In spring and fall 1985, air expendable bathythermograph surveys of a large area off the northeast coast of South America revealed an extensive field of subthermocline thermal staircases which is probably the site of vigorous salt fingering. During both seasons the staircases were shallowest in the south (180--360 m) and deepest in the northwest (420--650 m), occuring on the average between the 8¿ and 13¿C isotherms. Typically, each staircase consisted of 10 well-mixed layers with average thickness of 16 m and average interlayer temperature change of 0.52¿. Thicker layers seemed to be associated with larger temperature changes. No seasonal variation in these paramters was observed. The interfaces separating the layers had a modal thickness of 2 m, with interfaces in the spring tending to be thinner than in the fall. The region bounded by 10¿--14¿N, 52¿--57¿W tended to have staircases with more layers, thicker layers, and larger interlayer temperature changes. The sharp northeastern staircase field boundary occurs at the confluence of the Subtropical Underwater and the Antarctic Intermediate Water, suggesting that the staircases may be formed in this region and then extend south and west to form the rest of the field. ¿ American Geophysical Union 1989