Earthquake Effects
Earthquake Effects
Primary Effects
- Short periods of intense ground motion
- Can damage human structures
- “Earthquakes don’t kill people, buildings kill people”
- A few factors determine the amount and intensity of damage done
- Key factor of intensity of damage is the earthquake’s magnitude
- Length is also important (larger earthquakes tend to be longer)
- How buildings are structured and constructed
- Surface materials on which structures are built
- Structures on loose/sedimentary materials usually experience more intense shaking
- Structures on solid rock are generally more stable
- Some structures can be engineered specifically to mitigate earthquake damage
Secondary Effects
- Other processes related to the shaking
- Mountainous areas → landslides (loose rocks/soil break free)
- Wet, low-lying areas → liquefaction (wet soils liquify)
- Especially common in areas of sandy soils
- Ground cracking
- Fire
- Shaking may break gas lines, which catch fire
- Eg. 1906 San Francisco earthquake → wooden buildings survived quake but not fire
- Tsunamis
- Fault movements displace water above the fault
- Waves radiate from epicenter
- Not overly noticeable in middle of ocean, but can wreck coastal areas
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