Earthquakes: What affects the extent of damage during/after earthquake Flashcards

1
Q

Factors that affect the extent of damage during/after earthquake

A
  • magnitude
  • depth of focus
  • distance from epicentre
  • geology of epicentre (type of soil at epicentre)
  • population density
  • time of occurence
  • level of preparedness of ppl
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2
Q

Magnitude

A
  • higher magnitude, greater damage
  • larger amt of energy released by earthquake
  • Richter Scale used to measure magnitude
  • for each increasing magnitude on Richter Scale, impact of earthquake becomes 10x greater than previous one
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3
Q

Depth of focus

A
  • shallower depth of focus, greater extent of damage of an earthquake
  • becose most seismic waves reach land surface quickly than deep focus earthquake
  • deep-focus vs shallow focus earthquake
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4
Q

Deep-focus earthquake

A

location: occurs between 70 to 700km below earth’s surface
Impact on land: smaller impact, seismic waves take longer time to reach surface, would have lost most of their energy by then

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5
Q

Shallow-focus earthquake

A

location: occurs in upper 70km of earth’s crust

impact on land: greater impact as seismic waves reach land surface more quickly

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6
Q

Distance from epicentre

A
  • closer the place is to epicentre, greater extent of damage of an earthquake
  • places near epicentre receive strongest shock waves
  • e.g. 2011 Christchurch : epicentre few km away from city
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7
Q

Geology of epicentre (type of soil)

A
  • softer/looser/more unconsolidated the soil, greater extent
  • seismic waves are amplified when soil is soft, structures more likely to collapse
  • structures built on saturated and unconsolidated sediments can be affected by liquefaction
  • liquefaction is when ground becomes unstable and saturated soil flows like liquid
  • e.g. 6.3 earthquake Christchurch, many houses and buildings had to be abandoned due to liquefaction after earthquake in 2011
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8
Q

Stable soil to liquefied soil (Liquefaction)

A

stable soil: loosely packed grains of soil held tgt by friction
-pore spaces filled with water
-building stands erect on stable soil
liquefied soil: shaking destabilizes soil by increasing space between grains
-with structure lost, soil flows like liquid

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9
Q

Population density

A
  • refers to no. of ppl per unit area
  • higher the population density, higher chances of ppl being killed or injured during earthquake
  • more people, more deaths
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10
Q

Time of occurrence

A
  • time of day in which earthquake occurs determines where ppl are and what they are doing
  • affect ppl chance of survival
  • e.g. if earthquake occurs at night when ppl are sleeping, higher chance of being trapped in houses, more deaths (not as alert)
  • e.g. more than 24000 ppl died when earthquake occured @1:47am in Sun Moon Lake Region in Taiwan, 1999
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11
Q

Level of preparedness of ppl

A
  • amt of preparation taken by authorities and citizens makes a significant difference to impact of earthquake
  • e.g. evacuation plans, trained rescue workers, earthquake-resistant buildings
  • e.g. Japan (prone to earthquakes due to geographical location) hold drills for earthquakes in both workplaces and schools regularly
  • damage caused by earthquakes more manageable if ppl are btr prepared
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