Geography

Volcanoes and plate tectonics

Review the Earth’s layers, volcano structure and three plate-boundary types, then use a retrieval quiz to recall key ideas. The organiser combines concise notes, vocabulary and examples with a self-check. Review diagrams with your class.

Read the parts of a composite volcano, then compare what happens at different plate boundaries.

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Volcanoes and plate tectonics

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Page 1

1
Layers of the Earth
1
2
3
4
1
Crust: thin and solid; thicker under
continents than under oceans.
2
Mantle: the thickest layer; mostly solid
rock that flows very slowly.
3
Outer core: liquid iron and nickel.
4
Inner core: solid iron and nickel.
Not to scale: the crust is drawn thicker.
2
Inside a composite volcano
ash cloud
main vent
magma chamber
crater
secondary
(side) vent
layers of
ash and lava
3
Plate boundaries: where two plates meet
oceanic
continental
Convergent
destructive
Plates move towards each other. The
denser oceanic plate sinks under the
other (subduction) and magma rises.
BRINGS composite volcanoes,
earthquakes
E.G. Mount St Helens, USA
magma rises
Divergent
constructive
Plates move apart. Magma rises to fill
the gap, then cools and hardens to
make new crust.
BRINGS shield volcanoes, ocean
ridges
E.G. Iceland (Mid-Atlantic Ridge)
seen from above
Conservative
or transform
Plates slide past each other. No
magma rises, so no volcanoes. Plates
stick, then slip suddenly.
BRINGS earthquakes, but no
volcanoes
E.G. San Andreas Fault, USA
4
Key vocabulary
crust the thin, solid outer layer of the
Earth.
mantle the thickest layer: mostly solid
rock that flows very slowly.
tectonic plate a huge, slowly moving slab
of crust and upper mantle.
magma molten (melted) rock below the
Earth's surface.
plate boundary the place where two
tectonic plates meet.
convergent (destructive) plates move
towards each other.
divergent (constructive) plates move
apart; magma fills the gap.
conservative plates slide past each other;
crust is not made or destroyed.
lava molten rock that has reached the
Earth's surface.
composite volcano 
 steep; layers of
ash and thick (viscous) lava; explosive.
shield volcano 
 gentle slopes, runny
(low-viscosity) lava, gentle eruptions.
pyroclastic flow a fast-moving current of
hot gas, ash and rock fragments that
rushes down the side of a volcano.
5
Key facts
6
Famous eruptions
Topic knowledge organiser · Geography · Volcanoes and plate tectonics
GEOGRAPHY
AGES 11 TO 14
KNOWLEDGE ORGANISER
Volcanoes and plate tectonics
Most volcanoes and earthquakes are at plate
boundaries.
Plates move a few centimetres a year, about as fast as
your fingernails grow.
The core is metal, not lava; the mantle is not a sea of
magma.
Mauna Loa, Hawaii, is a shield volcano over a hotspot in
the middle of a plate.
AD 79
Vesuvius, Italy: buried the Roman towns of
Pompeii and Herculaneum.
1883
Krakatoa, Indonesia: a huge explosion and
deadly tsunamis.
18 May 1980
Mount St Helens, USA: a huge landslide, then a
sideways blast.
2010
Eyjafjallajökull, Iceland: its ash cloud
disrupted air travel across Europe.
Page 1 of 2

Page 2

NAME
CLASS
DATE
LEARNING GOAL
I can recall and explain the key ideas about
plate tectonics and volcanoes.
SUCCESS CRITERIA
I can define key words such as magma and lava.
I can explain the three types of plate boundary.
I can label and compare volcanoes.
1
/2
Magma and lava: what is the difference?
2
/1
Name the four layers, from the outside in.
1
2
3
4
3
/2
True or false? "The mantle is a sea of liquid magma."
Circle, then correct it. 
True
False
4
/1
How fast do plates move? Give a comparison.
5
/2
Convergent boundary: which plate sinks? Why?
6
/2
Divergent boundary: what happens? Name a place.
7
/2
Conservative boundary: why are there no volcanoes?
8
/2
Give two differences: composite vs shield.
9
/2
What is a pyroclastic flow? Why is it deadly?
10
/2
Number 1 to 4, earliest first. Circle the eruption that
disrupted air travel across Europe.
Krakatoa
Mount St Helens
Vesuvius
Eyjafjallajökull
11
Label the composite volcano
6 marks
A
B
C
D
E
F
A
B
C
D
E
F
PEEK LAST
crater
magma chamber
ash cloud
layers of ash and
lava
main vent
secondary vent
GO FURTHER Why does Iceland have volcanoes, but the San Andreas Fault has none?
Self-quiz · My score: 
 / 24
Not yet
Getting there
Got it
VOLCANOES AND PLATE TECTONICS
SELF-QUIZ
Cover, recall, check
Cover page 1. Recall from memory. Check and correct in a new colour.
Page 2 of 2

A teaching sequence

Recall and explain vocabulary, Earth structure, plate-boundary processes and differences between composite and shield volcanoes using the organiser as a study aid.

Read the parts of a composite volcano, then compare what happens at different plate boundaries.

Read the complete material

Review diagrams, movement and key terms

Use the labelled Earth layers and composite-volcano diagram to review structure and key terms. Compare convergent, divergent and conservative boundaries by movement and the features the organiser associates with each.

How do the labelled structures and boundary movements connect?

Study examples before covering the organiser

Study the selected eruption examples and vocabulary, then cover the notes.

Which place or term needs a subject-teacher clarification?

Recall definitions, comparisons and labels

Answer the second-page prompts from memory, including definitions, comparisons and diagram labels.

Can you answer without copying from the covered notes?

Check and explain one misconception

Check responses against reviewed notes, correct inaccuracies in another colour and explain one misconception in the pupil’s own words. Ask about any example that needs clarification before discussion.

Which reviewed detail supports the correction in your own words?

Before you teach

Look for the thinking behind an answer, choose the support your class needs and leave room for an independent response.

What to look for

Ask pupils to distinguish magma from lava, explain how plates move at each boundary and connect a named example to the process. Check volcano labels and historical claims against a trusted course source before using them as assessed facts. Ask pupils to explain their reasoning.

Give a little support

Preteach a small group of key terms with diagrams or physical models. Offer the organiser in sections, read prompts aloud and let pupils answer orally before writing. Pair new vocabulary with labelled pictures.

Take the idea further

Ask pupils to compare two boundary settings using a labelled sketch, or to investigate how a specific eruption affected people and places using a reliable source beyond the organiser. Invite them to distinguish evidence from explanation.

Things to keep in mind

The notes simplify dynamic Earth processes and give selected examples rather than a complete geography course. Check scientific terms, place names, dates and the intended curriculum before use; this resource is not an independently verified answer key.

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Ideas to try with your class

Sample teaching perspectives on what to try, what to adapt and what to watch for.

📝

Margin Note

This two-page volcanoes organiser reviews Earth's crust, mantle and cores, labels a composite volcano and contrasts plate boundaries and volcano types. It states that the layer diagram is not to scale and the crust is drawn thicker.

✏️

Spare Pencil

The organiser combines vocabulary, labelled diagrams and recall prompts, helping pupils connect Earth's structure to plate processes and volcano form. The scale disclaimer makes clear that the picture is a learning model.

📎

Paperclip Perspective

Cover labels and ask pupils to retrieve each term, then reveal them for checking. Compare the composite-volcano diagram with the stated features of shield volcanoes using the page's vocabulary.

🤔

One More Question

The diagrams simplify Earth's structure and volcanic systems. Check definitions against the course material and keep the not-to-scale warning visible when pupils interpret relative size.

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