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C3.1 Chile - Lesson 4: Chile quakes and shakes
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Slide 1:
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Aardrijkskunde
Middelbare school
vwo
Leerjaar 3
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Slide 1 - Diapositive
Slide 2 - Diapositive
CHILE
where the Earth stops
C3.1: Chile quakes and shakes
zlb@st-maartenscollege.nl
Slide 3 - Diapositive
What is the plan for today?
Finish C3.1: Chile quakes and shakes
NEXT LESSON:
THE ROCK CYCLE
Slide 4 - Diapositive
GOALS OF LAST LESSON
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 5 - Diapositive
Differences between a
oceanic
and a
continental
plate
Continental plate:
- Thick, light and mainly
granite
.
Oceanic place:
- Thin, heavy and mainly
basalt
.
Slide 6 - Diapositive
PLATEMOVEMENTS
Slide 7 - Diapositive
You can explain how
trenches
are formed in a
subduction
zone
(GG 68).
Slide 8 - Diapositive
You can explain in 3 steps how
volcanoes
are formed near a subduction zone.
Slide 9 - Diapositive
Formation of
volcanoes
in a
subductionzone
1. Subduction
2. Deep inside the earth ...
3. The
magma
...
Slide 10 - Diapositive
HORSTS AND
GRABEN
Slide 11 - Diapositive
GOALS OF THIS LESSON
You can
give
2
explanations
for the fact that the Andes became so high
(GG 78 + coursebook: ‘The Andes’)
.
You can
describe
and explain the difference between
young
and
old
mountain
ranges
(GG 80).
Based on altitude, you can
tell
what relief type a landscape is (GG 77).
You can
name
and describe the 5 altitude belts (GG 41).
You can
link
a cross-section to a map (§1, question 7).
Slide 12 - Diapositive
We discuss 4 + 5 now
Slide 13 - Diapositive
Slide 14 - Diapositive
Slide 15 - Diapositive
ANDES
Give
2 reasons why the Andes became so high.
(G78 + coursebook:
‘The Andes’).
Slide 16 - Diapositive
ANDES
It's the longest
subductionzone
.
The pressure from the rising magma pushed the horizontal layers of rock sideways and upwards. Creates a
fold mountain range
.
Slide 17 - Diapositive
Slide 18 - Diapositive
Describe
and
explain
the difference
between
old-
and
young mountain ranges
. (G80)
Slide 19 - Diapositive
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).
But..
Why
?
Slide 20 - Diapositive
Slide 21 - Diapositive
Young or old?
Slide 22 - Diapositive
Young or old?
Slide 23 - Diapositive
CHECK EXERCISE 6
Slide 24 - Diapositive
Slide 25 - Diapositive
RE-DO EXERCISE 7
Slide 26 - Diapositive
Slide 27 - Diapositive
Use G77.
Write down 1 to 4 and add the correct type of relief.
Slide 28 - Diapositive
ANSWER
1 – Low mountain range
2 – High mountain range
3 – Lowland / plain
4 – Low mountain range
Slide 29 - Diapositive
Slide 30 - Diapositive
Use map 220 and the general key in the Atlas (55th edition).
Write down 1 to 4 and add the correct topographical name.
This is along the TROPIC OF CAPRICORN!!!
Slide 31 - Diapositive
Slide 32 - Diapositive
1 – Atacama
2 – (Cordilleras
de los) Andes
3 – Gran Chaco
4 – Serra do Mar /
Serra da Mantiqueira
Slide 33 - Diapositive
Slide 34 - Vidéo
Let's go!
Use the GeoGuide
Make exercise 8 of C3.1
Rules while working:
You're allowed to work together with your neighbor (WHISPERING).
Finished?
Work out the list of knowledge and skills of C3.1 in your
notebook
--
or
number your notes!!!
Slide 35 - Diapositive
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