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Figure F2. Seismic Line GeoB00-203 across ODP Holes 1026B and 1027C. Sediment structures and the sediment/basalt interface are clearly visible, as are steeply dipping normal faults to the west of Hole 1026B and a small basement high about halfway between the holes. Hole 1027C is located below the center of a major distributary channel for turbidites that flowed off the North American continental shelf (Davis et al., 1992; Zühls-dorff et al., 2005; Underwood et al., 2005; Hutnak et al., 2006).

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