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# Quick check: plate boundaries and evidence

Year 8 Earth and space · Plate tectonics

<!-- Speaker note: A self-test on divergent, convergent and transform boundaries and the evidence for plate tectonics (AC9S8U03, nodes 3 to 6, taught in class; node 6 a hinge). About 18 minutes (Nodes 3 to 5 4 min each · Evidence 6 min). -->

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## Today

**We are learning to** a few quick questions on what happens where plates move apart, collide and slide past each other, and the evidence that plates move. Taught in class; use this to check yourself.

- I can say what forms at each kind of plate boundary.
- I can explain why earthquakes happen at transform boundaries.
- I can give three lines of evidence for plate tectonics.

<!-- Speaker note: Before class: A Quick check: a few questions on what students should know for AC9S8U03 nodes 3 to 6, which you teach in class. It has no board, no clip and no new teaching, and it is optional, so it never holds up course completion. Set the width with `?width=minimum`, `typical` (default) or `wider`. Use it as a self-test after your teaching, a starter, or revision. The Layers and What moves the plates lessons on screen come first (nodes 1 and 2); these are the boundaries and evidence you teach in class. Students can do one node at a time. Teacher: Do each boundary as a pair: a question and the "I can" line. Teacher: Finish with the Which boundary sort and the evidence sort, then ask for a third line of evidence out loud. -->

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## Why it matters

> Earthquakes, volcanoes, mountains and trenches all happen at the edges of plates. What happens at each kind of edge?

<!-- Speaker note: Your teacher covers the three kinds of plate boundary and the evidence for plate tectonics in class. These questions check the basics. -->

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## What forms

**Two oceanic plates move apart. What forms at the gap?**

- A fold mountain range
- An earthquake zone only, with no new rock
- A deep trench
- A mid-ocean ridge, as magma rises and cools into new crust

* Answer: A mid-ocean ridge, as magma rises and cools into new crust

<!-- Speaker note: Tension lets magma rise into the gap, where it cools into new oceanic crust. Over time this builds a ridge and spreads the seafloor. -->

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## Age of the seafloor

**You collect rock from the seafloor at the ridge and from far away on either side. Where is the rock youngest?**

- At the ridge, getting older with distance
- Far from the ridge, getting younger towards the ridge
- The same age everywhere
- Youngest on one side only

* Answer: At the ridge, getting older with distance

<!-- Speaker note: New crust forms at the ridge and moves away, so the oldest crust is furthest from it. -->

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## Ocean meets continent

**An oceanic plate meets a continental plate. What happens?**

- The plates slide sideways past each other
- The denser oceanic plate sinks beneath the continent (subduction), forming a trench and a line of volcanoes
- Both plates sink equally
- Both plates stop moving

* Answer: The denser oceanic plate sinks beneath the continent (subduction), forming a trench and a line of volcanoes

<!-- Speaker note: Oceanic crust is denser, so it sinks. A deep trench forms at the bend, and melting above the sinking plate feeds a volcanic arc. -->

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## Continent meets continent

**Why does a collision between two continents make mountains rather than subduction?**

- Both are light, buoyant crust, so neither sinks easily and the rock crumples upwards
- The plates stop moving when they meet
- One continent always slides under the other, as ocean crust does
- Continental crust is denser than the mantle, so it sinks

* Answer: Both are light, buoyant crust, so neither sinks easily and the rock crumples upwards

<!-- Speaker note: Continental crust is too light to sink far. The collision squeezes and folds the rock upwards, as in the Himalayas. -->

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## Why earthquakes?

**Two plates slide past each other along a transform boundary. Why do earthquakes happen there?**

- Magma pushes the plates apart
- The plates melt
- The plates stop moving
- The plates stick, stress builds, and the rock suddenly slips and releases it

* Answer: The plates stick, stress builds, and the rock suddenly slips and releases it

<!-- Speaker note: Friction locks the plates for a while. When the stress becomes too great, the rock slips and the energy is released as an earthquake. -->

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## Volcanoes?

**Do transform boundaries have volcanoes?**

- Yes, because of friction
- Usually not, because plates are neither pulling apart nor sinking, so magma does not form
- Yes, many large ones
- Yes, but only in the ocean

* Answer: Usually not, because plates are neither pulling apart nor sinking, so magma does not form

<!-- Speaker note: Volcanoes need magma. Sliding past does not make a gap for magma to rise or push a plate down into the mantle to melt. -->

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## Which boundary?

**Which kind of boundary is it?**

Groups: Divergent · Convergent · Transform

Mid-ocean ridge · Ocean trench · San Andreas Fault in California · Himalayas · East African Rift

* Answer: Mid-ocean ridge → Divergent; Ocean trench → Convergent; San Andreas Fault in California → Transform; Himalayas → Convergent; East African Rift → Divergent

<!-- Speaker note:  -->

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## Evidence or not?

**Is it evidence that the plates have moved?**

Groups: Evidence · Not evidence

The coastlines of South America and Africa fit together · The same fossils on continents now separated by ocean · The seafloor is youngest at the mid-ocean ridges · Earthquakes and volcanoes line up along plate edges · The Moon has craters

* Answer: The coastlines of South America and Africa fit together → Evidence; The same fossils on continents now separated by ocean → Evidence; The seafloor is youngest at the mid-ocean ridges → Evidence; Earthquakes and volcanoes line up along plate edges → Evidence; The Moon has craters → Not evidence

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## The strongest evidence

**Which evidence most strongly shows the seafloor is spreading from ridges?**

- Earthquakes along the ridges
- The pattern of rock ages: young at the ridge, older with distance, the same on both sides
- The size of the oceans
- Coastlines that look alike

* Answer: The pattern of rock ages: young at the ridge, older with distance, the same on both sides

<!-- Speaker note: The matching age pattern on both sides is what spreading predicts, and is hard to explain any other way. -->

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## What each shows

**Match each piece of evidence to what it shows.**

| | |
|---|---|
| `Coastlines of South America and Africa fit` | A. The continents were once joined |
| `The same fossils on continents now far apart` | B. Where plates meet and move against each other |
| `Seafloor youngest at the ridges` | C. The same plants and animals once lived on connected land |
| `Earthquakes and volcanoes in lines` | D. New crust forms at the ridges and spreads outwards |

* Answer: Coastlines of South America and Africa fit → A. The continents were once joined; The same fossils on continents now far apart → C. The same plants and animals once lived on connected land; Seafloor youngest at the ridges → D. New crust forms at the ridges and spreads outwards; Earthquakes and volcanoes in lines → B. Where plates meet and move against each other

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## Exit ticket

**Name the three kinds of plate boundary and one feature of each.**

* Divergent: mid-ocean ridge. Convergent: trench, volcanic arc or fold mountains. Transform: earthquakes along a fault.

<!-- Speaker note: Students answer on paper or a mini whiteboard before the reveal. Anyone who cannot answer needs the main idea again next lesson. Where this leads: Back in class: model the boundaries with trays or modelling clay; plot recent earthquakes and volcanoes on a world map. -->
