Mass Wasting Flashcards

1
Q

Mass Wasting

A

-Masses of debris (mud, sand, gravel) or bedrock moving downhill driven by gravity
-Caused by slope failure
-Slopes can become unstable when they are oversteepened or comprise of unconsolidated material.
-Part of natural weathering and erosion process
Resisting force < Gravitational force - Friction < Shear Force

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2
Q

Triggers of Mass Wasting

A
  • tectonically uplifted areas
  • the oversteepening of a slope
  • vibrations from earthquakes or manmade events
  • heavy rainstorms
  • freeze-thaw action
  • volcanic activity
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3
Q

How can slope stability be determined

A
  • the angle of the slope
    -material strength
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4
Q

Factors of Mass Wasting

A

-Nature of material
-Cohesion (Cohesionless materials, loose sediments, can be stable within their ‘angle of repose ‘, depends on size, roughness, water content)
-Shear Strength
-Slope angle
-Thickness of debris over bedrock
-Consolidated vs unconsolidated material
-Water content
-Vegetation- (heavily vegetated vs light or no vegetation)

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5
Q

Nature of Material

A

-Unconsolidated (any loose and un-cemented material) such as soil, sediments, etc
-Angle of repose → for unconsolidated material, it is the maximum slope at which a pile of loose material will remain stable.

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6
Q

What determines the angle of repose

A

1) Particle size
2) Particle shape
3) Moisture Content

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7
Q

Example of Stronger Soils

A

Cemented, vegetated, clay-rich
* Clays can increase cohesion of materials
* Mineral cements (silica or carbonate) hold rock together
* Roots add strength to material by binding loose material together.

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8
Q

Example of Weaker Rocks

A

Planes of weakness (in bedrock) can reduce cohesion and stability
* bedding planes; foliation; joints
* plane orientation

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9
Q

Classification of Mass Wasting

A

-Type of material that moves
-Nature of movement (flow or slide)
-How fast Material Moves

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10
Q

What is rock fall

A
  • Sudden and rapid free fall movement of rock
  • Occur on steep slopes
  • Forms talus piles
  • Can be associated with rockslide
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11
Q

What is land-rock slide

A

 Movement along a defined slippage surface
 Blocks of rock detach along bedding planes, joints, fractures, etc.
 Occur on steep slopes
 Triggered by rain falls or ground vibration
 Very fast and most destructive type of mass wasting

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12
Q

What is flow (debris flow/avalanche)

A
  • Mixture of rocks, mud, & water
  • Moves as a viscous fluid
  • Common after heavy rains
  • Rapid movement – up to 100 km/h
  • Common in semi-arid regions
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13
Q

What happened to the Gyama Gold Mine Area

A

Happened March 28th 2013. 70 km east of Lhasa, Tibet. This rock avalanche buried 83 people. It was about 3 km long and between 20 m and 50 m thick, with a volume of about 2 million cubic meters.

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14
Q

What caused the Gyama Gold Mine Area Avalanche

A
  • steep V-shaped valley
  • earthquake activity
  • high meltwater runoff
  • lack of stability at its back started the slip
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15
Q

What is slump

A

– Scarp
– “Hummocky” terrain on and below

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16
Q

What is creep

A

Slow downslope movement – mm/y too slow to be observed in action

17
Q

What is Solifluction

A

Occurs in regions underlain by permafrost (permanently frozen, water-bearing ground)
 During warm periods top portion ‘active layer’ thaws and becomes saturated, loses cohesion and slides

18
Q

What engineering practices should be used to prevent mass wasting

A
  • Planting vegetation and/or drainage ditches
  • Retaining Walls
  • Shotcrete
  • Rock Bolts
  • Slope Stitching to Prevent Sliding