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4.3 glaciers
4.3: Glaciers
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Aardrijkskunde
Middelbare school
vmbo t, mavo, havo, vwo
Leerjaar 2
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4.3: Glaciers
Slide 1 - Diapositive
What do you know about glaciers?
Slide 2 - Diapositive
Glacier
A large ice mass, often shaped like a river.
Glaciers are able to move due to gravity
Terminous/snout is the end of a glacier
Slide 3 - Diapositive
Slide 4 - Diapositive
Slide 5 - Diapositive
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Slide 7 - Diapositive
Glaciers usually form in a cirque
Cirque (keteldal)
Slide 8 - Diapositive
Plucking and abrasion
Plucking: A type of erosion in a glacier: the movement of the glacier pulls rocks away. (afbreken)
Abrasion : A type of erosion in a glacier: the glacier scrapes along its bottom and sides. (wrijving)
Slide 9 - Diapositive
Slide 10 - Diapositive
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Slide 12 - Carte
Slide 13 - Vidéo
Off to work
Do 2 first in class. You need an atlas
then 3-5
Slide 14 - Diapositive
Glacial erosional landforms
Slide 15 - Diapositive
Notes
Because of plucking and abrasion, the glaciers forms a valley called a U-Shaped valley
Slide 16 - Diapositive
Slide 17 - Carte
Hanging valley
A valley created by a tributary galcier which hangs above the main valley
Slide 18 - Diapositive
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Depositional landforms
Glaciers do not only erode material. They also carry the eroded rocks and sediments to other places: this is called
deposition
Slide 20 - Diapositive
Slide 21 - Diapositive
Moraines
Slide 22 - Diapositive
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Moraines
A depositional landform formed by glaciers: sediments that have been pushed together.
Slide 24 - Diapositive
Exercise
Pick a glacier in the world.
In which country is your glacier
What is the weight of your glacier
What is there to do for tourist on your glacier
How has the glacier changed over the years
Slide 25 - Diapositive
Off to work
4.3: 6,7,8
Slide 26 - Diapositive
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