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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. Solifluction - Wikipedia

    en.wikipedia.org/wiki/Solifluction

    Solifluction is a collective name for gradual processes in which a mass moves down a slope ("mass wasting") related to freeze-thaw activity. This is the standard modern meaning of solifluction, which differs from the original meaning given to it by Johan Gunnar Andersson in 1906. [1] [2]

  5. 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]

  6. Slumgullion Earthflow - Wikipedia

    en.wikipedia.org/wiki/Slumgullion_Earthflow

    It is "a striking example of mass wasting (the movement of large masses of earth material)." The Lake Fork of the Gunnison River was dammed by the earthflow, creating Lake San Cristobal. [1] A second earthflow has been moving continuously for about 300 years over older, stable rock. [3]

  7. Volcanic landslide - Wikipedia

    en.wikipedia.org/wiki/Volcanic_landslide

    A volcanic landslide or volcanogenic landslide is a type of mass wasting that takes place at volcanoes. Occurrences

  8. 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 ...

  9. Gros Ventre landslide - Wikipedia

    en.wikipedia.org/wiki/Gros_Ventre_landslide

    It is one of the world's largest known examples of recent mass wasting events aside from volcanic eruptions. Slide Lake is now much smaller than before the flood. Slide Lake is now much smaller than before the flood.