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HAZARD #1: EARTHQUAKES




                          7.1 Araucania earthquake (Chile, 2011)


Earthquake: result of a sudden release of energy in the Earth’s crust that creates seismic
waves, followed by smaller aftershocks and potential secondary hazards (ex: tsunamis, industrial
leaks, etc)
SAN ANDREAS FAULT




             1. Describe the crustal movement of
                the San Andreas fault
             2. Explain how this tectonic plate
                boundary different from the one
                near Seattle in its movement and
                geographical manifestation
EARTHQUAKE CHARACTERISTICS: PLATE BOUNDARY TYPES – Find regional examples for each type




Oceanic-Continental convergence
EARTHQUAKE CHARACTERISTICS: FOCUS, EPICENTER, DEPTH, SHOCKWAVES




Shallow focus = ~100 km depth or less
Deep focus = 100-700 km depth

P-waves (primary / push-pull) = felt first (5-8 km/s): feels like a shock wave rattling windows
S-waves (secondary / shake) = felt a few seconds later (3-5 km/s): can be very destructive

Ex 1: Loma Prieta (California 1989): 6.7 magnitude at 18 km depth (inland)
Ex 2: Sendai (Japan 2011): 9.0 magnitude at 32 km depth (70 km the coast)
SOIL LIQUEFACTION DUE TO EARTHQUAKES
Explain factors linked to the high soil liquefaction risk
SECONDARY HAZARDS DUE TO EARTHQUAKES




Tsunami in Japan (2011)                 Mudslide in Taiwan (2010)




                                        Fire in San Francisco (1906)
EARTHQUAKE CHARACTERISTICS: DAMAGE FACTORS

 Explain how each of the following factor can affect the outcome of an earthquake:

 •   Strength and depth of earthquake
 •   Number of aftershocks
 •   Population density
 •   Type of buildings
 •   Time of day
 •   Distance from epicenter
 •   Types of rocks -> risk of liquefaction
 •   Secondary hazards: tsunami, fire, mudslides, famine, epidemic
 •   Development level (linked to preparedness and response)


3 most destructive recent earthquakes
1. Indonesia 2004 (9.1)               250,000 victims (tsunami)
2. Haiti 2010 (7.0)                   230,000 victims
3. Pakistan 2005 (7.6)                86,000 victims
EARTHQUAKE SPATIAL DISTRIBUTION: TECTONIC PLATE BOUNDARIES
                            Most destructive recent earthquakes




CASE STUDIES IN TEXTBOOK:
Comparable strength earthquakes with different outcomes (p.201):
• Kobe (Japan, 1995, 7.2): 5,000 victims
• Kashmir (Pakistan, 2005, 7.6): 86,000 victims

1. Suggest reasons why the Kobe earthquake was so devastating
2. Explain why the Kashmir earthquake was more devastating than the one in Kobe
EARTHQUAKE SPATIAL DISTRIBUTION: THE “RING OF FIRE” ON THE PACIFIC RIM

Convergence (subduction) zones:




 1. Name large four large cities located on the “ring of fire”
 2. Explain why some regions located on the “ring of fire” are more vulnerable to
    earthquake hazards than others
EARTHQUAKE SPATIAL DISTRIBUTION: SEISMIC HAZARD




1. Name a megacity exposed to a high seismic hazard resulting from:
    • Lateral sliding
    • Subduction
2. For one named vulnerable region, explain what factors may increase the seismic hazard

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I.1 Earthquakes

  • 1. HAZARD #1: EARTHQUAKES 7.1 Araucania earthquake (Chile, 2011) Earthquake: result of a sudden release of energy in the Earth’s crust that creates seismic waves, followed by smaller aftershocks and potential secondary hazards (ex: tsunamis, industrial leaks, etc)
  • 2. SAN ANDREAS FAULT 1. Describe the crustal movement of the San Andreas fault 2. Explain how this tectonic plate boundary different from the one near Seattle in its movement and geographical manifestation
  • 3. EARTHQUAKE CHARACTERISTICS: PLATE BOUNDARY TYPES – Find regional examples for each type Oceanic-Continental convergence
  • 4. EARTHQUAKE CHARACTERISTICS: FOCUS, EPICENTER, DEPTH, SHOCKWAVES Shallow focus = ~100 km depth or less Deep focus = 100-700 km depth P-waves (primary / push-pull) = felt first (5-8 km/s): feels like a shock wave rattling windows S-waves (secondary / shake) = felt a few seconds later (3-5 km/s): can be very destructive Ex 1: Loma Prieta (California 1989): 6.7 magnitude at 18 km depth (inland) Ex 2: Sendai (Japan 2011): 9.0 magnitude at 32 km depth (70 km the coast)
  • 5.
  • 6. SOIL LIQUEFACTION DUE TO EARTHQUAKES
  • 7. Explain factors linked to the high soil liquefaction risk
  • 8. SECONDARY HAZARDS DUE TO EARTHQUAKES Tsunami in Japan (2011) Mudslide in Taiwan (2010) Fire in San Francisco (1906)
  • 9. EARTHQUAKE CHARACTERISTICS: DAMAGE FACTORS Explain how each of the following factor can affect the outcome of an earthquake: • Strength and depth of earthquake • Number of aftershocks • Population density • Type of buildings • Time of day • Distance from epicenter • Types of rocks -> risk of liquefaction • Secondary hazards: tsunami, fire, mudslides, famine, epidemic • Development level (linked to preparedness and response) 3 most destructive recent earthquakes 1. Indonesia 2004 (9.1) 250,000 victims (tsunami) 2. Haiti 2010 (7.0) 230,000 victims 3. Pakistan 2005 (7.6) 86,000 victims
  • 10. EARTHQUAKE SPATIAL DISTRIBUTION: TECTONIC PLATE BOUNDARIES Most destructive recent earthquakes CASE STUDIES IN TEXTBOOK: Comparable strength earthquakes with different outcomes (p.201): • Kobe (Japan, 1995, 7.2): 5,000 victims • Kashmir (Pakistan, 2005, 7.6): 86,000 victims 1. Suggest reasons why the Kobe earthquake was so devastating 2. Explain why the Kashmir earthquake was more devastating than the one in Kobe
  • 11. EARTHQUAKE SPATIAL DISTRIBUTION: THE “RING OF FIRE” ON THE PACIFIC RIM Convergence (subduction) zones: 1. Name large four large cities located on the “ring of fire” 2. Explain why some regions located on the “ring of fire” are more vulnerable to earthquake hazards than others
  • 12. EARTHQUAKE SPATIAL DISTRIBUTION: SEISMIC HAZARD 1. Name a megacity exposed to a high seismic hazard resulting from: • Lateral sliding • Subduction 2. For one named vulnerable region, explain what factors may increase the seismic hazard