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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AardrijkskundeMiddelbare schoolvwoLeerjaar 2

This lesson contains 29 slides, with text slides.

time-iconLesson duration is: 45 min

Items in this lesson

From the mountains to the sea


C2.1: The formation of the Alps


zlb@st-maartenscollege.nl

Slide 1 - Slide

What is the plan for today?

  • Finish paragraph 1
  • Repeat the most important parts

Slide 2 - Slide

Goals of last lesson
  1. You are able to explain the differences between endogenic and exogenic forces.
  2. You can think of 2 examples for both endogenic and exogenic forces (G66).
  3. You can explain why shells and fossils can be found in the Alps.
  4. You can explain in 4 steps how the Alps are formed. 

Slide 3 - Slide

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 - Slide

Today's goals
  1. You can mention 3 differences between a young and an old mountain range.
  2. You know the 4 different reliefforms, with their height (G77).
  3. You can explain the process of the 3 types of weathering (G81).
  4. You can explain the erosive effect of weathered material in the mountains (G84).

Slide 5 - Slide

Check homework!
2 to 5

Slide 6 - Slide

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 - Slide

Weathering
Open your notebook and work out the 3 kinds of weathering.

- What are the characteristics?
- What are the differences?

Slide 8 - Slide

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 - Slide

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You know the 4 different reliefforms, with their height (G77).

Slide 15 - Slide

Relief
0 - 200m - Lowland
200 - 500m - Hills
500 - 1500m - Low mountain range
1500 and above - High mountain range

Slide 16 - Slide

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Slide 18 - Slide

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 - Slide

Plate movements

Slide 20 - Slide

take note!
Three different movements:

Transform
Divergent
Convergent

Slide 21 - Slide

Plate movements

Slide 22 - Slide

Open G80

You can mention 3 differences between a young and an old mountain range.

Slide 23 - Slide

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 - Slide

Young or old?

Slide 25 - Slide

Young or old?

Slide 26 - Slide

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 - Slide

Today's goals
  1. You can mention 4 differences between a young and an old mountain range.
  2. You know the 4 different reliefforms, with their height (G77).
  3. You can explain the process of the 3 types of weathering (G81).
  4. You can explain the erosive effect of weathered material in the mountains (G84).

Slide 28 - Slide

Homework for next lesson

6 till 9 of paragraph 1.

Slide 29 - Slide