2.2 The Rhine: a river in Europe

2.2 The Rhine: a river in Europe
1 / 23
next
Slide 1: Slide
AardrijkskundeMiddelbare schoolhavo, vwoLeerjaar 2

This lesson contains 23 slides, with text slides.

time-iconLesson duration is: 30 min

Items in this lesson

2.2 The Rhine: a river in Europe

Slide 1 - Slide

Aims
After studying this section, you will be able to:
  • Describe the differences between the upper, middle and lower courses of the river Rhine;
  • Explain the different uses of the river Rhine.

Slide 2 - Slide

Slide 3 - Slide

Slide 4 - Slide

Erosion, weathering, sedimentation

Erosion

  • Process of wearing away rock, soil or other solid materials. Always during transportation

Weathering

  • Process in which rocks are broken down. Always on a specifc location

Sedimentation

  • Process of deposition (leaving behind materials).

Slide 5 - Slide

Freeze-thaw weathering
Biological weathering

Slide 6 - Slide

A cross section of the river Rhine

The gradient decreases when the river flows from the source to the mouth.

The source of the river is in the Swiss Alps. This part is the upper course of the river.
Most of the middle course lies in Germany.
The lower course is in the Netherlands where it flows into the North Sea via a delta.
Here you find processes like weathering, erosion and transportation.
The most important process in the delta is sedimentation.

Slide 7 - Slide

Slide 8 - Slide

Slide 9 - Slide

Homework
Do exercises 2.2:  1-5 

Slide 10 - Slide

2.2 The Rhine: a river in Europe

Slide 11 - Slide

Drainage basin
  • From the source in the Alps to the mouth in The Netherlands;
  • 1,230 kilometres long;
  • The Rhine is a mixed river: Mostly rainfall water in winter and glacial water in summer.
  • The discharge is the amount of water that flows by a certain place in m3/s.

Slide 12 - Slide

Slide 13 - Slide

Summer
Winter

Slide 14 - Slide

Summer
Winter

Slide 15 - Slide

Calculating fall and drop of river
  • The fall = The difference in height between two places along a river.
  • The drop = The fall of the river per kilometre.
  • The difference in height between Spijk (where the Rhine enters the Netherlands) and Hoek of Holland (where it flows into the sea) is 12 metres. Between these two places the river Rhine has a length of 150 kilometres.
  • What is the fall?
  • Calculate the drop of the river.




Answers

Fall =  12 metres.

Drop = 12 m / 150 km= 0.08 m/km.

Slide 16 - Slide

Slide 17 - Slide

Meandering

Slide 18 - Slide

Slide 19 - Slide

Meandering
Meanders are produced when water in the stream channel erodes the sediments of an outer bend of a streambank and deposits this and other sediment on subsequent inner bends downstream.

Slide 20 - Slide

Slide 21 - Slide

Groynes help to limit river bank erosion and to keep the water depth in the middle of the river constant and accessible for ships.

Slide 22 - Slide

Homework 2mhT
  • Read 2.2 
  • Do exercises 6-10

Slide 23 - Slide