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Processes of Mass Wasting Janet Koch EDU 290 PowerPoint Presentation
Definition ,[object Object]
Water influences the effects of mass wasting but gravity is the most important factor,[object Object]
Angle of Repose
Type of Material (Rock, soil, sediment)
Water saturation (increases slope failure)  ,[object Object]
When Gravity Wins ,[object Object]
Shear strength resists movement, if gravity is too strong the object loses friction,[object Object]
Weathering and Climate ,[object Object]
Weathering decomposes material and reduces the strength of the slope
Loose materials are most susceptible as they are not stable,[object Object]
Vegetation Increases slope stability!  Absorb water from rainfall and roots stabilize within soil
Criteria for Mass Wasting Type of material… Type of movement… Rate of movement… Rock, debris, soil, mud Fall, slide, slump, flow, creep Fast, slow, not visible
Falls Very rapid movement, talus formation, often triggered by earthquakes.
Slump Movement along a curved surface, caused by steepening of the slope
Flow Slow to rapid movement but often appears to have a plastic movement (Debris-flow vs. Mudflow)
Solifluction Common in areas of permafrost, very slow movement when frozen surface melts in summer

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Edu290 ppt1koch

  • 1. Processes of Mass Wasting Janet Koch EDU 290 PowerPoint Presentation
  • 2.
  • 3.
  • 5. Type of Material (Rock, soil, sediment)
  • 6.
  • 7.
  • 8.
  • 9.
  • 10. Weathering decomposes material and reduces the strength of the slope
  • 11.
  • 12. Vegetation Increases slope stability! Absorb water from rainfall and roots stabilize within soil
  • 13. Criteria for Mass Wasting Type of material… Type of movement… Rate of movement… Rock, debris, soil, mud Fall, slide, slump, flow, creep Fast, slow, not visible
  • 14. Falls Very rapid movement, talus formation, often triggered by earthquakes.
  • 15. Slump Movement along a curved surface, caused by steepening of the slope
  • 16. Flow Slow to rapid movement but often appears to have a plastic movement (Debris-flow vs. Mudflow)
  • 17. Solifluction Common in areas of permafrost, very slow movement when frozen surface melts in summer
  • 18. Creep Slowest flow, visible through features such at tilted trees or telephone poles
  • 19. How do we control masswasting? Improve drainage Ditches, gutters, vegetation, drainpipes Decrease slope Cut and fill, benching Build retaining walls Provide support at the bottom of a slope
  • 20. References Text and Figures Schaetzl, Randy, 2011, Masswasting, Environmental Geomorphology 306 Steinbis, Martin, 20ll, Masswastepdf, Geology 100 Pictures Clip art images