Title: Chapter 9 Mass Wasting
1Chapter 9 Mass Wasting
GEOL 101 Introductory Geology
2Mass 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
3Mass 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
4Type of Movement
5Rate of Movement
6Controlling factors
7Gravity Forces
8Oversteepened Slopes
9Common Types of Mass Wasting
- Creep
- Debris flow
- Earthflow
- Mudflow
- Debris Avalanche
- Rockslide and Rock Fall
10Slow 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
11Creep
12Creep
13Creep Mechanism
14Permafrost Regions in the Northern Hemisphere
15Permafrost Mechanism
16SolifluctionPermafrost in Fairbank, AK
17Permafrost DamageFairbanks, AK
18Rapid 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
19Rapid Forms of Mass Wasting
20Earthflow
21EarthflowSonoma County, CA
22Mudflow Damagenorthern, CA
23Lahar (Debris Flow)1980 Mt. St. Helens eruption
24Rock AvalanceGlacier National Park, MT
25Rapid 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
26Slump (with Earthflow near toe)
27Slumpsouthwest, MT
28Gro Ventre Rockslide
29Vaiont Canyon, ItalyLandslide
30Landslide ScarDawson, Yukon
31Slide Surface Orientation
32Rock FallWallawa Mountains, OR
33Controls 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
34Undercutting by Waves
35Earthquake Shaking(Liquefaction)
36Earthquake Triggered LandslidesLake Tahoe, CA
37Mass Wasting Prevention
- Slope Monitoring
- Engineering
- Planting vegetation
- Cut-and-fill
- Lower water table
- Terrace slopes
- Retaining walls
- Rock bolts
- Avalanche Shed
38Slope Monitoring
39Mass Wasting Prevention
40Mass Wasting Prevention
41Mass Wasting Prevention
42Mass Wasting Prevention