Lesson 3: Plate movement

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Notebook and pen on your desk
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Slide 1: Slide

AardrijkskundeMiddelbare schoolhavoLeerjaar 5

This lesson contains 33 slides, with text slides.

Lesson duration is: 180 min

Items in this lesson

Ready to start

Phone in your bag
Notebook and pen on your desk
Laptop and headphones in your bag (for later use)

timer

3:00

Slide 1 - Slide

1. Startklaar

Bij de start van iedere les verwelkomt de docent de leerlingen bij de ingang van de deur, noemt leerlingen bij naam, maakt oogcontact en besteedt aandacht aan hun welbevinden. De docent geeft het goede voorbeeld en spreekt hoge verwachtingen uit voor het verloop van de les door succescriteria op gewenst gedrag, schooltaal en effectief leren te benoemen. De leerlingen zijn startklaar: ingelogd in LessonUp, telefoons opgeborgen in het Zakkie, en JdW-map op tafel.

5.1 Dynamic Earth: Risks from Below and Above

Learner Profile: Knowledgeable

ATL: Structure information & Make connections between sources

Related concepts: Processes

Key concept: time, place and space

Technology and innovation shape how societies respond to Earth’s processes across time, place, and space.

Global context: Scientific and technical innovation

Individuals & Societies

Slide 2 - Slide

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Today's program

Planner
Review previous lesson
learning objectives lesson 3
Notes + practice
Check Learning objectives
What to expect for FA1

Slide 3 - Slide

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Periode 1

Week 1

Week 2

Week 3

Week 4

Week 5

Week 6

FA1

Week 7

Week 8

Week 9

Week 10

Week 11

Week 12

FA2

Recap

Exams

Slide 4 - Slide

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Review previous lesson

10 statements: are they true or false?

key terms: Geofactors, Continental & Oceanic crust, Lithosphere, Asthenosphere,
Upper & lower Mantle, Inner & outer core, Convection currents, Seismic waves

Key terms: Continental drift (Wegener), Paleomagnetism

Slide 5 - Slide

https://www.nu.nl/klimaat/6303415/al-een-jaar-recordtemperaturen-in-oceanen-tekenen-dat-opwarming-versnelt.html?referrer=https%3A%2F%2Fwww.google.com%2F

Statement 1

The lithosphere consists only out of the oceanic and continental crust

Slide 6 - Slide

false: also upper mantle

Statement 2

The most inner core of the Earth is solid.

Slide 7 - Slide

true

Statement 3

The asthenosphere is solid

Slide 8 - Slide

false: it's soft and flexible.

Statement 4

The waves that scientists study to understand the layers of the Earth are called tectonic waves.

Slide 9 - Slide

false: seismic waves

Statement 5

Primary waves can pass through solids and liquids.

Slide 10 - Slide

true

Statement 6

The theory of continental drift comes from the German Scientist Buys Ballot.

Slide 11 - Slide

False: Wegener

Statement 7

Wegener found 3 evidences for continental drift:

Flora & fauna, Rocks and climate.

Slide 12 - Slide

true

Statement 8

The oceanic crust closest to the oceanic ridge is the oldest.

Slide 13 - Slide

false: it's the youngest

Statement 9

The magnetic north and south pole of the Earth don't change.

Slide 14 - Slide

false: they do change

Statement 10

The parallel patern of magnetic parts in rock on the seafloor are evidence of seafloor spreading.

Slide 15 - Slide

true

Learning objectives

What causes tectonic plates to move?
What are the types of plate movements?

Key terms: Internal heating, Convection currents, Ridge push & Slab pull, Convergent plate, boundaries & Subduction, Divergent plate boundaries, Transform plate boundaries, Rifting

Slide 16 - Slide

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We now understand the evidence of moving plates
(Wegener + Paleomagnetism)

But what causes tectonic plates to move?

Slide 17 - Slide

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Notebook en pen ready?

Slide 18 - Slide

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What causes tectonic plates to move?

Convection currents
due to internal heat
Ridge-push
Slab-pull