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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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Lesson duration is:
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4.3: Glaciers
Slide 1 - Slide
What do you know about glaciers?
Slide 2 - Slide
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 - Slide
Slide 4 - Slide
Slide 5 - Slide
Slide 6 - Slide
Slide 7 - Slide
Glaciers usually form in a cirque
Cirque (keteldal)
Slide 8 - Slide
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 - Slide
Slide 10 - Slide
Slide 11 - Slide
Slide 12 - Map
Slide 13 - Video
Off to work
Do 2 first in class. You need an atlas
then 3-5
Slide 14 - Slide
Glacial erosional landforms
Slide 15 - Slide
Notes
Because of plucking and abrasion, the glaciers forms a valley called a U-Shaped valley
Slide 16 - Slide
Slide 17 - Map
Hanging valley
A valley created by a tributary galcier which hangs above the main valley
Slide 18 - Slide
Slide 19 - Slide
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 - Slide
Slide 21 - Slide
Moraines
Slide 22 - Slide
Slide 23 - Slide
Moraines
A depositional landform formed by glaciers: sediments that have been pushed together.
Slide 24 - Slide
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 - Slide
Off to work
4.3: 6,7,8
Slide 26 - Slide
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