Deep Tow surveys conducted at two sites at the base of the Blake Spur and Blake Escarpment serve to delineate the contact between Mesozoic platform carbonates of the Blake Plateau and adjacent abyssal strata. The continental margin in the surveyed areas consists of steep limestone cliffs and headlands with over 2 km of relief. This extreme topography distorts the hydrographic structure of the water column and intensifies abyssal current flow in the surveyed areas. Significant lateral scarp retreat is indicated by the presence of broad, nearly horizontal benches of Mesozoic limestone presently exposed at the base of the Blake Spur and Escarpment in 4.5-5 km water depth; and by angular, apparently truncated limestone ledges that crop out on the cliff face. At the Blake Spur, the contact between Mesozoic platformal limestones and basinal Tertiary strata does not occur directly at the foot of the cliff, but is exposed on the abyssal plain within a 50 m deep erosional moat. Here, strong (>2 knots) south-flowing bottom currents occur within 100 m of the sea floor. The coincidence of this vigorous current flowing within the moat near the base of the escarpment and the eroded character of the sea floor suggests that currents are an important mechanism in sculpting this abyssal headland and contributing to lateral scarp retreat. Similar erosional processes are indicated along the Blake Escarpment near 29 o 03'N, where the relatively straight cliff face is interrupted by occasional steep-walled box canyons. On the headland between the canyons, the Mesozoic outcrop projects into the Blake-Bahama Basin for several kilometers as a broad, arcuate, gently-sloping bench. These outcropping benches of Mesozoic strata at the base of the escarpment are analogous to larger-scale buried benches observed in the subsurface that were formed by pre-Miocene erosion. Neogene and Quaternary scarp retreat is suggested by the location of the contact between Mesozoic rocks and younger strata seaward of the steeper cliff face, and is probably the result of current-induced erosion. Focused erosion may be facilitated by the presence of a thin (~50 m) filament of corrosive Antarctic Bottom Water (AABW) that flows vigorously along the base of the cliff at both sites. The recessed position of the canyons shelters them from the main flow of this abyssal current, but the steepness and morphology of the canyon walls suggest that additional unidentified erosional processes are focused at the canyon heads.