C2.3 - Lesson 6: Catchment area of the Rhine

From the mountains to the sea



C2.3: Catchmentarea of the Rhine


zlb@st-maartenscollege.nl
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Slide 1: Slide
AardrijkskundeMiddelbare schoolvwoLeerjaar 2

This lesson contains 19 slides, with text slides.

time-iconLesson duration is: 45 min

Items in this lesson

From the mountains to the sea



C2.3: Catchmentarea of the Rhine


zlb@st-maartenscollege.nl

Slide 1 - Slide

What is the plan for today?

REPEAT LAST TIME:
  • C2.2: Rivers of ice
START OF A NEW PARAGRAPH
  • C2.3: Catchment area of the Rhine

Slide 2 - Slide

Rules during class
  1. A maximum of one person is speaking.
  2. Raise your finger or hand if you want to say something.
  3. Phones are off or quiet and are in your bag
  4. Always bring your books: Coursebook, workbook, notebook & chromebook.

Slide 3 - Slide

Goals of last lesson
  1. You can explain the differences in origin between a U-shaped valley and a V-shaped
    valley
  2. You can relate the terms glacial tunnel, glacial portal and glacier-fed river to each other.
  3. You can explain how the weathered material is carried by 4 different transporters (G83).
  4. You can describe the relationship between the flow speed of the river and erosion.

Slide 4 - Slide

MORAINES

Slide 5 - Slide

Slide 6 - Slide

You can explain how a glacier is formed, using the following terms: precipitation, firn , basin, glacier (G87).

Precipitation - Water (rain, snow or hail) from the athmosphere that falls on the Earth.
Firn - Crystalline, ice snow left over from previous seasons. (old snow)
Firn basin - A place high in the mountains where firn accumulates.

Slide 7 - Slide

Slide 8 - Slide

V-shaped valley
caused by a river
U-shaped valley
caused by a glacier

Slide 9 - Slide

You can relate the terms glacial tunnel, glacial portal and glacier-fed river to each other.

Slide 10 - Slide

C2.3: Catchment area of 
the Rhine

Slide 11 - Slide

Today's goals
  1. You can explain the relationship between meanders and the flow speed in the Upper Plain
    (W9, W10, G90). 
  2. You can explain in 3 steps how an oxbow lake is created (W11, G90).
  3. You can use a map to show the watershed between two catchment areas (G120).
  4. You can explain why the flow rate in summer is much lower than in winter (G120).

Slide 12 - Slide

Catchment area of the Rhine

Catchment area /
watershed

Slide 13 - Slide

MEANDERS (G90)

A natural bend in a river.

EROSION
SEDIMENTS

Slide 14 - Slide

Formation of an oxbow lake

Slide 15 - Slide

G120 in your GeoGuide
W8 in your workbook

Slide 16 - Slide

Today's goals
  1. You can explain the relationship between meanders and the flow speed in the Upper Plain
    (W9, W10, G90). 
  2. You can explain in 3 steps how an oxbow lake is created (W11, G90).
  3. You can use a map to show the watershed between two catchment areas (G120).
  4. You can explain why the flow rate in summer is much lower than in winter (G120).
Answer today's goals in your notebook, it's part of the homework.

Slide 17 - Slide

Let's go!
  • Read the text at page 28/29 of your coursebook.
  • Make exercises 1, 2, 3, 5 & 6 of paragraph 3 in your workbook.
  • Read GeoGuide numbers 90/120/121.

Rules while working:
  • You work alone and in silence.
  • Raise your finger if you've a question.
  • Always read the exercise well before you ask your question.


Slide 18 - Slide

Homework for next lesson

Make exercises 1, 2, 3, 5 & 6 of paragraph 3 in your workbook.

Slide 19 - Slide