C3.1 Chile - Lesson 3: Chile quakes and shakes

CHILE
where the Earth stops





C3.1: Chile quakes and shakes
zlb@st-maartenscollege.nl
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time-iconLesduur is: 45 min

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CHILE
where the Earth stops





C3.1: Chile quakes and shakes
zlb@st-maartenscollege.nl

Slide 1 - Tekstslide

What is the plan for today?

FINISH
  •  C3.1: Chile quakes and shakes

Slide 2 - Tekstslide

Rules during class
  1. A maximum of one person is speaking.
  2. Raise your finger or hand if you want to say something.
  3. Phones are off or quiet and are in your bag
  4. Always bring your books: Coursebook, Geoguide, workbook, notebook & chromebook.

Slide 3 - Tekstslide

C3.1: CHILE QUAKES AND SHAKES

Slide 4 - Tekstslide

LAST WEEKS GOALS
  1. You can name the 3 types of movements tectonic plates can make.
  2. You can explain the words epicentre, hypocentre and seismic gap in your own words.
  3. You can describe the difference between continental and oceanic plates.
  4. You can explain how trenches are formed in a subduction zone (GG 68).
  5. You can explain in 3 steps how volcanoes are formed near a subduction zone.


Slide 5 - Tekstslide

You can name the 3 types of movements tectonic plates can make (GG 68).

Slide 6 - Tekstslide

Slide 7 - Tekstslide

You can explain the words epicentre, hypocentre 
and seismic gap in your own words.
                                           (GG 73 + Coursebook)

Slide 8 - Tekstslide

PLATEMOVEMENTS

Slide 9 - Tekstslide



Situation
in
Chile

Slide 10 - Tekstslide

GOALS OF THIS LESSON
  1. You can give 2 explanations for the fact that the Andes became so high (GG 78 + coursebook: ‘The Andes’).
  2. You can describe and explain the difference between young and old mountain ranges (GG 80).
  3. Based on altitude, you can tell what relief type a landscape is (GG 77).
  4. You can name and describe the 5 altitude belts (GG 41).
  5. You can link a cross-section to a map (§1, question 7).





Slide 11 - Tekstslide

ANDES

Give 2 reasons why the Andes became so high.
(G78 + coursebook: 
‘The Andes’).

Slide 12 - Tekstslide

ANDES
  1. It's the longest subductionzone.
  2. The Andes is a fold mountain range.
- Mountains that form when the Earth's crust is crumpled and pushed upwards.

Slide 13 - Tekstslide

Slide 14 - Tekstslide

Describe and explain the difference
between old- and young mountain ranges. (G80)

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Answer
Young mountain ranges are high with steep slopes, sharp peaks and deep valleys.
Old mountain ranges have gentle slopes and are round at the top. They are also much lower.

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Young or old?

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Young or old?

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Use G77. 
Write down 1 to 4 and add the correct kind of relief.

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ANSWER
1 – Low mountain range
2 – High mountain range
3 – Lowland / plain
4 – Low mountain range

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Use map 220 and the general key in the Atlas (55th edition). 
Write down 1 to 4 and add the correct topographical name.
Tip: pay attention to lettertype when selecting a name.

Slide 22 - Tekstslide

1 – Atacama
2 – (Cordilleras 
        de los) Andes
3 – Gran Chaco
4 – Serra do Mar / 
Serra da Mantiqueira

Slide 23 - Tekstslide

Let's go!
  • Read the text at page 40/41 in your coursebook.
  • Make exercises 6, 7 & 8
  • Use G77, G78 & G80

Rules while working:
  • You're allowed to work together with your neighbor (WHISPERING).

This is also the homework for tomorrow!

Slide 24 - Tekstslide

Homework for next lesson

6, 7 & 8 of C3.1

Slide 25 - Tekstslide