WEATHERING & MASS WASTING. Weathering Processes Factors Influencing Weathering Processes Physical...

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WEATHERING & MASS WASTING

Transcript of WEATHERING & MASS WASTING. Weathering Processes Factors Influencing Weathering Processes Physical...

Page 1: WEATHERING & MASS WASTING. Weathering Processes Factors Influencing Weathering Processes Physical Weathering Processes –Frost action –Crystallization.

WEATHERING&

MASS WASTING

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Page 3: WEATHERING & MASS WASTING. Weathering Processes Factors Influencing Weathering Processes Physical Weathering Processes –Frost action –Crystallization.

Weathering Processes  

• Factors Influencing Weathering Processes  • Physical Weathering Processes 

– Frost action– Crystallization (salt-crystal growth)– Pressure-release jointing 

• Chemical Weathering Processes  – Hydration and hydrolysis– Oxidation– Carbonation and solution

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Regolith, Soil, and Parent Materials

Figure 10.4

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Physical Weathering

Figure 10.6

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Joint-block Separation

Figure 10.6

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Physical Weathering in

Sandstone

Figure 10.8

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Exfoliation in Granite

Figure 10.9

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Exfoliation in Granite

Figure 10.9

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Exfoliation in Granite

Figure 10.9

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Chemical Weathering

Figure 10.10

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Chemical Weathering

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Spheroidal Weathering

Figure 10.11

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Oxidation in Rock and Soil

Figure 10.12

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Slope Mechanics and Form

Figure 10.3

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Slope Mechanics and Form

Figure 10.3

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Mass Movement Processes  

• Mass Movement Mechanics – The role of slopes 

• Classes of Mass Movements – Falls and avalanches – Landslide– Flow – Creep

• Human-Induced Mass Movements

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Mass Movement Classes

Figure 10.19

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Soil Creep

 

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Soil Creep

Figure 10.23

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Rockfall

Figure 10.7

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Soil Creep, California

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Madison River Landslide

Figure 10.18

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Talus Slopes

Figure 10.20

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Debris Avalanche,

Peru

Figure 10.21

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Yungay, Peru, May 31, 1970

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Colluvium, San Bernardino Mountains, California

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Avalanche Chute, Colorado

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Gros Ventre Slide, Wyoming

Figure 10.22

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Figure 10.24

Scarification

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Karst and Limestone Regions

Figure 10.13

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Karst Topography

Figure 10.14

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Sinkholes

Figure 10.15

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Cavern Features

Figure 10.17

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End of Chapter 10

Elemental Geosystems 5e

Robert W. ChristophersonCharles E. Thomsen

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Mystery or Soil Creep?

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Four Years’ Mass-Wasting, Bosnia

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Four Years’ Mass-Wasting, Bosnia

• 100*40/2 cm2 = 2000 cm2 (4 years)

• = 500 cm2 /year

• Removed from 1 km slope per year = 500 cm2 /100,000 cm= 1 cm/200 yr= 5000 cm (50 m)/m.y. = 50m /m.y.

• A 1-m (100 cm) soil mantle yields 500 cm2 /year, so movement = 500 cm2 /year/100 cm= 5 cm/year

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Mudflows, California

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Urban Planning, San Diego

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Avalanche Chute, Colorado

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Landslide, Mount Saint Helens

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Sherman Glacier, Alaska, March 27, 1964

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Viaont, Italy, October 9, 1963

1800 people died.

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Yungay, Peru, May 31, 1970

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Yungay, Peru, May 31, 1970

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Lituya Bay, Alaska, July 9, 1958

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Lituya Bay, Before and

After

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The Scour Line

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The Highest Wave Ever Recorded