C7.1 Japan - Lesson 4: Country in the Ring of Fire
Natural disasters in
JAPAN
C7.1: Japan: country in the Ring of Fire
zlb@st-maartenscollege.nl
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Slide 1: Tekstslide
AardrijkskundeMiddelbare schoolvwoLeerjaar 1
In deze les zitten 26 slides, met tekstslides.
Lesduur is: 45 min
Onderdelen in deze les
Natural disasters in
JAPAN
C7.1: Japan: country in the Ring of Fire
zlb@st-maartenscollege.nl
Slide 1 - Tekstslide
What's the plan for today?
C7.1: Japan: country in the Ring of Fire
Slide 2 - Tekstslide
YESTERDAYS 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 3 - Tekstslide
You can name the 3 types of movementstectonicplates can make.
Slide 4 - Tekstslide
You can name the 3 types of movementstectonicplates can make.
Transform
Divergent
Convergent
Slide 5 - Tekstslide
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).
Make a drawing in your notebook of the earth that includes the terms above.
Slide 6 - Tekstslide
TERMS
Earth’s crust
Core
Mantle
Magma
Lava
Convection current
Slide 7 - Tekstslide
Slide 8 - Tekstslide
Slide 9 - Tekstslide
Platemovements
Slide 10 - Tekstslide
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).
Slide 11 - Tekstslide
CHECK HOMEWORK
2, 3 & 4
Slide 12 - Tekstslide
Slide 13 - Tekstslide
ENDOGENIC- & EXOGENIC
Slide 14 - Tekstslide
ENDOGENIC FORCES
Change the earth's crust from the inside
EXOGENIC FORCES
Change the earth's crust from the outside
Slide 15 - Tekstslide
Exercise 3
Slide 16 - Tekstslide
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 - Tekstslide
Slide 18 - Tekstslide
Slide 19 - Tekstslide
CONVERGENT PLATE MOVEMENT
Japan:
Continental and oceanic plate
SUBDUCTION
Slide 20 - Tekstslide
You can explain how trenches are formed in a subductionzone.