Figure F4. Bed-by-bed columns based on FMS images. Correlation is identical to Figure F3, p. 15, and is based on age ties from Takahashi et al. (this volume). Turbidite sands in Hole 1118A are thicker and more abundant than in other holes, particularly below ~700 mbsf. Facies letters are provided adjacent to the columns. Very fine grained sand could not be distinguished from silt and fine-grained sand on the FMS images, so is not recognized as a separate sediment grade. (An oversized figure accompanies this volume.)

Figure F4. Bed-by-bed columns based on FMS images. Correlation is identical to Figure F3 and is based on age ties from Takahashi et al. (this volume). Turbidite sands in Hole 1118A are thicker and more abundant than in other holes, particularly below ~700 mbsf. Facies letters are provided adjacent to the columns. Very fine grained sand could not be distinguished from silt and fine-grained sand on the FMS images, so is not recognized as a separate sediment grade. (This figure is available in an oversized format.)