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2.8-2.9 High Netherlands
High Netherlands
section 2.8-2.9
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Slide 1:
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Aardrijkskunde
Middelbare school
vwo
Leerjaar 2
This lesson contains
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interactive quizzes
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High Netherlands
section 2.8-2.9
Slide 1 - Slide
This lesson
1. You can check and improve your infographic (High Netherlands).
2. For the rest of the class it's a new topic. So make some notes.
==> next lesson: Low Netherlands
Homework: first version of the infographic
Slide 2 - Slide
Program
The Dutch Landscape
Which landscapes do we distinguish and where are they in the Netherlands?
The natural history of the landscapes: soil types and relief.
Man's influence on the landscape
Slide 3 - Slide
The Dutch landscape
The Dutch landscape consists of:
A Low Netherlands
B High Netherlands
How is the boundary between
High and Low Netherlands defined?
A
B
Land > 1 meter above N.A.P.
Slide 4 - Slide
Forming of the dutch landscape
When you dig in the garden, you'll find shingle, sand and clay.
Almost nowhere do we find solid rock.
Why is that?
Shingle and sand
Solid rock in Limburg
Slide 5 - Slide
In which part of this catchment
area can we place the Netherlands
nowadays?
Slide 6 - Open question
Stroomgebied Maas en Rijn
Cause: the water flows slowly and the materials carried by the water are deposited.
Consequence: thick layers of shingle and sand in the whole of the Netherlands
Source of the shingle and sand
The Netherlands is still declining
Because most of the Netherlands is slowly sinking, the rivers can keep on bringing sediment.
Slide 7 - Slide
Forming of the dutch landscape
The landscape in High Netherlands was mostly formed during the ice ages between 200,000 and 10,000 years ago.
Slide 8 - Slide
Where did the ice came from during the second last ice age?
A
The Alps
B
Scandinavia
C
Schotland
D
The Ardennes
Slide 9 - Quiz
https:
Slide 10 - Link
Where could you find the ice during the second last ice age?
A
There was no ice in The Netherlands
B
Only in the north of the country
C
The ice reached the middle of the country
D
The whole of the country was covered in ice
Slide 11 - Quiz
Second last ice age
The ice reached the imaginary line
Haarlem-Utrecht-Nijmegen
North of this
HUN-line
the ice left traces in the landscape:
- pushed moraines
- glacial erratics
- melt-water valleys
Slide 12 - Slide
Slide 13 - Video
During the ice age ice tongues worked like bulldozers.
At the end of the ice
age, the ice withdrew again.
You can still find the push moraines in the landscape of High Netherlands.
e.g. Veluwe, Utrechtse Heuvelrug
Slide 14 - Slide
Traces of the ice age
In some parts of the Netherlands you can find rocks, sometimes with a diameter of more than one metre.
These
glacial erratics
came along with the ice and were deposited in the Netherlands when the ice melted.
Slide 15 - Slide
Where can we find glacial erratics?
A
In Limburg
B
In Zuid-Holland
C
In Groningen
D
All over the country
Slide 16 - Quiz
General knowledge:
What were the glacial erratics used for in Drente?
(use the Dutch word)
Slide 17 - Open question
Slide 18 - Slide
Human impact
Slide 19 - Slide
Soil type: sand
Advantage:
- high and so dry
Disadvantage:
- infirtile
The rainwater infiltrates easily and transports nutrients to deeper layers.
Slide 20 - Slide
Solution infirtile soil
Previous
-
manure
of the sheep
Nowadays
-
fertilizer
(industrial)
Previous
Slide 21 - Slide
High Netherlands: a lot of variation in landuse
Slide 22 - Slide
Homework
WB page 54: 2,3
WB page 57: 4a,b,c,d
Note:
the assignments belong to different sections (2.8 and 2.9)
Slide 23 - Slide
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