🏗️ Cross bracing
Steel beams are fixed in an X shape across the frame. They stop the building twisting and swaying too far.
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Unlock This CourseWe cannot stop an earthquake or an eruption. But we can reduce the damage they do. Remember from the last lesson that monitoring and prediction give warning, and that early warning systems give a few seconds or minutes. This lesson is about what is done before a hazard strikes so that fewer people are hurt.
There are three groups of methods: protection (making buildings and land safer), planning (deciding where and how people live and what they do in an emergency) and technology (warning devices and apps).
When you evaluate any method, ask four questions: what are its strengths, what are its weaknesses, how much does it cost, and who benefits? A method is sustainable here if it keeps people safe for the long term, can be paid for and maintained by the country itself, and does not harm the environment.
Key terms:
Most earthquake deaths happen because buildings collapse, not because the ground opens up. So the single most useful protection is a building that does not fall down. Engineers use five main ideas.
Steel beams are fixed in an X shape across the frame. They stop the building twisting and swaying too far.
The building sits on layers of rubber and steel, The ground moves, but the building above moves much less.
Rubber dampers take in the energy of the shaking, like the shock absorbers in a car.
A very heavy weight near the top of a tall building swings the opposite way to the sway and cancels it out. Taipei 101 in Taiwan has one.
A fifth idea is a flexible frame. Steel and reinforced concrete bend a little without snapping, so the building sways instead of breaking. Rigid, unreinforced brick or stone walls can crack and fall.
Many older buildings are not safe. Retrofitting adds bracing, stronger foundations or shock absorbers to them. It is cheaper than rebuilding, but it still costs a lot, and each building needs its own survey.
Building codes are legal rules that say how strong new buildings must be. Japan has strict codes that were tightened in 1981, and modern Japanese buildings survive very strong shaking.
A code only works if it is enforced. That means inspectors check the plans and the finished building, and builders are punished for cutting corners. In some countries inspectors are few, corruption is a problem, or poor families build their own homes cheaply. Then the code exists on paper but buildings still collapse.
In 2010 Chile, an MIC with strict, enforced building codes, had an earthquake of magnitude 8.8, one of the strongest ever recorded. About 500 people died. A magnitude 7.0 earthquake in a country with weak building quality can kill far more. The difference is mostly building quality, planning and preparation, not the size of the earthquake.
Planners use hazard maps to decide where to build. Schools, hospitals and homes are kept away from the highest risk areas, such as unstable slopes, soft ground that turns to mud when shaken, river valleys that lahars follow, and low coasts that tsunamis flood. Land in dangerous zones can be used for parks, farming or car parks instead.
Hazard maps also show people which route to take out of danger. Their weakness is that they need detailed scientific survey work, and the land may be very valuable or already crowded with homes, especially in fast-growing cities in LICs.
Lava moves slowly enough that some can be diverted or cooled. In 1973 on Heimaey in Iceland, huge pumps sprayed sea water onto a lava flow. The lava cooled, slowed and the harbour was saved. It was expensive and only works on slow, small flows. Walls and channels can steer lava away from towns, but they cannot stop a large eruption.
Lahars follow river valleys. Engineers build barriers and check dams across the valleys to trap mud and boulders. Channels and dams cost a lot and need to be cleared out regularly, but they protect towns and farmland downstream.
Undersea earthquakes can cause tsunamis. Buoys on the surface connect to sensors on the sea floor that measure the pressure of the water above. If the pressure changes, a tsunami may be passing, and the buoy sends the signal by satellite. Warnings then go out by sirens, radio, television and phone apps. Apps can reach many people at once and cost users little, but they need a phone signal, power and a working warning centre behind them. A warning from a buoy can give minutes or hours, depending on how far the earthquake was. Buoys are expensive to build and maintain, and an earthquake right beside a coast leaves almost no time.
| Approach | Strength | Weakness | Cost |
|---|---|---|---|
| Earthquake-resistant buildings | Stops the main cause of death | Only new or retrofitted buildings are safe | High |
| Hazard maps and land-use planning | Keeps people out of danger for good | Hard in crowded cities | Medium |
| Evacuation plans, drills, education | Cheap and works for everyone | People forget or ignore it | Low |
| Exclusion zones | Removes people from the danger completely | People lose homes and farms and may return | Medium to high (rehousing, compensation) |
| Lava and lahar barriers | Protects towns and farmland | Only works for small flows | High |
| Warning technology | Gives time to move to safety | Too little time near the source | High |
LICs and HICs differ. HICs can afford strong buildings, retrofitting and expensive warning systems, and they can enforce the rules. LICs often have limited money, rapid city growth and many homes built without permission or checks, so they depend more on low-cost methods such as drills, education and evacuation plans, and on help from aid.
A judgement. Safer buildings save the most lives from earthquakes, because buildings cause most deaths. But no single method is enough. The best results come from combining strong buildings, good planning, and well-practised evacuation. For volcanoes, hazard maps and evacuation save most lives, because lava and ash cannot easily be stopped.
Fig. 1.1 shows made-up data for two earthquakes of similar magnitude.
| Feature | City A | City B |
|---|---|---|
| Magnitude | 7.1 | 7.0 |
| Buildings meeting earthquake codes | 90% | 15% |
| Deaths | 40 | 6,000 |
(a) Identify one way a building can be made earthquake-resistant. [1 mark]
(b) Describe how a tsunami warning buoy works. [3 marks]
(c) Suggest why City B had many more deaths than City A. [3 marks]
(d) To what extent can protection and planning reduce the number of deaths from earthquakes? [6 marks]
(a) Cross bracing, base isolators, shock absorbers, counterweights or a flexible frame (1).
(b) Sensors on the sea floor measure the pressure of the water (1). A change in pressure shows that a tsunami may be passing (1). The buoy sends this to a warning centre by satellite so warnings can be sent out (1).
(c) Only 15% of buildings in City B met the codes, so many collapsed (1). In City A 90% did, so most stayed standing (1). City B may also lack enforcement of codes, or have poorer people with less money for safe homes (1).
(d) Level 3 (5-6 marks): protection can reduce deaths a great deal. Strong buildings stop collapse, which causes most deaths, as Fig. 1.1 shows (1). Planning keeps schools and hospitals off the riskiest ground (1). Drills and evacuation plans are cheap (1). However, retrofitting and rebuilding are expensive, so LICs may not afford them (1). Codes only work if they are enforced (1). Protection cannot stop the earthquake, and the biggest events can still cause damage (1). Overall protection and planning can reduce deaths by a large amount, but only when they are paid for, enforced and combined with warning and education, so it is true to a great extent in HICs and less so in LICs (1).
For a "To what extent" question, argue both sides, give a strength, a weakness and the cost of each point, and finish with a clear judgement.