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C2.1 - Lesson 3: The formation of the Alps
From the mountains to the sea
C2.1: The formation of the Alps
zlb@st-maartenscollege.nl
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Aardrijkskunde
Middelbare school
vwo
Leerjaar 2
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From the mountains to the sea
C2.1: The formation of the Alps
zlb@st-maartenscollege.nl
Slide 1 - Diapositive
What is the plan for today?
Finish paragraph 1
Repeat the most important parts
Slide 2 - Diapositive
Goals of last lesson
You are able to
explain
the differences between
endogenic
and
exogenic forces
.
You can
think
of 2 examples for both
endogenic
and
exogenic forces
(G66).
You can
explain
why shells and fossils can be found in the Alps.
You can
explain
in 4 steps how the Alps are formed.
Slide 3 - Diapositive
Endogenic & exogenic forces
Endogenic forces
Forces from
within
the Earth, that
changes the Earth's crust
.
Exogenic forces
Forces from
outside
the Earth, that
changes the Earth's crust
.
Slide 4 - Diapositive
Today's goals
You can
mention
3 differences between a young and an old mountain range.
You
know
the 4 different
reliefforms
, with their
height
(G77).
You can
explain
the process of the 3 types of
weathering
(G81).
You can
explain
the
erosive
effect of
weathered material
in the mountains (G84).
Slide 5 - Diapositive
Check homework!
2 to 5
Slide 6 - Diapositive
2
2 a
Exogenic forces change the Earth’s surface from the outside, endogenic forces change it from the inside.
b earthquake: ... force
weather: ... force
weathering: ... force
volcanic eruption: ... force
erosion: ... force
Slide 7 - Diapositive
Weathering
Open your notebook and work out the 3 kinds of weathering.
- What are the characteristics?
- What are the differences?
Slide 8 - Diapositive
Weathering
You can
explain
the process of the 3 types of
weathering
(G81).
"The disintegration of rock as a result of weather and vegetation."
Slide 9 - Diapositive
Slide 10 - Diapositive
Slide 11 - Diapositive
Slide 12 - Diapositive
Slide 13 - Diapositive
Slide 14 - Diapositive
You
know
the 4 different reliefforms, with their height (G77).
Slide 15 - Diapositive
Relief
0 - 200m -
Lowland
200 - 500m -
Hills
500 - 1500m -
Low mountain range
1500 and above -
High mountain range
Slide 16 - Diapositive
Slide 17 - Diapositive
Slide 18 - Diapositive
5
100 million years ago:
thick layers of dead animals and plants form in tropical sea.
80 million years ago:
The African plate starts to move and pushes sedimentary rock out of the tropical sea to the north.
30 million years ago:
The African plate collides with the Eurasian plate: formation of the Alps.
Slide 19 - Diapositive
Plate movements
Slide 20 - Diapositive
take note!
Three different movements:
Transform
Divergent
Convergent
Slide 21 - Diapositive
Plate movements
Slide 22 - Diapositive
Open G80
You can
mention
3 differences between a young and an old mountain range.
Slide 23 - Diapositive
Answer
Young mountain
ranges are high with (1) steep slopes, (2) sharp peaks and (3) deep valleys.
Old mountain
ranges have (1) gentle slopes and are (2) round at the top. (3) They are also much lower.
Young mountain ranges are still growing.
Slide 24 - Diapositive
Young or old?
Slide 25 - Diapositive
Young or old?
Slide 26 - Diapositive
Let's go!
Read the text at page 24/25 of your coursebook.
Make exercises
6 to 9
of paragraph 1 at page 23 in your workbook.
Read GeoGuide numbers 81 & 84.
Rules while working:
You work
alone
and in silence.
Raise your finger if you've a question.
Always read the exercise well before you ask your question.
FINISHED?
Open the list of knowledge and skill on your Chromebook and work out paragraph 1.
Slide 27 - Diapositive
Today's goals
You can
mention
4 differences between a young and an old mountain range.
You
know
the 4 different
reliefforms
, with their
height
(G77).
You can
explain
the process of the 3 types of
weathering
(G81).
You can
explain
the
erosive
effect of
weathered material
in the mountains (G84).
Slide 28 - Diapositive
Homework for next lesson
6 till 9 of paragraph 1.
Slide 29 - Diapositive
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