Figure F7. Close-up photograph of interval 198-1208A-3H-1, 90-135 cm, showing subparallel discontinuities at 98-118 cm, which could be the product of repeated erosion, faulting, or slumping. Darker (olive gray) nannofossil clay with diatoms is overlain by light olive-gray clayey nannofossil ooze. This interval is late Pleistocene in age.