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TABLE 7

Volcanic gas, at pressures equaling and probably exceeding lithostatic pressure, was intruded laterally at the base of the Bighorn Dolomite to produce a fluidized aggregate of fluid and solid that acted as a lubricant for this exceptionally low-angle landslide. This model was rejected by Pierce and Nelson (1970) based on field relations (over 50 discrete blocks were mapped, rather than a single sheet that is locally preserved as erosional remnants) and the unlikelihood that fluid pressure could be sustained over such a large area to support displacement of such a large landslide block

More surface area means faster drying

Lipsitt, and Stephen L

doi: 10.1001/archpedi.161.5.440