Figure F6. Uppermost sections of cores at continental rise sediment drift Sites 1095, 1096 and 1101, showing lithologic variation over the past 200-300 k.y. and correlations of (interglacial) oxygen isotopic stages 1, 5, 7, and 9, from Barker et al. (1998). IRD = ice-rafted detritus.

Figure F6. Uppermost sections of cores at continental rise sediment drift Sites 1095, 1096 and 1101, showing lithologic variation over the past 200-300 k.y. and correlations of (interglacial) oxygen isotopic stages 1, 5, 7, and 9, from Barker et al. (1998). IRD = ice-rafted detritus.