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Mass Wasting

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Classifying Mass Wasting Events

Classified by

  • Type
  • Material
  • Rate of movement

Type

    There are several types of mass movement. Here is a Shockwave animation from Pearson Education showing the five main types of mass movements.

    Type of movement: Fall, Slide, Flow
    Type of material: Rock or Regolith (debris or earth)
    =========================================
    Put together to describe! Examples: Rock Fall, Earth Slide, etc.

Slides and debris flows are the most common in Southern California.

Creep: gradual movement of slope materials
Slump (aka rotational): complex movement of materials on a slope
Topple
: the end-over-end motion of rock down a slope.
Fall: material free falls
Flow: viscous to fluid-like motion of debris.
Torrent: a sporadic and sudden channelized discharge of water and debris
Slide (aka translational): movement parallel to planes of weakness and slope.

The table below (modified from Varnes, 1978) summarizes one way of naming slope-failure deposits and their associated slope failure type.
      TYPE OF MATERIAL
      TYPE OF MOVEMENT
      BEDROCK
      ENGINEERING SOILS

      Predominantly coarse

      Predominantly fine
      Rock fall
      Debris fall
      Earth fall
      Falls
      Rock topple
      Debris topple
      Earth topple
      Topples
      Rock slump
      Debris slump
      Earth slump
      Slides
      rotational
      few units

      Rock block slide

      Rock slide

      Debris block slide

      Debris slide

      Earth block slide

      Earth slide

      translational
      many units
      Rock spread
      Debris spread
      Earth spread
      Lateral Spreads

      Rock flow

      (deep creep)

      Debris flow

      (soil creep)

      Earth flow
      Flows
      Combination of two or more principal types of movement
      Complex


Rate of Movement

  • Fast
    • Slumps
    • Rock slides
    • Debris flows
    • Earthflows
  • Slow
    • Creep
    • Solifluction (the gradual flow of a saturated layer that is underlain by an impermeable zone)

 

 

 
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CSULA Department of Geosciences and the Environment
Pasadena City College Department of Geology    
    © Sonjia Leyva 2018