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Mass Wasting

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Rockfall: rocks falling through air, form talus. Slides. Slump: slow, along curved surface ... Rockfall with Talus. Rock Slide. Rock Slide. Midterm 3. A step ... – PowerPoint PPT presentation

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Title: Mass Wasting


1
Mass Wasting
  • Or Stuff Rolls Downhill!

2
Mass Movements
  • Rock and soil moves down hill under the influence
    of gravity

3
Factors in slope stability.
  • 1) Material strength
  • 2) Internal friction
  • 3) External support
  • Together these are a slopes shear strength

4
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5
Shear Stress
  • The component of gravity dragging a rock down
    hill is the.

6
  • Slopes are in dynamic equilibrium
  • Angle of repose slope angle where shear strength
    equals forces of gravity

7
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9
Factors favoring movement
  • Slope angle -- steep
  • Weather and climate -- highly weathered
  • Water content - - High
  • Vegetation -- little vegetation
  • Overloading -- caused by humans

10
Types of Mass Movements
  • Classified based on movement rate, type (falling
    sliding, flowing), and material
  • Falls
  • Rockfall rocks falling through air, form talus
  • Slides
  • Slump slow, along curved surface
  • Rockslide fast, along planar surface
  • Flows (plastically or as a viscous fluid)
  • Mudflow fast, 50 silt and clay
  • Debris Flows larger size particles, more viscous
    (less water)
  • Earthflows slower
  • Creep slowest, extremely slow movement of
    material

11
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12
Rockfall
13
Rockfall with Talus
14
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15
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16
Rock Slide
17
Rock Slide
18
Midterm 3
  • A step back?
  • A 89
  • 79 B 88
  • 64 C 78
  • 55 D 63
  • F 54
  • HW Less than 89, turn in the right answers Due
    next Thurs.

19
Types of Mass Movements
  • Classified based on movement rate, type (falling
    sliding, flowing), and material
  • Falls
  • Rockfall rocks falling through air, form talus
  • Slides
  • Slump slow, along curved surface
  • Rockslide fast, along planar surface
  • Flows (plastically or as a viscous fluid)
  • Mudflow fast, 50 silt and clay
  • Debris Flows larger size particles, more viscous
    (less water)
  • Earthflows slower
  • Creep slowest, extremely slow movement of
    material

20
Mudflow
  • Estes Park, CO

21
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22
Earth Flow
  • Baraga, MI.

23
EarthFlow
  • Slumgullion Earth flow
  • This old stable flow descendes from an elevation
    of 11,500 feet to 8,500.
  • 4 miles in length and covers about 1,000 acres
  • Outside Lake City, CO
  • Drunken Forest - trees not vertical!

24
Slumgullion Earth Flow
25
Creep
  • Marathon, Texas

26
Creep
  • Wyoming

27
Creep
  • Champion, MI

28
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29
Rock Slide and Slumping
  • Point Fermin, CA

30
Group Exercise
  • Identify the following

31
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37
Minimizing Effects
  • Geological mapping to determine active landslides
    and rock types (soil and bedrock), and map sudden
    change in vegetation
  • Develop slope stability maps
  • Develop effective drainage
  • Stabilize slopes
  • Cut and fill method
  • Benching
  • Retaining walls
  • Rock bolts
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