Mammoth Memory

Sliding (or mudflow) – Occurs after periods of heavy rain when loose surface material becomes saturated and the extra weight causes the material to become unstable and move rapidly downhill, sometimes in an almost fluid state

Sliding (sliding) mud pies downhill in the pouring rain made them flow like water.

Sliding (sliding) mud pies downhill in the pouring rain made them flow like water.

Movement of material, en masse, which remains together until impacting the bottom of the slope.

Movement of material, en masse, which remains together until impacting the bottom of the slope.

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