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  2. Mass wasting - Wikipedia

    en.wikipedia.org/wiki/Mass_wasting

    Mass wasting, also known as mass movement, [1] is a general term for the movement of rock or soil down slopes under the force of gravity. It differs from other processes of erosion in that the debris transported by mass wasting is not entrained in a moving medium, such as water, wind, or ice.

  3. Slump (geology) - Wikipedia

    en.wikipedia.org/wiki/Slump_(geology)

    It is the removal of the slope's physical support which provokes this mass wasting event. Thorough wetting is a common cause, which explains why slumping is often associated with heavy rainfall, storm events and earthflows. Rain provides lubrication for the material to slide, and increases the self-mass of the material.

  4. Earthflow - Wikipedia

    en.wikipedia.org/wiki/Earthflow

    It is an intermediate type of mass wasting that is between downhill creep and mudflow. The types of materials that are susceptible to earthflows are clay, fine sand and silt, and fine-grained pyroclastic material. [1] When the ground materials become saturated with enough water, they will start flowing (soil liquefaction). Its speed can range ...

  5. Landslide - Wikipedia

    en.wikipedia.org/wiki/Landslide

    Landslides, also known as landslips, skyfalls or rockslides, [3] [4] [5] are several forms of mass wasting that may include a wide range of ground movements, such as rockfalls, mudflows, shallow or deep-seated slope failures and debris flows. [6]

  6. Mudflow - Wikipedia

    en.wikipedia.org/wiki/Mudflow

    A mudflow, also known as mudslide or mud flow, is a form of mass wasting involving fast-moving flow of debris and dirt that has become liquified by the addition of water. [1] Such flows can move at speeds ranging from 3 meters/minute to 5 meters/second. [2]

  7. Rockslide - Wikipedia

    en.wikipedia.org/wiki/Rockslide

    Amongst these erosional properties, water is arguably the most effective geologic agent that causes mass-wasting events to occur. Water aids in the downslope movement of surface material by adding weight to the soil and by filling pores which tends to push apart individual grains, decreasing the resistance of the material to movement. [4]

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  9. Geology of the Grand Canyon area - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Grand...

    This type of mass wasting is the main way the smaller and steeper side canyons transport sediment but it also plays a major role in excavating the larger canyons. [80] Glen Canyon Dam has greatly reduced the amount of sediment transported by the Colorado River through the Grand Canyon.