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3.2 chile
CHILE
where the Earth stops
C3.2: Chile quakes and shakes
1 / 37
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Slide 1:
Slide
Aardrijkskunde
Middelbare school
vwo
Leerjaar 3
This lesson contains
37 slides
, with
interactive quizzes
,
text slides
and
1 video
.
Lesson duration is:
45 min
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Items in this lesson
CHILE
where the Earth stops
C3.2: Chile quakes and shakes
Slide 1 - Slide
What is the plan for today?
Questions from last week
El nino
C3.2: Chile quakes and shakes
Slide 2 - Slide
Where in Chile do we have these climates?
North
South
Middle
Desertclimate
Seaclimate
Mediaterian climate
Slide 3 - Drag question
Look at this picture. Is this the normal or the el nino situation?
A
El Nino
B
Normale situatie
Slide 4 - Quiz
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 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 - Video
Rules during class
A
maximum
of one person is speaking.
Raise your finger or hand if you want to say something.
Phones are off or quiet and are in your bag
Always bring your books: Coursebook, Geoguide, workbook, notebook & chromebook.
Slide 8 - Slide
C3.1: CHILE QUAKES AND SHAKES
Slide 9 - Slide
LAST WEEKS GOALS
You can
name
the 3 types of movements tectonic plates can make.
You can
explain
the words
epicentre
,
hypocentre
and
seismic
gap
in your own words.
You can
describe
the difference between
continental
and
oceanic
plates.
You can
explain
how
trenches
are formed in a
subduction
zone (GG 68).
You can
explain
in 3 steps how
volcanoes
are formed near a
subduction
zone
.
Slide 10 - Slide
What do you know about earthquakes?
Slide 11 - Mind map
Name the three different plate movements
Slide 12 - Open question
You can
name
the 3 types of movements tectonic plates can make
Slide 13 - Slide
Explain in a sentence how a earthquake occurs
Slide 14 - Open question
Slide 15 - Slide
Slide 16 - Slide
PLATEMOVEMENTS
Slide 17 - Slide
Situation
in
Chile
Slide 18 - Slide
GOALS OF THIS LESSON
You can
give
2
explanations
for the fact that the Andes became so high
You know what the difference between
Horst
and
Grabens.
Slide 19 - Slide
ANDES
1. Give
2 reasons why the Andes became so high.
Read in your book 'The Andes'
Slide 20 - Slide
Give the two reasons
Slide 21 - Open question
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 - Slide
Slide 23 - Slide
Explain in your own words what horst and grabens are
Slide 24 - Open question
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 - Slide
Slide 26 - Slide
Describe
and
explain
the difference
between
old-
and
young mountain ranges
.
Slide 27 - Slide
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.
Slide 28 - Slide
Young or old?
Slide 29 - Slide
Young or old?
Slide 30 - Slide
Slide 31 - Slide
Use G77.
Write down 1 to 4 and add the correct kind of relief.
Slide 32 - Slide
ANSWER
1 – Low mountain range
2 – High mountain range
3 – Lowland / plain
4 – Low mountain range
Slide 33 - Slide
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 34 - Slide
1 – Atacama
2 – (Cordilleras
de los) Andes
3 – Gran Chaco
4 – Serra do Mar /
Serra da Mantiqueira
Slide 35 - Slide
Let's go!
Read the text at page 46/47 in your coursebook.
Do the assignments of section 3.2 ->
1 to 4 + 7 + 8 homework for Thursday 5th december
Rules while working:
You're allowed to work together with your neighbor (WHISPERING).
Slide 36 - Slide
Homework for next lesson
6, 7 & 8 of C3.1
Slide 37 - Slide
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