Figure F17. Digital images of (A) synsedimentary slump folding (interval 208-1266C-6H-2, 118-149 cm) and (B) inclined bedding (interval 208-1266A-10H-1, 95–140 cm), which suggests sedimentation on a depositional slope. Deposits formed in such a setting could result in mixing and duplication of the sequence through downslope creep or slides. The uppermost couplet of dark ash in A is overlain by white ooze and is in the correct orientation. Folding of this interval has overturned this sequence as an anticline with an axial plane that dips to the left, resulting in an inverted sequence. The lower ash-ooze couplet is again correctly oriented.

Figure F17. Digital images of (A) synsedimentary slump folding (interval 208-1266C-6H-2, 118–149 cm) and (B) inclined bedding (interval 208-1266A-10H-1, 95–140 cm), which suggests sedimentation on a depositional slope. Deposits formed in such a setting could result in mixing and duplication of the sequence through downslope creep or slides. The uppermost couplet of dark ash in A is overlain by white ooze and is in the correct orientation. Folding of this interval has overturned this sequence as an anticline with an axial plane that dips to the left, resulting in an inverted sequence. The lower ash-ooze couplet is again correctly oriented.