§2.3 Catchment area of the Rhine part 2

§2.3 Catchment area of the Rhine part 2

1 / 22
volgende
Slide 1: Tekstslide
AardrijkskundeMiddelbare schoolhavo, vwoLeerjaar 2

In deze les zitten 22 slides, met interactieve quizzen, tekstslides en 1 video.

time-iconLesduur is: 45 min

Onderdelen in deze les

§2.3 Catchment area of the Rhine part 2

Slide 1 - Tekstslide

Program
  • Retrospective
  • Learning Objectives
  • Explanation part 1
  • Getting started!
  • End

Slide 2 - Tekstslide

Where does erosion occur and where does sedimentation occur?
A
Erosion in the upper reaches, sedimentation in the lower reaches
B
Sedimentation in the upper reaches, erosion in the lower reaches
C
Sedimentation in the lower reaches, erosion in the middle reaches and sedimentation in the upper reaches
D
Erosion in the lower reaches, erosion in the middle reaches and sedimentation in the upper reaches

Slide 3 - Quizvraag

The end of the Rhine, where the river flows into the sea, is also called
A
Delta
B
The lower reaches
C
The middle reaches
D
Estuarium

Slide 4 - Quizvraag

This is where the water flows hardest
A
Middle reaches
B
Lower reaches
C
Upper reaches
D
In North-Korea

Slide 5 - Quizvraag

This is where most sedimentation takes place
A
Middle reaches
B
Lower reaches
C
Upper reaches
D
Sovjet-Union

Slide 6 - Quizvraag

What process predominates here in the photograph?
A
weathering
B
erosion
C
sedimentation
D
stupid question

Slide 7 - Quizvraag

What process predominates here in the photograph?
A
weathering
B
erosion
C
sedimentation
D
I'm smart

Slide 8 - Quizvraag

In the inside bend,..... place finds
A
Weathering
B
Erosion
C
Sedimentation
D
There is no bend

Slide 9 - Quizvraag

Discuss assignments
6 and 7

Slide 10 - Tekstslide

Goals
After this lesson:
... you will know the difference between fall and gradient
... you can explain in your own words what the flow rate and regime of a river are

Slide 11 - Tekstslide

Notes

Slide 12 - Tekstslide

Slide 13 - Tekstslide

Floodings
People like to live close to the river. They built streets and buildings. More impervious surface.
Impervious surface = Paved areas and infrastructure that prevent water from infiltrating into the ground.

This reduced infiltration (=intrusion of water into soil) and therefore the river fills up quickly.

Slide 14 - Tekstslide

Floods
When it rains hard, normally plants and trees can catch the water, but due to the increase of impervious surfaces, water can not infiltrate and flows to the river

So there is a greater chance of flooding

Slide 15 - Tekstslide

Slide 16 - Video

Catchment area Rhine and Meuse

Slide 17 - Tekstslide

Flow in river
Regime: The fluctuations in a river’s flow rate

Flow rate: the amount of water flowing at a particular point in the river (m3/s)


Slide 18 - Tekstslide



Fall:
The difference in altitude between two points along a river





Gradient:
The fall per kilometre in m/km

Slide 19 - Tekstslide

Fall =
height difference=
2500-2000= 500 m
Gradient = fall per km
Height difference
----------------------
Distance

Slide 20 - Tekstslide

Calculate the fall and gradient
Location 1: Spijk =12m
Location 2: Hoek van Holland= 0m
Distance between 1 and 2 = 150 km

Fall=...................
Gradient=......................... : ............... = .....m/km

Slide 21 - Tekstslide

Let's go to work!
From §2.3, make assignments 2, 8 and 10

Slide 22 - Tekstslide