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Paragraph 2.2: Rivers of ice
2.2: Rivers of Ice (glaciers)
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Aardrijkskunde
Middelbare school
vwo
Leerjaar 2
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2.2: Rivers of Ice (glaciers)
Slide 1 - Tekstslide
At the end of this lesson you will know
how glaciers erode and build landscape
Language aim:
you can explain the outline of a glacier with the words lateral morene/terminal morene
Slide 2 - Tekstslide
Remember last lesson?
Homework from last few weeks was paragraph 1
exercises 1 to 9.
Today we start with paragraph 2.
Slide 3 - Tekstslide
Weathering or erosion?
Slide 4 - Tekstslide
Weathering or erosion?
Slide 5 - Tekstslide
Weathering or erosion?
Slide 6 - Tekstslide
Types of weathering
Mechanical weathering
Weathering that does not change the composition of rock
Chemical weathering
Weathering that changes the composition of rock.
Biological weathering
Weathering caused by living organisms.
Slide 7 - Tekstslide
Slide 8 - Video
Slide 9 - Tekstslide
Slide 10 - Tekstslide
Slide 11 - Tekstslide
Slide 12 - Tekstslide
Slide 13 - Tekstslide
Note down!!
terminal moraine
Pulverized material pushed forward by a glacier.
lateral moraine
Debris on the side of an ice lobe
Slide 14 - Tekstslide
Assignment
Make a drawing of a glacier (not an exact replica)
Fill in the following words in the right spot:
Lateral moraine
Terminal moraine
Firn basin
Glacial portal
Ready?
Please start with paragraph 2: 1 to 4
Slide 15 - Tekstslide
Tasks
Paragraph 2: 1 to 4
Lesson up questions
Challenge?
Create your own lessonup including questions.
Slide 16 - Tekstslide
transported by ICE
transported by WIND
transported by WATER
Slide 17 - Sleepvraag
Match the descriptions with the terms.
The combination of abrasion and plucking.
Glaciers melt and leave behind rocks and sand.
A glacier picks up a rock.
Lines on a rock, made by glaciers that scraped the glacier bed.
A glacier moves down the mountain and drags rocks along.
Rocks at the base of the glacier scrape the glacier bed.
Water gets into little cracks in the rock. As the water freezes, it expands. The crack becomes bigger.
Rocks that are left behind when the glacier melts.
Rocks inside, underneath, besides and on top of glaciers
Deposition
Freeze-thaw weathering
Erosion
Plucking
Glacial till
Abrasion
Transportation
Striations
Moraines
Slide 18 - Sleepvraag
Explain in your own words how a waterfall forms.
Slide 19 - Open vraag
What do you know at the end of the lesson?
1.
The characteristics of the upper reaches of the Rhine
2.
How the Schaffhausen waterfall was formed
Language aim:
-You are able to use the words glacier fed, rain fed and mixed river in a correct sentence.
Slide 20 - Tekstslide
Glacier
Firn basin
Glacier
Glacial Portal
Lateral moraine
Slide 21 - Tekstslide
MORAINES
Slide 22 - Tekstslide
Slide 23 - Tekstslide
The rhine catchment area
Upper reaches
Alps in Switzerland (Basel) to Bingen Germany
Fast currents
A lot of erosion
V-Shaped valley with steep sides
Slide 24 - Tekstslide
en
Waterfall of schaffhausen
Slide 25 - Tekstslide
Slide 26 - Video
Assignment
The Rhine is a mixed rivertype. Take the atlas and find for every type a river. What is your approach?
Explain how you came to the conclusion. Write it down in your notebook.
Glacier fed:
Rain fed:
Mixed:
Done? continue with exercises 5 to 10 (or lessonup)
Slide 27 - Tekstslide
What do you know at the end of the lesson?
1.
The characteristics of the upper reaches of the Rhine
2.
How the Schaffhausen waterfall was formed
Language aim:
-You are able to use the words glacier fed, rain fed and mixed river in a correct sentence.
Slide 28 - Tekstslide
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