Earthquakes and volcanoes
The structure of the Earth, plate boundaries, how earthquakes and volcanoes happen, their hazards and how people reduce the risks.
📌 Key points
- The Earth has a solid inner core, liquid outer core, a mantle and a thin crust; the crust and upper mantle are broken into tectonic plates.
- Oceanic crust is thinner and denser than continental crust; when they meet, the oceanic plate is subducted (sinks) beneath the continental plate.
- At constructive (divergent) boundaries plates move apart and magma rises, forming ridges and gentle-sided volcanoes with runny basaltic lava, e.g. the Mid-Atlantic Ridge, which runs through Iceland.
- At destructive (convergent) boundaries an oceanic plate subducts, causing violent earthquakes, explosive volcanoes and fold mountains, e.g. the Nazca plate under the South American plate (the Andes).
- At conservative boundaries plates slide past each other; there are earthquakes but no volcanoes, e.g. the San Andreas Fault between the Pacific and North American plates.
- Where two continental plates collide, rocks are folded upwards into fold mountains, e.g. the Himalayas.
- An earthquake starts at the focus underground; the epicentre is the point on the surface directly above it; magnitude is measured on the Richter scale, where each whole number is 10 times greater in shaking (amplitude).
- Volcanic hazards include lava flows, pyroclastic flows (fast, hot clouds of gas and ash), ash falls and lahars (mudflows); earthquake hazards include building collapse, fires, landslides, liquefaction and tsunamis.
- People live near volcanoes for fertile soils, geothermal energy, minerals and tourism, and in earthquake zones because of jobs, family and the low frequency of large events.
- Risks can be reduced by monitoring volcanoes (seismometers, tiltmeters, gas readings), earthquake-resistant buildings (cross-bracing, deep foundations, shock absorbers), hazard mapping, evacuation plans and drills.
📖 Key terms
- Tectonic plate
- A large section of the Earth's crust and upper mantle that moves slowly.
- Subduction
- The sinking of a denser oceanic plate beneath another plate at a destructive boundary.
- Focus
- The point underground where an earthquake starts.
- Epicentre
- The point on the Earth's surface directly above the focus.
- Magma
- Molten rock below the Earth's surface; it is called lava when it reaches the surface.
- Pyroclastic flow
- A fast-moving current of very hot gas, ash and rock from an erupting volcano.
- Tsunami
- A series of large sea waves caused by an earthquake or eruption under the sea.
- Lahar
- A mudflow of volcanic ash and water.
✏️ Worked example
Earthquake A measured 7.0 and earthquake B measured 5.0 on the Richter scale. How many times greater was the shaking (amplitude) in A than in B?
- The Richter scale is logarithmic: each increase of 1 means 10 times more shaking.
- Difference in magnitude = 7.0 − 5.0 = 2.
- Multiply by 10 for each step: 10 × 10 = 100.
- Answer: earthquake A had 100 times greater shaking than earthquake B.
For 'explain' questions on plate boundaries, give a sequence: plates move (which way) → what happens to the crust (subduction, friction, magma rising) → the result (earthquake, volcano). Name a real example.
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