C3.1 Chile - Lesson 3: Chile quakes and shakes

1 / 28
next
Slide 1: Slide
AardrijkskundeMiddelbare schoolvwoLeerjaar 3

This lesson contains 28 slides, with text slides.

time-iconLesson duration is: 45 min

Items in this lesson

Slide 1 - Slide

Slide 2 - Slide

Slide 3 - Slide

Slide 4 - Slide

CHILE
where the Earth stops





C3.1: Chile quakes and shakes
zlb@st-maartenscollege.nl

Slide 5 - Slide

What is the plan for today?


  • Start C3.1: Chile quakes and shakes

Slide 6 - Slide

C3.1: CHILE QUAKES AND SHAKES

Slide 7 - Slide

Slide 8 - Slide

Slide 9 - Slide

Slide 10 - Slide

GOALS OF THIS LESSON
  1. You can name the 3 types of movements tectonic plates can make.
  2. You can explain the words epicentre, hypocentre and seismic gap in your own words.
  3. You can describe the difference between continental and oceanic plates.
  4. You can explain how trenches are formed in a subduction zone (GG 68).
  5. You can explain in 3 steps how volcanoes are formed near a subduction zone.


Slide 11 - Slide

You can name the 3 types of movements tectonic plates can make (GG 68).

Slide 12 - Slide

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 - Slide

Slide 14 - Slide

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 - Slide

Differences between a oceanic and a continental plate
Continental plate:
- Thick, light and mainly
   granite.

Oceanic place:
- Thin, heavy and mainly
   basalt.

Slide 16 - Slide

PLATEMOVEMENTS

Slide 17 - Slide

You can explain how trenches are formed in a subduction zone (GG 68).

Slide 18 - Slide

Formation of a trench
in a subductionzone
Long, deep and narrow depression
on the ocean floor caused by subduction.

Slide 19 - Slide

Slide 20 - Slide

You can explain in 3 steps how volcanoes are formed near a subduction zone.

Slide 21 - Slide

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 - Slide

HORSTS AND GRABEN

Slide 23 - Slide

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 - Slide

Slide 25 - Slide



Situation
in
Chile

Slide 26 - Slide

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 - Slide

Homework for next lesson

Make 1 to 5 of C3.1

Slide 28 - Slide