This lesson contains 24 slides, with interactive quizzes, text slides and 4 videos.
Lesson duration is: 45 min
Items in this lesson
The Dutch landscape
Slide 1 - Slide
learning goals
Describe the landscape of Zuid-limburg
Explain how different elements in the landscape of
Zuid-Limburg were formed
Slide 2 - Slide
Slide 3 - Video
What are the similarities between the Dutch and Chinese loess landscape?
Slide 4 - Mind map
Zuid Limburg
In Zuid-Limburg layers of solid rock are close to the surface while in the rest of our country they are located deeper in the earths crust.
Slide 5 - Slide
Slide 6 - Slide
Slide 7 - Slide
Why do we only find marl, limestone, coal and sandstone only in Zuid-Limburg so close to the surface?
Slide 8 - Mind map
Answer
Since 300 million years Zuid-Limburg is slowly rising and during the rise layers are folded.
The earths layers are no longer horizontal.
Slide 9 - Slide
Dallandschap (keyword)
The rivers Maas, Geul, Gulp flow faster in Zuid-Limburg than
in the rest of the Netherlands
( look at figure 4.41 )
Slide 10 - Slide
Why do rivers flow faster?
Slide 11 - Mind map
Slide 12 - Video
and on top of the canyons?
a thin layer ( compared to the United States )
of loess!
Slide 13 - Slide
Slide 14 - Video
Villages/meadows ? Woods? Agricultural fields?
Slide 15 - Slide
Why are the woods located on the steeper slopes?
The risk of erosion on the steeper slopes.
Slide 16 - Slide
Take an atlas?
Go to the page with the loess landscape.
How can you recognize if a slope is steep or not on a map?
What does a slope percentage of 10% mean?
Slide 17 - Slide
A lot of the layers in Zuid-Limburg have dissapeared like (A)coal, (B)marl, (C)limestone, (D) flint to be used as (1)tools, (2)fuel, (3)building material
A
A2/B3/C2/D1
B
A1/B2/C1/D3
C
A2/B3/C3/D1
D
A2/B1/C2/D1
Slide 18 - Quiz
What is a disadvantage of the mining of these layers?