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§5.1: Differences in nature - part 1
Chapter 5: Project Europe
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Chapter 5: Project Europe
Slide 1 - Tekstslide
Test week
Test (2x)
Chapter 5: project Europe
§5.1: Differences in nature
§5.2: Differences in population and culture
§5.3: Differences in climate
Slide 2 - Tekstslide
Today
Introduction
Explanation §5.1
Videoclip
Slide 3 - Tekstslide
Starting assignment
Several places in Europe will be shown
Choose the place where the chance on a natural disaster is the biggest
An event with a natural cause for example volcanic eruption, earthquake, landslide
Slide 4 - Tekstslide
Where is the chance on a
natural disaster
the biggest?
Slide 5 - Tekstslide
Slide 6 - Tekstslide
Slide 7 - Tekstslide
Slide 8 - Tekstslide
Slide 9 - Tekstslide
Slide 10 - Tekstslide
Slide 11 - Tekstslide
Volcanic eruption Iceland 2010
Slide 12 - Tekstslide
Slide 13 - Video
Today
Introduction
Explanation §5.1
Videoclip
Slide 14 - Tekstslide
Learning goals
You can explain the connection between
plate tectonics
and the presence of
natural disasters
in Europe.
You can explain how
volcanoes
are formed.
You know in which European countries you can find volcanoes and can explain why.
You know why the
type of volcanoes
in Italy and Iceland differ.
Slide 15 - Tekstslide
Divergent
Convergent
Transform
Slide 16 - Sleepvraag
Convergent
Divergent
Transform
Slide 17 - Sleepvraag
Plate tectonics
Europe:
volcanoes
and earthquakes
Slide 18 - Tekstslide
timer
0:30
What do you still know about volcanoes?
Slide 19 - Woordweb
Volcanoes
Convergent (continental and oceanic platen)
Divergent (two oceanic plates)
Hotspot
Slide 20 - Tekstslide
1: Subduction zone
(volcanoes on land)
Ocean floor is pushed into mantel
Rock melts, magma is formed
Heated substance lighter than surroundings
Heated substance wants to rise
Pressure too high: eruption
Magma becomes lava and leaves volcano via the crater
Slide 21 - Tekstslide
Stratovolcano
Convergent movement
Oceanic plate and continental plate
Subduction zone
Slide 22 - Tekstslide
Stratovolcano
Slide 23 - Tekstslide
Stratovolcano
Explosive
Steep slopes
Subduction zone
Slide 24 - Tekstslide
2: divergent movement (volcanoes in the ocean)
Two parts of ocean floor move apart
Crack in the Earth’s crust
Filled with hot rock (lava)
Lava comes into contact with water
Lava solidifies
A new piece of ocean floor is formed
Mid-ocean ridge
= sort of stretched out mountain range along the ocean floor
Slide 25 - Tekstslide
Mid oceanic ridge
Divergent movement
Oceanic and oceanic plate
Volcanoes in the oceans can become volcanic islands
Slide 26 - Tekstslide
Shield volcano
Effusive
(not explosive)
Flat slopes (vlakke hellingen)
Divergent movement and hotspots
Slide 27 - Tekstslide
Look at the map. Where in Europe do you find a subduction zone?
Slide 28 - Open vraag
Look at the map. Where in Europe do you find strato volcanoes and where do you find shield volcanoes?
Slide 29 - Open vraag
Volcanoes: Southern Europe (Mediterranean
Sea)
Subduction zone
Convergent movement of a oceanic and continental plate
Strato volcanoes
Explosive, steep slopes
Vesuvius
Slide 30 - Tekstslide
Volcanoes: Iceland
Formed by mid-ocean ridge
Divergent movement of two oceanic plates
Shield volcanoes
Effusive and flat slopes
Slide 31 - Tekstslide
Slide 32 - Kaart
Today
Introduction
Explanation §5.1
Videoclip
Slide 33 - Tekstslide
Slide 34 - Video
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