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Chapter 9 Mass Wasting

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Title: Chapter 9 Mass Wasting


1
Chapter 9 Mass Wasting
GEOL 101 Introductory Geology
2
Mass Wasting
  • Mass wasting downslope movement of rock,
    regolith, and soil under the direct influence of
    gravity
  • Role of mass wasting
  • Geologic process that often follows weathering
  • Combined effects if mass wasting and running
    water produce stream valleys

3
Mass Wasting Classification
  • Type of material
  • Debris
  • Mud
  • Earth
  • Rock
  • Snow
  • Type of movement
  • Fall (free-falling pieces)
  • Slide (material moves as a coherent mass)
  • Flow (material moves as a viscous fluid)
  • Rate of the movement
  • Rapid (Fast)
  • Slow

4
Type of Movement
5
Rate of Movement
6
Controlling factors
7
Gravity Forces
8
Oversteepened Slopes
9
Common Types of Mass Wasting
  • Creep
  • Debris flow
  • Earthflow
  • Mudflow
  • Debris Avalanche
  • Rockslide and Rock Fall

10
Slow Forms of Mass Wasting
  • Creep
  • Gradual movement of soil regolith downhill
  • Aided by the alternate expansion and contraction
    of the surface material
  • Solifluction
  • Flow of water-saturated debris over impermeable
    material, often permafrost
  • Can occur on gentle slopes

11
Creep
12
Creep
13
Creep Mechanism
14
Permafrost Regions in the Northern Hemisphere
15
Permafrost Mechanism
16
SolifluctionPermafrost in Fairbank, AK
17
Permafrost DamageFairbanks, AK
18
Rapid Forms of Mass Wasting
  • Earthflow
  • Form on hillsides in humid regions
  • Water saturates the soil
  • Involve materials rich in clay and silt
  • Mudflow
  • More water involved

19
Rapid Forms of Mass Wasting
20
Earthflow
21
EarthflowSonoma County, CA
22
Mudflow Damagenorthern, CA
23
Lahar (Debris Flow)1980 Mt. St. Helens eruption
24
Rock AvalanceGlacier National Park, MT
25
Rapid Forms of Mass Wasting
  • Slump
  • Movement of a mass of rock or unconsolidated
    material as a unit along a curved surface
  • Occurs along oversteepened slopes
  • Rockslide
  • Blocks of bedrock slide down a slope
  • Generally very fast and destructive

26
Slump (with Earthflow near toe)
27
Slumpsouthwest, MT
28
Gro Ventre Rockslide
29
Vaiont Canyon, ItalyLandslide
30
Landslide ScarDawson, Yukon
31
Slide Surface Orientation
32
Rock FallWallawa Mountains, OR
33
Controls and Triggers
  • Gravity is the controlling force
  • Important triggers include
  • Saturation of the material with water
  • Diminishes particle cohesion
  • Water adds weight
  • Oversteepening of slopes
  • Stable slope angle (angle of repose) is different
    for various materials
  • Oversteepened slopes are unstable
  • Removal of anchoring vegetation
  • Ground vibrations from earthquakes
  • May cause expensive property damage
  • Liquefaction water saturated surface materials
    behave as fluid-like masses that flow

34
Undercutting by Waves
35
Earthquake Shaking(Liquefaction)
36
Earthquake Triggered LandslidesLake Tahoe, CA
37
Mass Wasting Prevention
  • Slope Monitoring
  • Engineering
  • Planting vegetation
  • Cut-and-fill
  • Lower water table
  • Terrace slopes
  • Retaining walls
  • Rock bolts
  • Avalanche Shed

38
Slope Monitoring
39
Mass Wasting Prevention
40
Mass Wasting Prevention
41
Mass Wasting Prevention
42
Mass Wasting Prevention
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