Cette leçon contient 35 diapositives, avec quiz interactifs et diapositives de texte.
Éléments de cette leçon
Chapter 2.4 7.1 7.2 (review)
Slide 1 - Diapositive
Weather and climate
What is the difference?
Weather is what is happening in the atmosphere at a specific place and time.
Climate is the average weather in a large area during a period of 30 or 40 years.
Slide 2 - Diapositive
Landscapezones are characterized by the vegetation that grows there.
Savannah:
Clusters of trees, grass and shrubs
Tundra:
Moss, grass and shrubs
The vegetation is dependent on precipitation and temperature.
Slide 3 - Diapositive
A diagram of the average temperature and the average precipitation is called a climate chart.
Red line: the average temperature
Blue bars: the average precipitation
Slide 4 - Diapositive
Which climate?
Slide 5 - Diapositive
Which climate?
Slide 6 - Diapositive
Slide 7 - Diapositive
High density
low density
Polar region
New York city
Temperate zone
Slide 8 - Question de remorquage
Earth’s crust is always changing
Natural forces
Exogenic Endogenic
change the Earth’s crust change the Earth's crust
from the outside from the inside
weatering / erosion vulcanos/earthquakes
Slide 9 - Diapositive
Layers of the earth
Crust: layer we live on, solid and very thin. Made of rocks.
Mantle: thickest layer of the earth, liquid but also moveable.
Slide 10 - Diapositive
Layers of the earth
Outer core: liquid also made out of nickel and iron. Cooler around 3000 - 4500 degrees C.
Inner core: solid made out of nickel and iron. Very warm (4000 and 6000 degrees C.)
Slide 11 - Diapositive
We have two types of tectonic plates:
Oceanic plates:
Found under oceans,
thin (up to 10 kilometres) but heavier.
Made of basalt.
Continental plates:
Found under continents,
thick (up to 75 kilometres) but lighter.
Made of granite.
Slide 12 - Diapositive
Three different plate movements
Plates move away from each other = divergent movement
Plates move toward each other = convergent movement
Plates slide alongside each other = transform movement
Slide 13 - Diapositive
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 - Diapositive
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 - Diapositive
convergent
When two continental plates collide with each other :
continental plates (lighter) will push each other up.
--> mountain range
Slide 16 - Diapositive
convergent
When an oceanic plate collide with a continental plate (subduction):
the heavier oceanic plate will sink back in the mantle.
the lighter continental plate will rise up.
--> vulcanos
--> trench
--> mountains
Slide 17 - Diapositive
subduction?
Slide 18 - Diapositive
Ring of fire
Slide 19 - Diapositive
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 20 - Quiz
Inner core
Crust
Mantle
Outer core
Slide 21 - Question de remorquage
Solid
Very thin
Convection current
Liquid
Slide 22 - Question de remorquage
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 23 - Quiz
Divergent
Convergent
Transform
Slide 24 - Question de remorquage
What are the effects of plate movements?
Slide 25 - Diapositive
I =...........................
II=............................
III=............................
IV=............................
Slide 26 - Diapositive
You can explain how a earthquake occurs.
Earth plates slide past each other. Because this is difficult, the tension between the plates is built up. If there is too much tension, the plates will shoot to discharge the tension.
Slide 27 - Diapositive
You can name the difference between a epi- and a hypocentre.
Earthquakes start in the Earth’s crust. The deepest point is called the hypocentre. The point on the Earth’s surface right above the hypocentre is called the epicentre. That is where you feel the worst tremors.
Slide 28 - Diapositive
You can name how the Richter scale works.
"Scale for measuring the force of an earthquake."
Slide 29 - Diapositive
How a tsunami is formed
Slide 30 - Diapositive
G 7 Switching scale level
local scale: local
regional scale: part of a country, province or territory
national scale: country ,
continental scale: continent , Zooming in
global scale: the world .
Zooming out
Slide 31 - Diapositive
Explain how a volcano forms in a subduction zone.
Slide 32 - Question ouverte
Slide 33 - Diapositive
Which scalelevel suits the image?
A
Local
B
continental
C
National
D
regional
Slide 34 - Quiz
Which scale level suits the statement?
The earthquake off the coast of Japan could be felt as far as North America