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Type of material, i.e., Rock or Soil
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Mechanism of movement, i.e., sliding, flowing, falling
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Velocity of movement, i.e., fast or slow
Summary of Landslides
Slides:
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- Slump (slow)
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- Slide/Glide (fast)
Flows:
-
- Avalanche (fast)
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- Creep (slow)
Falls:
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- Mostly fast
-
Slumps are the most common landslides
-
Moves on curved, concave upward surfaces, spoon-shaped
surfaces
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Vary in size form meters to kilometers
-
Involves mainly weathered geologic materials
(Figure here)
Slide/Glide:
-
Involves large masses of rocks
-
Move along sliding planes
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Mainly sedimentary bedding planes
Condition:
-
Bedding should be inclined less steeply than inclination of natural
slope
(Figure here)
Causes of Landslides
Gravity: is driving force for sliding
Cohesive and frictional forces: are resistive
forces: against sliding
If
GRAVITY > RESISTIVE FORCES = sliding
-
Certain Factors increase driving forces & promote sliding
- Increase in slope angle:
(Figure here)
Lack of lateral support:
(Figure here)
Added weight at the top of the slope
(Figure here)
-
Certain Factors reduce strength of slopes and thus reduce resistance to
sliding:
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Infiltration to produce ground H2O
-
Weathering of minerals and rocks
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Burrowing animals
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Excavation of slopes
Stabilization of Landslides
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Methods based on reducing instability of slopes, i.e., to decrease
driving forces OR increase resistive forces
a. Water Drainage and Control:
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Water is prevented from infiltrating
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putting liners at surface
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- In places with a lot of H2O subsurface, construct horizontal drains
to remove water from soils
b. Excavation and Redistribution
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Reconstruct slope: remove materials from top to bottom
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Toe may be removed and replaced with compacted soils i.e., TOE BUTTRESSED
c. Retaining Devices:
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Using stones, concrete, etc. buttress the toes of slopes
Transps (Types) - (5)
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Evidences of past/possible landslides:
-
Slope> 27° (i.e., 2:1 slope), accurate
scars (of former slumps, glides, etc.), bumpy convex upward slopes, springs,
wet areas, water-loving plants (i.e., H2O saturation), dip of bedding out
of hill, gentle angle of bedding than natural slope.
-
Evidence of creep:
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Telephone poles and fences tilting down-slope
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Cracked retaining wall, bent bases of tree
on slope, etc.
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