sábado, enero 31, 2009

Landslide Types


Landslides or slope movements can be classified in many ways. There are many attributes used as criteria for identification and classification including:

  • Rate of movement: This ranges from very slow creep (millimetres/year) to extremely rapid (metres/second).
  • Type of material: Landslides are composed of bedrock, unconsolidated sediment and/or organic debris.
  • Nature of movement: The moving debris can slide, slump, flow or fall.

Common landslide types are:

Slump diagramSlump: complex movement of materials on a slope; includes rotational slump.

NOTE: This is the same type of landslide that is occuring in Anaheim Hills.

Slide diagramSlide: movement parallel to planes of weakness and occasionally parallel to slope.

Creep diagramCreep: gradual movement of slope materials

Topple diagramTopple: the end-over-end motion of rock down a slope.

Fall diagramFall: material free falls.

Flow diagramFlow: viscous to fluid-like motion of debris.

Torrent diagramTorrent::a sporadic and sudden channelized discharge of water and debris.

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