• Channel-form debris flows. Clast deposits that occur in channel-form geometries are known from locality A and perhaps also at localities C and F. The best exposed channel (locality A) is approximately 20-25 m across and about 4 m thick. The clasts are lenticular with tapered margins, perhaps in part due to structural stretching, and range in size from less than 1 to about 5 cm thick and from 2 to 30 cm long. Graded bedding is not observed; however, the long axes of the clasts are usually subparallel to bedding...At locality A the upper contact of the debris flow is undulatory and is capped by a carbonate turbidity-flow deposit. The channel-form debris flow deposits at locality A (perhaps also C and F) may represent either proximal flow or flow retained in a channel system.

• The dark-gray to black limestone clasts [containing fossils] have micritic, microspar, and finely crystalline textures. They are abundant in the channel-form deposits and are supported by a calcareous, bluish-gray shale/slate matrix.