---
marp: true
theme: default
html: true
---

# What moves the plates?

Year 8 Earth and space · Plate tectonics

<!-- Speaker note: Students explain that the lithosphere is divided into moving plates and describe mantle convection, driven by Earth's inner heat (from the core and from radioactive decay in the mantle), as the mechanism (AC9S8U03, node 2, a hinge node). About 25 minutes (Engage and Explore 9 min · Explain 10 min · Evaluate 3 min · Typical adds 4 min, Wider about 5 min). -->

---

## Today

**We are learning to** the lithosphere is broken into rigid plates that move a few centimetres a year. Slow convection currents in the hot mantle carry them, driven by Earth's inner heat: from the core below and from radioactive elements in the mantle rock itself.

- I can explain that the lithosphere is divided into plates that move.
- I can describe mantle convection as the mechanism that moves the plates.
- I can state that plates move a few centimetres a year.

<!-- Speaker note: Before class: A concept tutorial for introducing or revising the idea; it does not replace a convection demonstration. Set the width with `?width=minimum`, `typical` (default) or `wider`. The hinge risk is plate movement with no mechanism: without convection, boundary features (nodes 3 to 5) look arbitrary. Assumed: convection, and density from Year 7 (less dense rises). These tutorials teach convection in Year 9 (Heat transfer), so Explore opens with a one-question recap (warm fluid rises because it is less dense). If the class has not met convection, demonstrate it first (see In class, below). Model notes, worth saying aloud: the board draws the mantle as moving particles, but the real mantle is solid rock that flows over millions of years. In the model hot particles are pushed up directly; real hot rock rises because it is less dense. The plates on top move with the surface flow. Teacher: In your own words: the six-word paragraph is the node's checkpoint. -->

---

## Why it matters

> Australia is moving north about 7 centimetres a year, nearly twice as fast as your fingernails grow. A whole continent. What could possibly push it?

<!-- Speaker note: Earth's surface is not fixed. This lesson is about the engine underneath. -->

---

<span style="background:#dbeafe; color:#1a1a1a; border:1.5px solid #3b82f6; padding:6px 18px; border-radius:8px; font-size:1em; font-weight:500;">💬 Discussion</span>

## Engage: predict

**Earth's surface is broken into huge plates that move a few centimetres a year. What do you predict moves them?**

- The pull of the Moon
- Earthquakes pushing them along
- Slow currents in the hot rock below them
- Ocean currents and waves

<!-- Speaker note: What happens: Slow currents in the hot mantle below: heated rock rises, spreads under the plates, cools and sinks, carrying the plates with it. The heat comes from the core below and from radioactive elements in the mantle rock. Take two or three predictions before anyone runs it. -->

<!-- Speaker note: Teacher: a quick hands-up for each option; 'earthquakes' is common and gets fixed in Explain. -->

---

<span style="background:#fef3c7; color:#1a1a1a; border:1.5px solid #f59e0b; padding:6px 18px; border-radius:8px; font-size:1em; font-weight:500;">✍️ Activity</span>

## Explore it

{{embed: https://studio.learningwaypoints.com/tutorials/_playground-science/index.html?id=deck%2Fscience%2Fearth-8%2Fplates%2Fstep-2&code=widget%3A+convection%0Apreset%3A+mantle%0A}}

[Open this step in the tutorial](https://studio.learningwaypoints.com/tutorials/science/earth-8/plates/?full=step-2#step-2)

<!-- Speaker note:  -->

<!-- Speaker note: Teacher: ask students to describe the ringed particle's whole path in four words (heated, rises, cools, sinks). -->

<style scoped>pre, marp-pre { font-size: 0.5em; line-height: 1.25; } section { font-size: 25px; }</style>

---

<span style="background:#dcfce7; color:#1a1a1a; border:1.5px solid #22c55e; padding:6px 18px; border-radius:8px; font-size:1em; font-weight:500;">✅ Check</span>

## What happened?

* Slow currents in the hot mantle below: heated rock rises, spreads under the plates, cools and sinks, carrying the plates with it. The heat comes from the core below and from radioactive elements in the mantle rock.

<!-- Speaker note: Reveal after running. Ask who predicted it, and what made them think so. -->

---

<span style="background:#dcfce7; color:#1a1a1a; border:1.5px solid #22c55e; padding:6px 18px; border-radius:8px; font-size:1em; font-weight:500;">✅ Check</span>

## The layers

**Put each description with its part of the Earth.**

Groups: Lithosphere (the plates) · Mantle · Core

Rigid pieces that move a few centimetres a year · Hot solid rock that flows very slowly · Heats the mantle from below · Also heated from within, by radioactive elements in its rock · Where the convection currents are · The crust and the top of the mantle

* Answer: Rigid pieces that move a few centimetres a year → Lithosphere (the plates); Hot solid rock that flows very slowly → Mantle; Heats the mantle from below → Core; Also heated from within, by radioactive elements in its rock → Mantle; Where the convection currents are → Mantle; The crust and the top of the mantle → Lithosphere (the plates)

<!-- Speaker note:  -->

<!-- Speaker note: Teacher: the 'why rock rises' question targets 'heat rises'. The number check gives the scale. -->

<style scoped>pre, marp-pre { font-size: 0.5em; line-height: 1.25; } section { font-size: 21px; }</style>

---

<span style="background:#dcfce7; color:#1a1a1a; border:1.5px solid #22c55e; padding:6px 18px; border-radius:8px; font-size:1em; font-weight:500;">✅ Check</span>

## Why rock rises

**Why does hot rock above the core rise?**

- Hot things always go up because heat rises
- It is less dense than the cooler rock around it
- The core pushes it out
- It has melted into liquid magma, which floats up

