2.8-2.9 High Netherlands

High Netherlands
 


section 2.8-2.9
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Slide 1: Tekstslide
AardrijkskundeMiddelbare schoolvwoLeerjaar 2

In deze les zitten 23 slides, met interactieve quizzen, tekstslides en 1 video.

Onderdelen in deze les

High Netherlands
 


section 2.8-2.9

Slide 1 - Tekstslide

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 - Tekstslide

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 - Tekstslide

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 - Tekstslide

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 - Tekstslide

In which part of this catchment
area can we place the Netherlands
nowadays?

Slide 6 - Open vraag

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 - Tekstslide

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 - Tekstslide

Where did the ice came from during the second last ice age?
A
The Alps
B
Scandinavia
C
Schotland
D
The Ardennes

Slide 9 - Quizvraag

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 - Quizvraag

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 - Tekstslide

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 - Tekstslide

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 - Tekstslide

Where can we find glacial erratics?
A
In Limburg
B
In Zuid-Holland
C
In Groningen
D
All over the country

Slide 16 - Quizvraag

General knowledge:
What were the glacial erratics used for in Drente?
(use the Dutch word)

Slide 17 - Open vraag

Slide 18 - Tekstslide

Human impact

Slide 19 - Tekstslide

Soil type: sand
Advantage:
- high and so dry

Disadvantage:
- infirtile


The rainwater infiltrates easily and transports nutrients to deeper layers.

Slide 20 - Tekstslide

Solution infirtile soil
Previous
- manure of the sheep

Nowadays
- fertilizer (industrial)




Previous

Slide 21 - Tekstslide

High Netherlands: a lot of variation in landuse

Slide 22 - Tekstslide

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 - Tekstslide