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Rip-Up Clasts, California

Pictures of Sedimentary Structures

Rip-up clasts are created by vigorous flows of coarse sediment, like the seafloor avalanche that formed this turbidite bed. (more below)
Mud lumps caught up in a landslide
Photo (c) 2008 Andrew Alden, licensed to About.com (fair use policy)
As the gravel and sand coursed down slope, it occasionally swept up chunks of the muddy sides of its channel. A few of these clasts are preserved as mudstone, which is much softer than the conglomerate around it. Thus these particular rip-up clasts have largely eroded out of the surrounding rock, but enough of the shaly material is left to tell what once filled the holes. They may also be called mudstone clasts, intraformational or intrabasinal clasts, or clay chips.

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