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3.2 chile
CHILE
where the Earth stops
C3.2: Chile quakes and shakes
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Slide 1:
Diapositive
Aardrijkskunde
Middelbare school
vwo
Leerjaar 3
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CHILE
where the Earth stops
C3.2: Chile quakes and shakes
Slide 1 - Diapositive
What is the plan for today?
Questions from last week
C3.2: Chile trembles
Slide 2 - Diapositive
Where in Chile do we have these climates?
North
South
Middle
Desertclimate
Seaclimate
Mediterranean
Slide 3 - Question de remorquage
During the el nino situation
A
There is a low pressure area near south america
B
There is a high pressure area near south america
C
There is a low pressure area near Australia
Slide 4 - Quiz
Look at this picture. Is this the normal or the el nino situation?
A
El Nino
B
Normal situation
Slide 5 - Quiz
During el nino there are alot of fish in the ocean near south america
A
True
B
False
Slide 6 - Quiz
Slide 7 - Vidéo
What do you remember of know about earthquakes?
Slide 8 - Carte mentale
Name the three different plate movements
Slide 9 - Question ouverte
You can
name
the 3 types of movements tectonic plates can make
Slide 10 - Diapositive
Explain in two steps how an earthquake occurs.
Slide 11 - Question ouverte
Slide 12 - Diapositive
Why does Chile have so many earthquakes? Look at figure 8.
Slide 13 - Question ouverte
Slide 14 - Diapositive
PLATEMOVEMENTS
Slide 15 - Diapositive
Situation
in
Chile
Slide 16 - Diapositive
The end :)
Slide 17 - Diapositive
GOALS OF THIS LESSON
You know what a seismic gap is and how to recognize it.
You can
give
2
explanations
for the fact that the Andes became so high
You know what the difference between
Horst
and
Grabens.
Slide 18 - Diapositive
Seismic gap
1) Where on this map is a seismic gap?
2) Why isn’t there a seismic gap anymore?
Slide 19 - Diapositive
ANDES
1. Give
2 reasons why the Andes became so high.
Read in your book 'The Andes'
Slide 20 - Diapositive
Give the two reasons.
Slide 21 - Question ouverte
ANDES
It's the
longest
subductionzone
.
The Andes is a
fold mountain range
.
- Mountains that form when the Earth's crust is crumpled and pushed upwards.
Slide 22 - Diapositive
Slide 23 - Diapositive
Explain in your own words what horst and grabens are
Slide 24 - Question ouverte
Horst and Graben
Between a fault line a crust can drop down this is called a
Graben
. Another block will be pushed up this is what we call a
Horst
Slide 25 - Diapositive
Slide 26 - Diapositive
Let's go!
Do the assignments of section 3.2 ->
1 to 4 + 7 + 8 homework for Wednesday 3rd december
Finished? Start with reading 3.3, Do assignments 2,4,5,6,7,8.
Rules while working:
You're allowed to work together with your neighbor (WHISPERING).
Slide 27 - Diapositive
Homework for next lesson
6, 7 & 8 of C3.1
Slide 28 - Diapositive
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