Chapter 3: Earthquakes and volcanoes

1 / 53
suivant
Slide 1: Vidéo
AardrijkskundeMiddelbare schoolhavo, vwoLeerjaar 2

Cette leçon contient 53 diapositives, avec quiz interactif, diapositives de texte et 7 vidéos.

time-iconLa durée de la leçon est: 45 min

Éléments de cette leçon

Slide 1 - Vidéo

Slide 2 - Vidéo

What are we going to do?
Introduction 
Explanation chapter 3 §1
Exercises
Learning goals: 
- You know the layers of the Earth
- You know what a tectonic plate is. 
- You understand the difference between an oceanic and a continental tectonic plate. 

Slide 3 - Diapositive

Slide 4 - Diapositive

The Earth
- The inner core is solid and very hot (5200-6200 degrees).
- The outer core is liquid. 
- The mantle is the thickest layer and this layer is solid, but can actually move over very long periods of time. 
- The crust is solid.  

Slide 5 - Diapositive

Tectonic plates
The movement of the tectonic plates is called plate tectonics. 
Places where two plates meet are called plate boundaries

Slide 6 - Diapositive

Exercises
Read paragraph 3.1 (any words you don't understand? let me know). 

Do the exercises 2 to 5. 

Slide 7 - Diapositive

What are we going to do?
Repeat previous content. 
Further explanation of chapter 3 §1
Exercises
Learning goals: 
- You know the layers of the Earth
- You know what a tectonic plate is. 
- You understand the difference between an oceanic and a continental tectonic plate. 

Slide 8 - Diapositive

The Earth
- The inner core is solid and very hot (5200-6200 degrees).
- The outer core is liquid. 
- The mantle is the thickest layer and this layer is solid, but can actually move over very long periods of time. 
- The crust is solid.  

Slide 9 - Diapositive

Slide 10 - Diapositive

Slide 11 - Vidéo

Tectonic plate types
Two different plate types: 
- Oceanic plates
- Continental plates

Slide 12 - Diapositive

Slide 13 - Diapositive

Slide 14 - Diapositive

What are we going to do?
Repeat previous content. 
Further explanation of chapter 3 §2
Exercises
Learning goals: 
- You know the three different kind of plate movements
- You can explain why earth’s tectonic plates move
- You are able to explain the effects of plate movements on the earth's surface. 

Slide 15 - Diapositive

Exercises
Read paragraph 3.2 (any words you don't understand? let me know). 

Do the exercises 5 to 8. 

Slide 16 - Diapositive

Oceanic plate 
Continental plate

Slide 17 - Diapositive

Plate movements
Three different types of plate movements

Divergent plate boundary
Plates move away from each other and create new plate materials (basaltic rock). 

Slide 18 - Diapositive

Mid oceanic ridges from space
(divergent plate boundaries)

Slide 19 - Diapositive

Mid oceanic ridge in Iceland

Slide 20 - Diapositive

Plate movements
Three different types of plate movements

Convergent plate boundary
Folding the land and creating mountains. 

Slide 21 - Diapositive

Plate movements
Three different types of plate movements

Convergent plate boundary. 
Destroying the earth crust and creating volcanoes. 
(subduction)


Slide 22 - Diapositive

Plate movements
Three different types of plate movements

Transform plate boundaries. 
Causing heavy earthquakes. 


Slide 23 - Diapositive

Transform plate boundary

Slide 24 - Diapositive

In conclusion.

Slide 25 - Diapositive

The whole system 

Slide 26 - Diapositive

Exercises
Read paragraph 3.2 
Correct your exercises of paragraph 3.1 
Do the exercises 1 to 4 of paragraph 3.2 

Questions? Let me know!

Slide 27 - Diapositive

What are we going to do?
Repeat previous content. 
Exercise §2
Exercises workbook & correcting them
Learning goals: 
- You know the three different kind of plate movements
- You can explain why earth’s tectonic plates move
- You are able to explain the effects of plate movements on the earth's surface. 

Slide 28 - Diapositive

Slide 29 - Diapositive

Exercise
1. Explain why there are volcanoes in the south of Italy with geographical terms!
Use the atlas and your book as a source for your answer.
2. Give an explanation on why those volcanoes are explosive. Use the two websites, the atlas and your book as a source for your answer.
You may work in duo's. 


Slide 30 - Diapositive

Slide 31 - Lien

Slide 32 - Lien

What are we going to do?
Repeat previous content. 
Discuss §3
Exercises workbook & correcting them
Learning goals: 
- You can explain why an earthquake takes place somehwere. 
- You can describe the effect of earthquakes. 

Slide 33 - Diapositive

In conclusion.

Slide 34 - Diapositive

The whole system 

Slide 35 - Diapositive

Shaking earth
There's tension being build up between 2 plates that move towards each other or across each other. 
That tension releases energy in the form of shockwaves. 
--> this is an earthquake. 

Slide 36 - Diapositive

Slide 37 - Vidéo

Richter scale
The size of an earthquake is measured on the Richter scale. 
If the magnitude (size) of the earthquake is high, it is likely to cause damage. 

Slide 38 - Diapositive

Effects of an earthquake
Aftershocks
Landslides
Liquefaction --> If the soil contains a lot of water, the soil starts to behave like a liquid and buildings and cars can sink into it. 

Slide 39 - Diapositive

Slide 40 - Vidéo

Mercalli
To measure the effects of earthquake we use the Mercalli scale. 

Slide 41 - Diapositive

What are we going to do?
Repeat previous content. 
Discuss §3 & §5
Exercises workbook & correcting them
Learning goals: 
- You are able to explain the forming of a tsunami

- You know the different types of volcanoes and are able to correspond them with the different fault lines. 

Slide 42 - Diapositive

Tsunami's

Slide 43 - Diapositive

What do you know
about volcanoes?

Slide 44 - Carte mentale

Slide 45 - Vidéo

Volcanoes
We find volcanoes at diverging boundaries and subduction boundaries. 

When magma exits the earth it's called an eruption. 

Slide 46 - Diapositive

Composite volcanoes
These volcanoes look like very steep mountains and can be very explosive (violent) volcanoes. 

Usually you'll encouter these volcanoes near subduction zones. 

Slide 47 - Diapositive

Shield volcano

Slide 48 - Diapositive

Secondary effects
Lahars --> Due to the temperature of the hot ash and gas from a volcanic eruption the snow will melt and cause mudflows. 
These mudflows are called: Lahars. 

The eruptions are also able the impact the climate, if it is a large eruption. 

Slide 49 - Diapositive

Slide 50 - Diapositive

Slide 51 - Vidéo

Hot spots
There are also volcanoes that occur at places that are not near any plate boundaries. 

We call these volcanoes hot spots. 

Slide 52 - Diapositive

Get to work!
Finish the exercises of §3 and correct your answers! 

Done? 
Start with paragraph 5. 

Slide 53 - Diapositive