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  2. Debris flow - Wikipedia

    en.wikipedia.org/wiki/Debris_flow

    Debris flows tend to move in a series of pulses, or discrete surges, wherein each pulse or surge has a distinctive head, body and tail. A debris flow in Ladakh, triggered by storms in 2010. It has poor sorting and levees. Steep source catchment is visible in background. Debris-flow deposits are readily recognizable in the field.

  3. Mass wasting - Wikipedia

    en.wikipedia.org/wiki/Mass_wasting

    Landslides can be further classified by the importance of water in the mass wasting process. In a narrow sense, landslides are rapid movement of large amounts of relatively dry debris down moderate to steep slopes. With increasing water content, the mass wasting takes the form of debris avalanches, then earthflows, then mudflows.

  4. Sediment transport - Wikipedia

    en.wikipedia.org/wiki/Sediment_transport

    Large masses of material are moved in debris flows, hyperconcentrated mixtures of mud, clasts that range up to boulder-size, and water. Debris flows move as granular flows down steep mountain valleys and washes. Because they transport sediment as a granular mixture, their transport mechanisms and capacities scale differently from those of ...

  5. Mud and debris are flowing down hillsides across California ...

    www.aol.com/news/mud-debris-flowing-down...

    Commonly called mudslides, these dangerous torrents are usually referred to by geologists and first responders as debris flows, which the U.S. Geological Survey describes as fast-moving landslides ...

  6. Sediment gravity flow - Wikipedia

    en.wikipedia.org/wiki/Sediment_gravity_flow

    Most flows are liquefied, and many references to fluidized sediment gravity flows are in fact incorrect and actually refer to liquefied flows. [5] Debris flow or mudflow – Grains are supported by the strength and buoyancy of the matrix. Mudflows and debris flows have cohesive strength, which makes their behavior difficult to predict using the ...

  7. Sorting (sediment) - Wikipedia

    en.wikipedia.org/wiki/Sorting_(sediment)

    The degree of sorting is determined by the range of grain sizes in a sediment deposit and is the result of various transport processes (rivers, debris flow, wind, glaciers, etc.). This should not be confused with crystallite size, which refers to the individual size of a crystal in a solid. Crystallite is the building block of a grain.

  8. Alluvial fan - Wikipedia

    en.wikipedia.org/wiki/Alluvial_fan

    Debris flow fans receive most of their sediments in the form of debris flows. Debris flows are slurry-like mixtures of water and particles of all sizes, from clay to boulders, that resemble wet concrete. They are characterized by having a yield strength, meaning that they are highly viscous at low flow velocities but become less viscous as the ...

  9. Trump Doesn't Stand for Obama but Then Chats with Him ... - AOL

    www.aol.com/lifestyle/trump-doesnt-stand-obama...

    The five living U.S. presidents — Joe Biden, Donald Trump, Barack Obama, George W. Bush and Bill Clinton — reunited to honor the life and legacy of Jimmy Carter. On Thursday, Jan. 9, a date ...