F16. Highly disturbed interval caused by XCB coring.

F17. Normal-graded sandstone with a sharp, scoured base.

F18. Zoned plagioclase crystals set in siltstone matrix.

F19. Smear slide dominated by colorless, vesicular glass.

F20. Sharp-based, massive laminae of coarse- to fine-grained sand.

F21. Graded beds and laminae of volcaniclastic sandstone and siltstone.

F22. Volcaniclastic sandstone showing traces of primary bedding.

F23. Unaltered basaltic andesite clast set in a wackestone.

F24. Calcareous rock composed of shell and carbonate fragments.

F25. Cross section of a rugose coral in packstone.

F26. Silty claystone with shell fragments (without bioturbation).

F27. Burrowed silty claystone with local concentrations of shell fragments.

F28. Interlaminated lignite with silty claystone and sandstone laminations.

F29. Highly altered siltstone and sandstone with goethite concretions.

F30. Fragments of dolerite and orthoconglomerate.