Fig. 5.From: Sediment distribution on the inner continental shelf off Khao Lak (Thailand) after the 2004 Indian Ocean tsunamiThe boulder density on the reef fringing Pakarang Cape (seafloor type G) is higher towards its offshore boundary (A, approx. 11-m water depth), compared with the landward boundary (B, approx. 9-m water depth). For positions, refer to Fig. 2.Back to article page