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C3.1 Chile - Lesson 3: Chile quakes and shakes
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Aardrijkskunde
Middelbare school
vwo
Leerjaar 3
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Slide 1 - Diapositive
Slide 2 - Diapositive
Slide 3 - Diapositive
Slide 4 - Diapositive
CHILE
where the Earth stops
C3.1: Chile quakes and shakes
zlb@st-maartenscollege.nl
Slide 5 - Diapositive
What is the plan for today?
Start C3.1: Chile quakes and shakes
Slide 6 - Diapositive
C3.1: CHILE QUAKES AND SHAKES
Slide 7 - Diapositive
Slide 8 - Diapositive
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GOALS OF THIS 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 11 - Diapositive
You can
name
the 3 types of movements tectonic plates can make (GG 68).
Slide 12 - Diapositive
Make 1 drawing in your notebook:
You can explain the words
epicentre
,
hypocentre
and
seismic
gap
in your own words.
(GG 73 + Coursebook)
Drawing: Difference between epicentre and hypocentre
Slide 13 - Diapositive
Slide 14 - Diapositive
You can
explain
the words epicentre, hypocentre
and seismic gap in your own words.
(GG 73 + Coursebook)
Seismic gap
a place where no heavy earthquakes have occurred compared with the surrounding areas.
Slide 15 - Diapositive
Differences between a
oceanic
and a
continental
plate
Continental plate:
- Thick, light and mainly
granite
.
Oceanic place:
- Thin, heavy and mainly
basalt
.
Slide 16 - Diapositive
PLATEMOVEMENTS
Slide 17 - Diapositive
You can explain how
trenches
are formed in a
subduction
zone
(GG 68).
Slide 18 - Diapositive
Formation of a
trench
in a
subductionzone
Long, deep and narrow depression
on the ocean floor caused by subduction.
Slide 19 - Diapositive
Slide 20 - Diapositive
You can explain in 3 steps how
volcanoes
are formed near a subduction zone.
Slide 21 - Diapositive
Formation of
volcanoes
in a
subductionzone
1. An oceanic plate dives under a continental plate.
2. Deep inside the earth it's very hot and the plate starts to melt.
3. The
magma
finds a way through
the earth's surface and you have
a
volcano
.
Slide 22 - Diapositive
HORSTS AND
GRABEN
Slide 23 - Diapositive
HORST AND
GRABEN
Open G79 + notebook:
1. Which platemovement
causes this landscape?
2. Explain: How is a Graben
formed?
3. Look for an example of this
landscape in Europe in the
atlas.
Slide 24 - Diapositive
Slide 25 - Diapositive
Situation
in
Chile
Slide 26 - Diapositive
Let's go!
Read the text at page 40/41 in your coursebook.
Make exercises 4 to 6
Use the
atlas
and G77, G78 & G80
Rules while working:
You're allowed to work together with your neighbor (WHISPERING).
This is also the homework for the next lesson!
Slide 27 - Diapositive
Homework for next lesson
Make 1 to 5 of C3.1
Slide 28 - Diapositive
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