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Numerous small canyons and gullies begin or end on the middle and upper continental slope off Guatemala suggesting rapidly varying depositional centers and erosional sites. Seismic data indicate downslope sediment transport and deposition on the midslope above a high-amplitude diffractive acoustic basement. Near Hole 570 acoustic basement is at a position and depth that corresponds to recovered serpentinites and serpentinized peridotites. The topographic high west of Site 570 is the source of a high-gradient magnetic anomaly, and on the basis of seismic and magnetic data it is interpreted to be an exposed outcrop of acoustic basement.

A High Resolution Geophysical Survey of Deep Sea Drilling Project Leg 84 Site 570