C7.1 Japan - Lesson 2: Country in the Ring of Fire
雪
Yuki
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Slide 1: Slide
AardrijkskundeMiddelbare schoolvwoLeerjaar 1
This lesson contains 26 slides, with text slides and 1 video.
Lesson duration is: 45 min
Items in this lesson
雪
Yuki
Slide 1 - Slide
Natural disasters in
JAPAN
C7.1: Japan: country in the Ring of Fire
zlb@st-maartenscollege.nl
Slide 2 - Slide
What's the plan for today?
C7.1: Japan: country in the Ring of Fire
Slide 3 - Slide
LAST LESSON'S GOALS
You can give a connection between land use and relief in Japan.
You can explain the difference between endogenic and exogenic forces.
You can name the 3 types of movements tectonic plates can make.
You can name 2 differences between continental and oceanic plates.
You can explain what the Ring of fire is.
Slide 4 - Slide
Slide 5 - Video
You can name the 3 types of movementstectonicplates can make.
Slide 6 - Slide
You can name the 3 types of movementstectonicplates can make.
Transform
Divergent
Convergent
Slide 7 - Slide
TERMS OF C7.1
You can explain these terms in your own words: Earth’s crust, core, mantle, magma, lava, convection current, plates, faults, plate tectonics (GG 66 + 67).
Try to explain them to your neighbour.
Slide 8 - Slide
TERMS
Earth’s crust
Core
Mantle
Magma
Lava
Convection current
Slide 9 - Slide
Slide 10 - Slide
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CHECK HOMEWORK
2, 3, 4 & 5
Slide 12 - Slide
Slide 13 - Slide
ENDOGENIC- & EXOGENIC
Slide 14 - Slide
ENDOGENIC FORCES
Change the earth's crust from the inside
EXOGENIC FORCES
Change the earth's crust from the outside
Slide 15 - Slide
Slide 16 - Slide
TODAYS GOALS
You can explain how trenches are formed in a subductionzone.
You can explain in 3 steps how volcanoes are formed in a subductionzone.
You can explain how a mid-oceanic ridge is formed (GG 68).
You know that volcanism around subductionzones is different than volcanism in mid-oceanicridges.
Slide 17 - Slide
Slide 18 - Slide
Slide 19 - Slide
CONVERGENT PLATE MOVEMENT
Japan:
Continental and oceanic plate
SUBDUCTION
Slide 20 - Slide
You can explain how trenches are formed in a subductionzone.