A debris flow is a type of sediment gravity flow. It is a rapid mass movement of a concentrated mixture of sediment, organic matter, and water that can flow like a liquid yet can stop on sloping surfaces and form a nearly rigid deposit. Observed debris flows commonly have been likened to flowing masses of wet concrete. Generically, debris flow includes mudflow (debris containing mostly sand, silt, and clay), lahar (volcanic debris flows), and till flow (debris flow from active or stagnant ice).
Debris flows are a significant geomorphological and sedimentological agent in a wide range of geologic and climatic settings. Subaerial debris flows pose a natural hazard than can cause fatalities, damage structures, and diminish land productivity. Subaqueous debris flows can produce turbidity currents, and they can transport sand from continental slopes to abyssal plains, threatening underwater infrastructures and creating important hydrocarbon reservoirs. Modern debris-flow deposits that line...
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Cross-references
Alluvial Fans Avalanche and Rock Fall Earth Flows Fabric, Porosity, and Permeability Flume Grading, Graded Bedding Grain Flow Grain Size and Shape Gravity-Driven Mass Flows Hindered Settling Imbrication and Flow-Oriented Clasts Liquefaction and Fluidization Mass Movement Slope Sediments Slurry Submarine Fans and Channels Tills and Tillites
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Major, J.J. (1978). Debris flow. In: Middleton, G.V., Church, M.J., Coniglio, M., Hardie, L.A., Longstaffe, F.J. (eds) Encyclopedia of Sediments and Sedimentary Rocks. Encyclopedia of Earth Sciences Series. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-3609-5_58
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