Earthquakes: What affects the extent of damage during/after earthquake Flashcards
Factors that affect the extent of damage during/after earthquake
- 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
Magnitude
- 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
Depth of focus
- 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
Deep-focus earthquake
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
Shallow-focus earthquake
location: occurs in upper 70km of earth’s crust
impact on land: greater impact as seismic waves reach land surface more quickly
Distance from epicentre
- 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
Geology of epicentre (type of soil)
- 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
Stable soil to liquefied soil (Liquefaction)
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
Population density
- 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
Time of occurrence
- 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
Level of preparedness of ppl
- 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