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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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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):
Which two plates caused the earthquake?
What plate movement do they make?
How many earthquakes above a magnitude of 6 have been measured in Morocco since 1980?
What is the earthquake risk in Marrakech?
What is the name of the mountain range where the earthquake occurred?
The location of the earthquake is between Marrakech a
nd
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
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 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
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 17 - Tekstslide
ANDES
Give
2 reasons why the Andes became so high.
(G78 + coursebook:
‘The Andes’).
Slide 18 - Tekstslide
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 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
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