Chapter 7.1 Japan, country in the ring of fire (part 2)
Chapter 7.1
Japan, country in the ring of fire.
(Part 2)
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AardrijkskundeMiddelbare schoolhavoLeerjaar 1
This lesson contains 22 slides, with interactive quizzes, text slides and 3 videos.
Items in this lesson
Chapter 7.1
Japan, country in the ring of fire.
(Part 2)
Slide 1 - Slide
Natural forces change the earth's crust. Natural forces that change the earth's crust from outside are called ......
A
exogenic forces
B
endogenic forses
Slide 2 - Quiz
Exogenic
Endogenic
Erosion
tectonic
plates
Slide 3 - Drag question
Inner core
Crust
Mantle
Outer core
Slide 4 - Drag question
Solid
Very thin
Convection current
Liquid
Slide 5 - Drag question
What causes the magma to flow around in the mantle?
A
The heat in the core of the earth
B
The heat of the sun's rays on the earth
Slide 6 - Quiz
What is the name of the process of circulation of magma in the mantle?
Slide 7 - Open question
What is the difference between lava and magma?
Slide 8 - Slide
Two different earth plates
Oceanic plate (Thin but heavy)
continental plate (Thick but lighter)
Slide 9 - Slide
Tectonic plate types
Oceanic plate
Tectonic plate underneath an ocean.
Quite thin, only up to 10 kilometres.
Type of rock: basalt (heavy)
Continental plate
Tectonic plate that makes up the continents.
Much thicker than oceanic plates, between 35 and 40 kilometres. Underneath large mountains, such as the Himalayas, the crust can even be up to 75 kilometres thick.
Type of rock: granite (lighter than basalt)
Slide 10 - Slide
Tectonic plates of the world
The Netherlands lies on the Eurasian Plate.
This is the plate boundary between the South American Plate and the African Plate.
This is the plate boundary between the Pacific Plate and the North American Plate.
Look at the places where most earthquakes and volcanoes take place. What do you notice?
Slide 11 - Slide
Divergent
Convergent
Transform
Slide 12 - Drag question
What are the effects of plate movements?
Slide 13 - Slide
Transform
* earthshakes
Earth plates slide past each other. That is not gradual, but difficult. Tension is built up. If there is too much tension, the plates will shoot to discharge the tension.
Heavy earthquakes are born.
Slide 14 - Slide
divergent
Two oceanic plates are moving away from eachother.
Because of the high pressure in the
mantle, the magma rise up.
When it comes into contact with
seawater, the magma solidifies.
A mountain range is created on
the sea floor. --> mid-oceanic ridge
Slide 15 - Slide
convergent
When two continental plates collide with each other :
continental plates (lighter) will push each other up.
--> mountain range
Slide 16 - Slide
convergent
When an oceanic plate collide with a continental plate (subduction):
the heavier oceanic plate will sink back in the mantle.