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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Slide 1: Tekstslide
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In deze les zitten 32 slides, met tekstslides en 1 video.

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

Slide 2 - Tekstslide

Slide 3 - Video

Earthquakes in Morocco
Use map 181C in the atlas (GB55):
  1. Which two plates caused the earthquake?
  2. What plate movement do they make?
  3. How many earthquakes above a magnitude                                                            of 6 have been measured in Morocco since 1980?
  4. What is the earthquake risk in Marrakech?
  5. What is the name of the mountain range where the earthquake occurred?
The location of the earthquake is between Marrakech and Agadir

Slide 4 - Tekstslide

What is the plan for today?

FINISH
  •  C3.1: Chile quakes and shakes

Slide 5 - Tekstslide

C3.1: CHILE QUAKES AND SHAKES

Slide 6 - 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 7 - Tekstslide

Slide 8 - Tekstslide

Slide 9 - Tekstslide

Slide 10 - Tekstslide

Slide 11 - Tekstslide

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

Slide 12 - Tekstslide

Slide 13 - Tekstslide

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

Slide 14 - Tekstslide

PLATEMOVEMENTS

Slide 15 - Tekstslide



Situation
in
Chile

Slide 16 - 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 17 - Tekstslide

ANDES

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

Slide 18 - Tekstslide

ANDES
  1. It's the longest subductionzone.
  2. The pressure from the rising magma pushed the horizontal layers of rock sideways and upwards. Creates a fold mountain range.

Slide 19 - Tekstslide

Slide 20 - Tekstslide

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

Slide 21 - Tekstslide

Answer
Young mountain ranges are high with steep slopes (1), sharp peaks (2) and deep valleys (3).
Old mountain ranges have gentle slopes (1) and are round at the top (2). They are also much lower/undeep valleys (3).

Slide 22 - Tekstslide

Young or old?

Slide 23 - Tekstslide

Young or old?

Slide 24 - Tekstslide

Slide 25 - Tekstslide

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

Slide 26 - Tekstslide

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

Slide 27 - Tekstslide

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 28 - Tekstslide

Slide 29 - Tekstslide

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

Slide 30 - 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 the homework for the next lesson!

Slide 31 - Tekstslide

Homework for next lesson

6, 7 & 8 of C3.1

Slide 32 - Tekstslide