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- A landslide or Landslip is
a geological phenomenon which
includes a wide range of ground
movement
HELP!!!!
Landslides occur when the
stability of a slope changes from a
 stable to an unstable condition. A
  change in the stability of a slope
   can be caused by a number of
 factors, acting together or alone.
    Natural causes of landslides
                include:
   groundwater pressure acting to destabilize the
    slope.
   Loss or absence of vertical vegetative
    structure, soil nutrients, and soil structure (e.g.
    after a wildfire).
   erosion of the toe of a slope by rivers or
    ocean waves.
   weakening of a slope through saturation by
    snowmelt, glaciers melting, or heavy rains.
   earthquakes adding loads to barely stable slope.
   Earthquake-
    caused liquefaction destabilizing slopes.
   volcanic eruptions.
“Landslides are
aggravated by
human activities”
   deforestation, cultivation and construction, which
    destabilize the already fragile slopes.
   vibrations from machinery or traffic.
   Blasting.
   earthwork which alters the shape of a slope, or
    which imposes new loads on an existing slope
   in shallow soils, the removal of deep-
    rooted vegetation that
    binds colluvium to bedrock.
   Construction, agricultural or forestry activities
    (logging) which change the amount of water
    which infiltrates the soil.
- Sand boils or Sand
Volcanoes occur when water under
pressure wells up through a bed of
sand. The water looks like it is
"boiling" up from the bed of sand
Sand boils can be a mechanism contributing
 to levee failure during floods. This effect is
  caused by a difference in pressure on two
  sides of a levee or dike, most likely during
        a flood. This process can result
    in piping, whereby the removal of soil
    particles results in a pipe through the
  embankment. The creation of the pipe will
   quickly pick up pace and will eventually
     result in failure of the embankment.
A sand boil is difficult to stop. The
most effective method is by creating a
body of water above the boil to create
 enough pressure to slow the flow of
water. A slower flow will not be able to
move soil particles. The body of water
            is often created
with sandbags forming a ring around
                 the boil
Land slides

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Land slides

  • 1.
  • 2.
  • 3.
  • 4.
  • 5. - A landslide or Landslip is a geological phenomenon which includes a wide range of ground movement
  • 7.
  • 8. Landslides occur when the stability of a slope changes from a stable to an unstable condition. A change in the stability of a slope can be caused by a number of factors, acting together or alone. Natural causes of landslides include:
  • 9. groundwater pressure acting to destabilize the slope.  Loss or absence of vertical vegetative structure, soil nutrients, and soil structure (e.g. after a wildfire).  erosion of the toe of a slope by rivers or ocean waves.  weakening of a slope through saturation by snowmelt, glaciers melting, or heavy rains.  earthquakes adding loads to barely stable slope.  Earthquake- caused liquefaction destabilizing slopes.  volcanic eruptions.
  • 10.
  • 12. deforestation, cultivation and construction, which destabilize the already fragile slopes.  vibrations from machinery or traffic.  Blasting.  earthwork which alters the shape of a slope, or which imposes new loads on an existing slope  in shallow soils, the removal of deep- rooted vegetation that binds colluvium to bedrock.  Construction, agricultural or forestry activities (logging) which change the amount of water which infiltrates the soil.
  • 13.
  • 14.
  • 15.
  • 16. - Sand boils or Sand Volcanoes occur when water under pressure wells up through a bed of sand. The water looks like it is "boiling" up from the bed of sand
  • 17.
  • 18. Sand boils can be a mechanism contributing to levee failure during floods. This effect is caused by a difference in pressure on two sides of a levee or dike, most likely during a flood. This process can result in piping, whereby the removal of soil particles results in a pipe through the embankment. The creation of the pipe will quickly pick up pace and will eventually result in failure of the embankment.
  • 19.
  • 20. A sand boil is difficult to stop. The most effective method is by creating a body of water above the boil to create enough pressure to slow the flow of water. A slower flow will not be able to move soil particles. The body of water is often created with sandbags forming a ring around the boil