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