Living with tectonic hazards: prediction, protection and planning
Around a tenth of the world's population lives within reach of an active volcano. That is not carelessness. It is a trade-off, and the job of a geographer is to weigh both sides.
Part of your national curriculum
- Human and physical geography: Understand tectonic processes and hazards, including earthquakes and volcanic activity
- Place knowledge: Understand the physical and human characteristics of an area of the UK and a wider region of the world beyond Europe
Lesson overview
What you'll learn in this lesson
Evaluate why people live in hazardous places and how risk is reduced.
Key learning points
- • Why people stay
- • Prediction
- • Protection
- • Planning and preparedness
This lesson at a glance
- 25 minutes
- 21 parts to scroll through
- 4 quick checks
- Marked quiz at the end
- Gentle pace: short sittings with pauses
Words to know
Scroll down — the lesson carries on below
Watch & discover
Part 1 of 21
Visual introductionPicture this
Living with tectonic hazards: prediction, protection and planning
Around a tenth of the world's population lives within reach of an active volcano. That is not carelessness. It is a trade-off, and the job of a geographer is to weigh both sides.
In a nutshell
Evaluate why people live in hazardous places and how risk is reduced.
Learning cycle
Part 2 of 21
Learning cycle 1 of 2
Part 1 · Why people stay
A short piece of teaching, then a check to make sure it has landed.
Explore the idea
Part 3 of 21
Learn
Why people stay
Volcanic soils are extremely fertile, which supports dense farming on the slopes of Etna or in Java. Geothermal energy heats and powers most of Reykjavik. Tourism brings jobs and money. Minerals such as sulphur, copper and diamonds are mined in tectonic zones. Beyond the benefits, many people simply cannot afford to move, have family and work there, or believe an event is unlikely in their lifetime.
Reset break
Part 4 of 21
Pause
That's sitting 1 of 5 done
Stretch, get a drink, look out of the window. There is no timer and nothing is counting down — your place is saved, so you can come back in five minutes or tomorrow.
Explore the idea
Part 5 of 21
Learn
Prediction
Volcanoes can be monitored and often predicted: seismometers detect rising magma, tiltmeters and satellites measure the bulge of the volcano's flank, and gas sensors pick up increasing sulphur dioxide. That warning allows evacuation. Earthquakes cannot be predicted with useful precision. The best available is a probability forecast for a region over decades, plus seconds-long automated warnings that stop trains and shut off gas once shaking begins.
Quick check
Part 6 of 21
Quick check
Part 7 of 21
Reset break
Part 8 of 21
Pause
That's sitting 2 of 5 done
Stretch, get a drink, look out of the window. There is no timer and nothing is counting down — your place is saved, so you can come back in five minutes or tomorrow.
Learning cycle
Part 9 of 21
Learning cycle 2 of 2
Part 2 · Protection
A short piece of teaching, then a check to make sure it has landed.
Explore the idea
Part 10 of 21
Learn
Protection
Aseismic design uses cross-bracing, deep foundations anchored into bedrock, counterweights or base isolators that let the building move independently of the ground, and automatic shut-off valves. Retrofitting older buildings is expensive but saves the most lives. Against lava and lahars, engineers use diversion channels, barriers and, for smaller flows, water cooling.
Explore the idea
Part 11 of 21
Learn
Planning and preparedness
Hazard maps keep hospitals, schools and fuel depots off the highest risk ground. Drills, such as Japan's annual national exercise, mean people act automatically. Emergency supplies, insurance, evacuation routes and clear public information turn a disaster into a manageable emergency. Planning is usually the cheapest of the three and gives the best value per pound spent, which is a strong evaluation point.
Reset break
Part 12 of 21
Pause
That's sitting 3 of 5 done
Stretch, get a drink, look out of the window. There is no timer and nothing is counting down — your place is saved, so you can come back in five minutes or tomorrow.
Quick check
Part 13 of 21
Quick check
Part 14 of 21
Quick check
Which measure gives the best protection per pound in a lower income country?
Explore the idea
Part 15 of 21
Worked example
Worked answer: 'Prediction is the most effective way to reduce the effects of tectonic hazards.' Evaluate (9 marks)
Argue for: volcanic prediction genuinely works, and monitoring plus timely evacuation has saved thousands of lives, so where the hazard is a volcano prediction is powerful. Argue against: earthquakes cannot be predicted, so in the world's most densely populated seismic cities prediction offers almost nothing, and warning is only useful if people have somewhere to go. Compare: protection through aseismic building saves lives in every earthquake without any warning, and planning through drills and hazard maps is cheap enough for lower income countries to afford. Conclude with a judgement that is conditional: prediction is most effective for volcanoes, but for earthquakes a combination of building design and preparedness saves far more lives, so the statement is only partly true.
Reset break
Part 16 of 21
Pause
That's sitting 4 of 5 done
Stretch, get a drink, look out of the window. There is no timer and nothing is counting down — your place is saved, so you can come back in five minutes or tomorrow.
Challenge round
Part 17 of 21
Game · Sort it
Which of these are true?
Drag each card into the right column. Tap a card first if dragging is fiddly.
True
Not true
Challenge round
Part 18 of 21
Game · Fill the gaps
Finish the sentences
Choose the word that belongs in each gap.
Beyond the benefits, many ____ simply cannot afford to move, have family and work there, or believe an event is unlikely in their lifetime.
Challenge round
Part 19 of 21
Game · Recall cards
Why can oceanic crust sink beneath continental crust?
Card 1 of 4
Mastery quiz
Part 20 of 21
Marked quiz
End of lesson quiz: Living with tectonic hazards: prediction, protection and planning
4 questions, marked with the reasoning shown. No timer.
1. Why can oceanic crust sink beneath continental crust?
2. Which is the strongest single piece of evidence for sea-floor spreading?
3. What does slab pull describe?
4. Why is Hawaii volcanic despite sitting far from a plate margin?
Lesson round-up
Part 21 of 21
Lesson round-up
Ready when you are
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Ask LunaPart 1 of 21 · Watch & discover
How this is going
- Not looked at yet
Understand tectonic processes and hazards, including earthquakes and volcanic activity
- Not looked at yet
Understand the physical and human characteristics of an area of the UK and a wider region of the world beyond Europe
