Classifying Mass Movements
Classified by- Type
- Material
- Rate of movement
Type
-
Type of movement: Fall, Slide, Flow
Type of material: Rock or Regolith (debris or earth)
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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
Rotational landslides - These slides mostly occur in homogeneous material and have a curved slide plane
Slump: 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: movement parallel to planes of weakness and slope.
Translational landslide - these slides typically occur along a planar surface, such as between bedding planes. Translational slides are the most common in S. California in Miocene-aged Formation rocks.
Development
of a rotational landslide in homogeneous material. The
material fails, creating a curved slideplane. The gap
at the top of the slide is called the scarp, and the
excess material at the base of the slide is called the
toe. |
translational
landslides begin in bedrock, such as siltstone, which
is dipping in the same direction as the slope topography. Erosion
occurs at the base of the hillside, either by a stream
or even by a road cut. The bed no longer has anything to
support it at its base, and begins to slide downslope. |
Table 1 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)
|