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See simulation of a slide
Classification of Landslide Mechanisms
by Hutchins (in Brunsden, 1995)
Type Form of initial failure surface Subsequent deformation
Falls
Detached from a a. planar failure surface Free fall, may break up, roll bounce, slide, flow down slopes below. May involve fluidisation, liquefaction, cohesionless grain flow, heat generation, chemical rate effects or other secondary mecanisms.
b. wedge
c. stepped
d. vertical
Topples
Detachment from a. single a. pre-existing as above
discontinuities
b. multiple b. surface tension
failures
Sags
Movement on a a. single sided mountain slope May be early stages of landsliding and not display toe deformations other than bulging.
b. double sided a. of rotational
c. stepped b. compound form listric bi-planar discontinuity
Slides
Rotational movement sliding on a a. single circular failure Toe area may deform in a complex way. May bulge, override, flow, creep. May be retrogresive.
b. successive surface
c. multiple
Compound movement a. single non-circular Often develops a graben at the head. May have a toe failure of different type.
b. progressive a. listric
c. multi-storied b. bi-planar
Translational movement sliding on a a. planar failure surface May develop complex runout after disintegrating. As for falls and flows. Can develop sudden spreading failure in quick clays.
b. stepped
c. wedge
d. non-rotational
Flows
Movement by flow or creep on a. complex natural topographic surface Flow will involve complex runout from source. May be catastrophic. May move in sheets of lobes and involve viscous or rheological mechanisms. Creep may be gravity, seasonal, pre-failure or progressive.
i. unconfined
ii. channelised
Complex
Movements involving two or more of the categories above