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Geophysical mass flows -debris flows, avalanches, landslides -are often initiated by volcanic activity. These flows can contain O(10 6 −10 10 ) m 3 or more of material. Typically this material is a mixture of soil and rocks in the centimeter size range, sometimes mixed with meter-sized boulders. These flows can be O(10) − O(100) m deep and can run out over tens of kilometers. And often these flows contain a significant quantity of interstitial fluid. The range of scales, the rheology of thisdoi:10.1098/rsta.2005.1596 pmid:16011934 fatcat:dih76h7r3fhyvmvpecmrdzhq2i