The structure of the Earth and plate boundaries Cambridge IGCSE Geography (9–1) revision
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In plain words
The ground feels solid and still. It is neither. The Earth's surface is a cracked shell, and its pieces are moving, a few centimetres a year, about as fast as your fingernails grow. Almost every earthquake and volcano happens where two pieces meet.
8 things to know
- The Earth has layers. The inner core is solid iron and nickel, and the hottest part. The outer core is liquid. The mantle is the thickest layer, made of hot rock that can flow slowly. The crust is the thin, solid outer layer.
- The lithosphere is the crust together with the rigid top of the mantle. It is broken into tectonic plates.
- Oceanic crust is thin and dense. Continental crust is thicker and less dense.
- Plates move because of convection currents in the mantle: hot rock rises, spreads and sinks, dragging the plates.
- Divergent (constructive) boundary: two plates move apart, magma rises to fill the gap and makes new crust. There are volcanoes and small earthquakes. Example: the Mid-Atlantic Ridge.
- Convergent (destructive) boundary: an oceanic plate meets a continental plate and is forced beneath it (subduction). There are deep ocean trenches, fold mountains, violent volcanoes and strong earthquakes. Example: the Nazca and South American plates.
- Convergent (collision) boundary: two continental plates meet. Neither sinks, so the crust crumples up into fold mountains. There are earthquakes but no volcanoes. Example: the Himalayas.
- Conservative (transform) boundary: two plates slide past each other. There are earthquakes but no volcanoes. Example: the San Andreas Fault.
Worked example
Explain why there are volcanoes at a destructive plate boundary but not at a collision boundary.
- At a destructive boundary the denser oceanic plate is subducted into the mantle, where it melts.
- The magma formed is less dense than the rock around it, so it rises through the continental plate and erupts.
- At a collision boundary both plates are continental and too light to sink. Nothing is subducted and melted, so there is no magma to erupt.
Tips and tricks
- Learn each boundary with its movement, its hazards and an example. Four boundaries, three facts each.
- Earthquakes happen at every type of boundary. Volcanoes only where magma can reach the surface: divergent and destructive boundaries.
It lands in your notebook with its questions as flashcards.
The structure of the Earth and plate boundaries: 6 questions and answers
These are the quiz’s questions. Do the quiz first, then come back here for the ones that got you.
Which layer of the Earth is liquid?
The inner core is solid because of the enormous pressure.
What is the lithosphere?
It is broken into plates.
At which boundary do plates move apart?
New crust forms in the gap.
At which boundary are there earthquakes but no volcanoes?
The plates slide past each other, and no magma is produced. Collision boundaries are the same.
How were the Himalayas formed?
The crust crumpled upwards into fold mountains.
What is subduction?
The denser oceanic plate sinks into the mantle.
Quiz
6 questions
Tap an answer and you’ll see straight away whether it’s right, and why.
Worksheet
3 questions, 10 marks. Write your answers on paper, then check them.
The structure of the Earth and plate boundaries
Cambridge IGCSE Geography (9–1) 0976 · 10 marks · papermunch.org
Name ______________________________ Date ______________
Describe the layers of the Earth.[4]
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The inner core is solid and very hot. The outer core is liquid. The mantle is a thick layer of hot rock that flows slowly. The crust is the thin, solid outer layer.
Describe what happens at a divergent (constructive) plate boundary.[4]
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Two plates move apart. Magma rises from the mantle to fill the gap. It cools to form new crust. Volcanoes and small earthquakes occur.
Explain why tectonic plates move.[2]
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Convection currents in the mantle: hot rock rises, spreads out and sinks, and this drags the plates above along.
Answers: The structure of the Earth and plate boundaries
- 1. The inner core is solid and very hot. The outer core is liquid. The mantle is a thick layer of hot rock that flows slowly. The crust is the thin, solid outer layer.
- 2. Two plates move apart. Magma rises from the mantle to fill the gap. It cools to form new crust. Volcanoes and small earthquakes occur.
- 3. Convection currents in the mantle: hot rock rises, spreads out and sinks, and this drags the plates above along.



