How We Perceive Earthquakes (i.e Intensity)
Intensity
- how we perceive earthquakes (the intensity we feel) depends on several factors…
1. magnitude:
1. lower magnitude = less intense
1. less energy, waves less powerful 2. shorter shaker time 2. distance from epicenter
1. further = less intense
1. seismic waves attenuate (weaken) as they travel 3. duration (how long)
1. shorter = less intense
1. larger earthquakes can have several minutes of shaking 4. foundation (ground) material
1. solid rock = least intense 2. well-compacted sediment = less intense 3. water-saturated sediment = more intense (potential for liquefaction) 5. building structure (building reaction to ground acceleration)
1. in general:
1. brick and concrete = bad 2. wood, steel, and reinforced concrete = good
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