Rheologic inferences from high water marks of debris flows

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Abstract

High water marks left by water rich debris flows can be used to constrain the rheologic character of the flow. A simplified time-dependent model based on the conservation of flow volume is used to illustrate the approach. An example from Madison County, Virginia is shown.

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Glaze, L. S., Baloga, S. M., & Barnouin-Jha, O. S. (2002). Rheologic inferences from high water marks of debris flows. Geophysical Research Letters, 29(8). https://doi.org/10.1029/2002GL014757

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