Fringing reefs in deeper waters (>5 m) have so far been described 
                primarily for the west coast. They are generally found where the 
                island shelf is "wider". For Dominica's west coast this 
                means approximately 200 - 500 m. None of these reef systems reach 
                the surface and so the reef flats remain in 12-8 meters. Lagoonal 
                settings or fringing-lagoon reefs are absent. 
              The 
                largest and best developed representative of this reef type (approximately 
                2.6 km long) is found along the west and southwest-facing contour 
                of the shelf lining the Grand Savane area. It is architecturally 
                diverse, with a high species richness and extensive live benthic 
                cover of sponges, soft corals and hard corals. Local dive sites 
                within this reef system include Lauro Reef, Rena's Reef and several 
                other sites in between these two. The reef flat and the fore reef 
                are the most appealing visually and in their diversity. Erosional 
                sand chutes exist, these are often lined with massive framework 
                builders such as M. annularis and M. faveolata. 
                Intermittently, towards shore, the reef flat gradually transitions 
                into sandy environments characterized by a variety of primary 
                hard substrates originating from cliffs, beaches, and rivers, 
                all of which form the stable substrate for sessile organisms. 
                See "OTHER CORAL HABITATS". 
                
              The 
                northern-most section of this system, within approximately 500 
                and 150 m from the mouth of the Batali River, is characterized 
                by a series of linear reefs, oriented perpendicularly to shore, 
                in waters between 10 and 30 meters depth. Although not connected 
                these individual reefs are aligned like a spur and grove system.
              Mero 
                harbors the second largest such system along the West coast but 
                with a substantial contribution of primary hard substrates in 
                5-10 meters depth. This region is also characterized by mixed 
                sea grass beds and large (500 m2 +) mono-specific coral assemblages. 
                See OLIGOSPECIFIC ASSEMBLAGES 
                .
              Besides 
                these two locations, true fringing reefs in deeper waters (with 
                coral accretion) are virtually absent along the west coast.
                
                SCCS1106