Cette leçon contient 23 diapositives, avec quiz interactifs, diapositives de texte et 2 vidéos.
Éléments de cette leçon
Low Netherlands
section 2.8-2.9
Slide 1 - Diapositive
This lesson
- The soil types in Low Netherlands - Man's influence on the landscape
Note!
1. You can check and improve your infographic (Low Netherlands).
2. For the rest of the class it's a new topic. So make some notes.
Slide 2 - Diapositive
Stroomgebied Maas en Rijn
Thick layers of shingle and sand in the whole of the Netherlands.
THE START
Slide 3 - Diapositive
When?
The landscape in Low Netherlands mostly formed in the last 10,000 years.
(High Netherlands between 200,000
and 10,000 years ago)
The climate warmed up
after the last ice age.
Slide 4 - Diapositive
What happened to the sea level after the ice age?
A
Drop in sea level (=lower)
B
Rise in sea level (=higher)
C
Remained the same
Slide 5 - Quiz
Sea level rise
Consequence:
The sea came closer to the Netherlands and flooded the lower part of the Netherlands.
Slide 6 - Diapositive
Soil types
In Low Netherlands, new soil types were deposited during this rise in sea level:
- Dune sand ==> section 2.5
- Peat
- Sea clay
Slide 7 - Diapositive
Characteristics of peat
- ability to retain a lot of moisture - contains residues of plant material
Disadvantage of peat
Subsidence (=inklinking)
Advantage of peat
Source for fuel
Slide 8 - Diapositive
How is peat formed?
1. The dunes along the sea are closed. 2. Behind the dunes a bog (=swamp) arises. 3. Dead plants disappear under water.
4. Without oxygen, the plant remains
won’t rot ==> accumulation of plant remains ==> peat
Slide 9 - Diapositive
Human impact
Slide 10 - Diapositive
Slide 11 - Vidéo
The typical landscape was formed due to peat mining. What was the peat used for?
Slide 12 - Question ouverte
Use the map.
How can you see this map is made in the landscape with peat?
Slide 13 - Diapositive
Parcellation
strip parcelling
Why this parcellation?
The peat was dug out along strips and laid out to dry next to it.
Slide 14 - Diapositive
Soil types
In Low Netherlands, new soil types were deposited during this rise in sea level:
- Dune sand ==> section 2.5
- Peat
- Sea clay
Slide 15 - Diapositive
How is see clay formed?
1. In the dunes there are openings. 2. During high tide the water flowed in through the opening. 3. During low tide the water flowed out again. 4. Behind the dunes the seawater came to a standstill. 5. Clay particles dropped to the bottem.
Slide 16 - Diapositive
Human impact
Slide 17 - Diapositive
Use the map.
How can you see this map is made in Low Netherlands?
Slide 18 - Diapositive
Parcellation
block shaped
Problems?
Floods by rivers and the sea.
Slide 19 - Diapositive
Slide 20 - Vidéo
Terps
Manmade hills to protect against floods from the sea.
Protection against the water
Pumping water out of the polder
First, mills were used to pump the water out of polder. Later, the mills were replaced by pumping engines.
Slide 21 - Diapositive
Where can we find most terps?
A
In Zuid-Holland
B
In Friesland and Groningen
C
In Noord-Brabant
D
In Gelderland
Slide 22 - Quiz
Homework
WB page 55: 4
WB page 57: 2+3
Note: the assignments belong to different sections (2.8 and 2.9)