the underling data for navigational charts of the Maldives. Several subsequent expeditions in the early 20th century by J.