Grain-size segregation and levee formation in geophysical mass flows

Data from large‐scale debris‐flow experiments are combined with modeling of particle‐size segregation to explain the formation of lateral levees enriched in coarse grains. The experimental flows consisted of 10 m3 of water‐saturated sand and gravel, which traveled ∼80 m down a steeply inclined flume...

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Bibliographic Details
Published inJournal of Geophysical Research: Earth Surface Vol. 117; no. F1
Main Authors Johnson, C. G., Kokelaar, B. P., Iverson, R. M., Logan, M., LaHusen, R. G., Gray, J. M. N. T.
Format Journal Article
LanguageEnglish
Published Washington, DC Blackwell Publishing Ltd 01.03.2012
American Geophysical Union
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