2.2 the Rhine a river in Europe

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Slide 1: Tekstslide
AardrijkskundeMiddelbare schoolhavo, vwoLeerjaar 2

In deze les zitten 33 slides, met interactieve quiz, tekstslides en 2 videos.

time-iconLesduur is: 60 min

Onderdelen in deze les

Slide 1 - Tekstslide

Slide 2 - Link

At the end of this lesson
You can describe the differences between the upper and middle courses of the River Rhine.

Language aims: you are able to use the keywords: upper course, middle course, gradient

Slide 3 - Tekstslide

Draw the following keywords in your notebook

1.Erosion
2.Weathering
3.Endogenic
4.Exogenic

Slide 4 - Tekstslide

Upper course


Swiss alps

Slide 5 - Tekstslide

Swiss alps
-A glacier starts dripping
-Water erodes the rock
-High and steep river banks (v-shape)
-Narrow river
-Gradient(slope) is high

Slide 6 - Tekstslide

Slide 7 - Tekstslide

Middle and lower course
Watershed middle course
Germany, Luxemburg, France, Belgium

Watershed lower course 
Germany, Belgium, Netherlands

Slide 8 - Tekstslide

Upper Rhine plain

Slide 9 - Tekstslide

Formation of an oxbow lake

Slide 10 - Tekstslide





Oxbow lake

Slide 11 - Tekstslide

Slide 12 - Video

Transportation instead of erosion
Suspension= stijgen
Traction= rollen
Solution= oplossen
Saltation= saltare = springen

Slide 13 - Tekstslide

Slide 14 - Video

To do:
>Exercises 3 to 6



Slide 15 - Tekstslide

Now you know
You can describe the differences between the upper and middle courses of the River Rhine.

Language aims: you are able to use the keywords: upper course, middle course, gradient

Slide 16 - Tekstslide

HORST & GRABEN

Slide 17 - Tekstslide

Horst & Graben
GRABEN

Slide 18 - Tekstslide

At the end of the lesson:
How you can calculate the fall and gradient between 2 points in a river (G121).


How you can explain the difference in formation between an estuary and a delta, using the terms sedimentation and erosion (G90).

Slide 19 - Tekstslide

Try to explain how a meander forms
-Write it in your notebook.


timer
3:00

Slide 20 - Tekstslide

The lower reaches of the Rhine

In the lower reaches after Bonn > slow current > meanders > Rhine splits into Waal, Nether-Rhine and IJssel.

Fall (verval) = difference in altitude between two points along a river
Gradient (verhang) = fall per kilometre

Example: Spijk (12 metres) and Hoek van Holland (0 metres) >>  150 km apart 

Fall = 12 metres
Gradient = 12 metres : 150 kilometres = 0.08 metres per km



Slide 21 - Tekstslide

Near the mouth
 


--Very little difference in altitude 
--Small fall and gradient > lot of sedimentation> riverbed clogs > delta

Slide 22 - Tekstslide

Slide 23 - Tekstslide

Slide 24 - Tekstslide

Slide 25 - Tekstslide

Slide 26 - Tekstslide

Regime
The lower reaches of the Rhine.

The Netherlands lies on the Rhine delta.
Risk of flooding, but also flat and fertile, so densely populated.
Regime = fluctuations in the amount of water transported by a river.


Slide 27 - Tekstslide

Fall and gradient
Read the text and fill in:

Fall(verval)= ..........



Gradient(verhang)= ........

Ready? Start exercise 7 to 10

The difference in altitude between two points along a river.
The fall per kilometre.

Slide 28 - Tekstslide

To do 
Draw a sketch of the Rhine...put the following words in it:
Erosion-Transportation-meanders-narrow river-wide river

Exercise 7 to 10 paragraph 2.2
Check your answers


Slide 29 - Tekstslide

What is your question about 2.2?

Slide 30 - Open vraag

Now you know:
How you can calculate the fall and gradient between 2 points in a river (G121).


How you can explain the difference in formation between an estuary and a delta, using the terms sedimentation and erosion (G90).

Slide 31 - Tekstslide

FALL & GRADIENT

Slide 32 - Tekstslide

Try to explain how a meander forms
-Write it in your notebook.

Ready? Do the exercises on the handouts.
Homework: 2.3 exercise 1 to 6.

Slide 33 - Tekstslide