2.2 the Rhine a river in Europe

1 / 33
suivant
Slide 1: Diapositive
AardrijkskundeMiddelbare schoolhavo, vwoLeerjaar 2

Cette leçon contient 33 diapositives, avec quiz interactif, diapositives de texte et 2 vidéos.

time-iconLa durée de la leçon est: 60 min

Éléments de cette leçon

Slide 1 - Diapositive

Slide 2 - Lien

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 - Diapositive

Draw the following keywords in your notebook

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

Slide 4 - Diapositive

Upper course


Swiss alps

Slide 5 - Diapositive

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 - Diapositive

Slide 7 - Diapositive

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

Watershed lower course 
Germany, Belgium, Netherlands

Slide 8 - Diapositive

Upper Rhine plain

Slide 9 - Diapositive

Formation of an oxbow lake

Slide 10 - Diapositive





Oxbow lake

Slide 11 - Diapositive

Slide 12 - Vidéo

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

Slide 13 - Diapositive

Slide 14 - Vidéo

To do:
>Exercises 3 to 6



Slide 15 - Diapositive

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 - Diapositive

HORST & GRABEN

Slide 17 - Diapositive

Horst & Graben
GRABEN

Slide 18 - Diapositive

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 - Diapositive

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


timer
3:00

Slide 20 - Diapositive

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 - Diapositive

Near the mouth
 


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

Slide 22 - Diapositive

Slide 23 - Diapositive

Slide 24 - Diapositive

Slide 25 - Diapositive

Slide 26 - Diapositive

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 - Diapositive

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 - Diapositive

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 - Diapositive

What is your question about 2.2?

Slide 30 - Question ouverte

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 - Diapositive

FALL & GRADIENT

Slide 32 - Diapositive

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 - Diapositive