Figure F5 (continued). L. Multicolor basalt breccia in Subunit IXC (interval 330-U1374A-15R-2A, 1–41 cm), interpreted as a debris flow deposit emplaced on a shallow-marine slope. M. Multicolor volcanic sandstone in Subunit XIA (interval 330-U1374A-21R-3A, 74–114 cm), interpreted as a hyperconcentrated flow deposit emplaced on a shallow-marine slope. N. Grayish basalt conglomerate with bioclasts in Subunit XIB (interval 330-U1374A-22R-1A, 55–95 cm), with (1) dissolved bivalve shell and (2) algal and possible bryozoan encrustation on a basalt clast, interpreted to have formed in an intertidal to subtidal environment on the slope of Rigil Guyot.
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