Geoscience Reference
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The greater slope lengths produce greater erosion potential. See Table 15.9.
Table 15.8 Landslide velocity scale (Cruden and Varnes, 1996).
Description
Velocity
(mm/s)
Typical
velocity
Probable destructive significance
Extremely rapid
Catastrophe of major violence; buildings
destroyed by impact of displaced material;
many deaths, escape unlikely.
5 10 3
5 m/second
Very rapid
Some lives lost; velocity too great to permit
all persons to escape.
5 10 1
3 m/minute
Rapid
Escape evacuation possible; structures,
possessions, and equipment destroyed.
5 10 1
1.8 m/hour
Moderate
Some temporary and insensitive structures
can be temporarily maintained.
5 10 3
13 m/month
Slow
Remedial construction can be undertaken
during movement; insensitive structures
require frequent maintenance work if total
movement is not large during a particular
acceleration phase.
5 10 5
1.6 m/year
Very slow
Some permanent structures undamaged by
movement.
5 10 7
16 mm/year
Extremely slow
Imperceptible without instruments;
construction possible with precautions.
Figure 15.1 Erosion and deposition process (Here from Bell, 1998, after Hjulstrom, 1935).
 
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