Landslides

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The U.S. Geological Survey defines landslides to include a wide range of ground movement, such as rock falls, deep failure of slopes, and shallow debris flows. Although gravity acting on an over-steepened slope is the primary reason for a landslide, there are other contributing factors.

Landslides and mudslides can be initiated by storms, earthquakes, fires, volcanic eruptions, or human modification of the land. They can move rapidly down slopes or through channels and can strike with little or no warning at avalanche speeds, posing a serious hazard to properties on or below hillsides.

When landslides occur—in response to such changes as increased water content, earthquake shaking, addition of load, or removal of downslope support—they deform and tilt the ground surface. The result can be destruction of foundations, offset of roads, breaking of underground pipes, or overriding of downslope property and structures.

SAFER: Areas that are typically considered safe from landslides

  • On hard, non-jointed bedrock that has not moved in the past.
  • On relatively flat-lying areas away from sudden changes in slope angle.
  • At the top or along the nose of ridges, set back from the tops of slopes.

LESS SAFE: Areas that are generally prone to landslide hazards

  • On existing old landslides.
  • On or at the base of slopes.
  • In or at the base of minor drainage hollows.
  • At the base or top of an old fill slope.
  • At the base or top of a steep cut slope.
  • Developed hillsides where leach field septic systems are used.

What Can You do?........ Prepare for Landslides
What is the City doing?.....City Actions