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.
CITATION STYLE
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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