* Answer: It is less dense than the cooler rock around it

<!-- Speaker note: Heated rock expands a little, so it is less dense and rises. Cooled rock is denser and sinks. -->

---

<span style="background:#dcfce7; color:#1a1a1a; border:1.5px solid #22c55e; padding:6px 18px; border-radius:8px; font-size:1em; font-weight:500;">✅ Check</span>

## Plates move apart

**On the board, where did the two plates move apart?**

- Above the sinking currents
- Above the rising current
- Where the board was coolest

* Answer: Above the rising current

<!-- Speaker note: Rising rock spreads out sideways under the plates, dragging them apart. This is a divergent boundary, like the Mid-Atlantic Ridge. -->

---

<span style="background:#dcfce7; color:#1a1a1a; border:1.5px solid #22c55e; padding:6px 18px; border-radius:8px; font-size:1em; font-weight:500;">✅ Check</span>

## How fast

**Australia moves about 7 cm north each year. How many kilometres is that in a million years? (100,000 cm = 1 km)**

* Answer: 70

<!-- Speaker note: 7 cm × 1,000,000 = 7,000,000 cm = 70 km. Slow, but over 50 million years that is 3,500 km. -->

---

<span style="background:#fef3c7; color:#1a1a1a; border:1.5px solid #f59e0b; padding:6px 18px; border-radius:8px; font-size:1em; font-weight:500;">✍️ Activity</span>

## Elaborate: the same idea in water

{{embed: https://studio.learningwaypoints.com/tutorials/_playground-science/index.html?id=deck%2Fscience%2Fearth-8%2Fplates%2Fstep-4&code=widget%3A+convection%0A}}

[Open this step in the tutorial](https://studio.learningwaypoints.com/tutorials/science/earth-8/plates/?full=step-4#step-4)

<!-- Speaker note: What this step is for: Seeing the same mechanism in a familiar fluid shows convection is general, and makes the mantle's difference (solid, very slow) stand out. -->

<style scoped>pre, marp-pre { font-size: 0.5em; line-height: 1.25; } section { font-size: 25px; }</style>

---

<span style="background:#dcfce7; color:#1a1a1a; border:1.5px solid #22c55e; padding:6px 18px; border-radius:8px; font-size:1em; font-weight:500;">✅ Check</span>

## Water and rock

**What is the biggest difference between the water and the mantle?**

- Mantle rock is solid and flows millions of times more slowly
- Mantle rock rises when it cools
- There is no heat source under the mantle

* Answer: Mantle rock is solid and flows millions of times more slowly

<!-- Speaker note: The mechanism is the same; the timescale is not. A loop in the beaker takes seconds; in the mantle, tens of millions of years. -->

---

<span style="background:#dcfce7; color:#1a1a1a; border:1.5px solid #22c55e; padding:6px 18px; border-radius:8px; font-size:1em; font-weight:500;">✅ Check</span>

## Three forces

**Match each force to how it moves a plate.**

| | |
|---|---|
| `Slab pull` | A. A plate slides away, downhill, from a high mid-ocean ridge |
| `Ridge push` | B. Flowing mantle carries the plate above it along |
| `Mantle drag` | C. Old, cold, dense plate sinks into the mantle and drags the rest of the plate behind it |

* Answer: Slab pull → C. Old, cold, dense plate sinks into the mantle and drags the rest of the plate behind it; Ridge push → A. A plate slides away, downhill, from a high mid-ocean ridge; Mantle drag → B. Flowing mantle carries the plate above it along

<!-- Speaker note:  -->

<style scoped>pre, marp-pre { font-size: 0.5em; line-height: 1.25; } section { font-size: 19px; }</style>

---

<span style="background:#dcfce7; color:#1a1a1a; border:1.5px solid #22c55e; padding:6px 18px; border-radius:8px; font-size:1em; font-weight:500;">✅ Check</span>

## Which matters most?

**The fastest plates (like the Pacific plate) are the ones with long edges sinking into the mantle. Which force does that suggest matters most?**

- Neither: plate speed is random
- Slab pull
- Ridge push

* Answer: Slab pull

<!-- Speaker note: Most geologists now think slab pull is the biggest force. All three are parts of the same convection system. -->

---

## Evaluate: look back

Write one sentence: "At first I thought… Now I think… because…"

**Revision summary**

- The **lithosphere** (crust and top of the mantle) is broken into rigid **tectonic plates**, moving a few centimetres a year.
- Earth's inner heat (from the **core** below, and from radioactive elements in the mantle rock) drives **convection currents** in the **mantle**: hot rock is less dense and rises, spreads, cools and sinks.
- The currents carry the plates: apart above rising rock, together above sinking rock.
- The mantle is solid rock that flows extremely slowly, not liquid magma.

<style scoped>pre, marp-pre { font-size: 0.5em; line-height: 1.25; } section { font-size: 23px; }</style>

---

<span style="background:#dcfce7; color:#1a1a1a; border:1.5px solid #22c55e; padding:6px 18px; border-radius:8px; font-size:1em; font-weight:500;">✅ Check</span>

## Exit ticket

**What drives the movement of tectonic plates?**

* Convection currents in the mantle: heated rock rises, spreads, cools and sinks, carrying the plates. The heat comes from the core and from radioactive elements in the mantle.

<!-- 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: Next: what happens where plates meet: divergent (node 3), convergent (node 4) and transform (node 5) boundaries. In class: a beaker of water heated from one side with a few potassium permanganate crystals or food colouring, and a raft of paper on top. -->
