Slumps are common in:

Name: Slumps are common in:
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Slumps are most commonly observed in soft sedimentary rocks such as shale and clay-rich rocks. These types of rocks are prone to instability due to their fine-grained nature and tendency to absorb water, resulting in lubrication and destabilization of the slope material. Hard sandstones, granites, and volcanic rocks are generally more resistant to slumping and are less prone to instability.

Slumps Are Common In