Figure F2. Seismic Line GeoB00-466 across Second Ridge and Site U1301. Sediment structures and the sediment/basement interface are clearly visible. Site U1301 is located over the peak of a buried basement ridge, adjacent to a high-angle normal fault, near the western edge of a major Pleistocene distributary channel for turbidites. Please see additional discussion in Zühlsdorff et al. (this volume). Arrow indicates location of Hole U1301A and approximate projection of Holes U1301B, U1301C, and U1301D onto this seismic profile. Details from this profile and an adjacent seismic line are shown in Figure F3, including approximate penetration depths for individual holes.
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