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C2.3 - Lesson 7: Catchment area of the Rhine
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Aardrijkskunde
Middelbare school
vwo
Leerjaar 2
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Lesson duration is:
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Slide 1 - Slide
Slide 2 - Slide
From the mountains to the sea
C2.3: Catchmentarea of the Rhine
zlb@st-maartenscollege.nl
Slide 3 - Slide
What is the plan for today?
Short repeat of C2.2: Rivers of ice
THE LAST PARAGRAPH
C2.3:
Catchment area of the Rhine
Slide 4 - Slide
Goals of last lesson
You can
explain
the differences in origin between a
U-shaped valley
and a
V-shaped
valley
.
You can
relate
the terms
glacial
tunnel
,
glacial
portal
and
glacier
-
fed
river
to each other.
You can
explain
how the
weathered
material
is carried by 4 different transporters (G83).
You can
describe
the relationship between the flow speed of the river and
erosion
.
Slide 5 - Slide
Slide 6 - Slide
You can
relate
the terms
glacial
tunnel
,
glacial
portal
and
glacier
-
fed
river
to each other.
Slide 7 - Slide
You can
describe
the relationship between the flow speed of the river and erosion.
Slide 8 - Slide
Slide 9 - Slide
Slide 10 - Slide
Higher means a higher current
Slide 11 - Slide
CHECK HOMEWORK
Slide 12 - Slide
Slide 13 - Slide
Slide 14 - Slide
C2.3: Catchment area of
the Rhine
Slide 15 - Slide
Today's goals
You can
explain
the relationship between
meanders
and the
flow speed
in the
Upper Plain
(W9, W10, G90).
You can
explain
in 3 steps how an
oxbow lake
is created (W11, G90).
You can
use
a map to show the
watershed
between two
catchment areas
(G120).
You can
explain
why the
flow rate
in summer is much lower than in winter (G120).
Slide 16 - Slide
Catchment area of the Rhine
Catchment area /
watershed
Slide 17 - Slide
Slide 18 - Slide
G120 in your GeoGuide
W8 in your workbook
Slide 19 - Slide
Upper- middle- and lower reaches
Slide 20 - Slide
MEANDERING (G90)
A natural bend in a river.
EROSION
SEDIMENTS
Slide 21 - Slide
Meander
On the lowlands -> low flow speed -> less erosion -> wide valley
Rhine will
meander
= make wide bends
Slide 22 - Slide
Slide 23 - Slide
Meanders are getting bigger and bigger. The water flows faster in the outer bend (
erosion
) and slower in the inner bend (
sedimentation
).
Slide 24 - Slide
Formation of an oxbow lake
Slide 25 - Slide
Open exercise 6 in your workbook
Finished? Make exercise 9
Slide 26 - Slide
G79: HORST &
GRABEN
Slide 27 - Slide
Let's go!
Read the text at page 28/29 of your coursebook.
Make exercises 1,
6 & 9
of paragraph 3 in your workbook.
Read GeoGuide number 79 & figure 3.26
Rules while working:
You're allowed to work together, but whisper.
Raise your finger if you've a question.
Finished?
Start working out the list of knowledge and skills.
Slide 28 - Slide
G121: Fall and gradient
Fall:
The difference in altitude between two points along a river.
Gradient:
The
fall
per kilometre.
Take question 8 in front of you
Slide 29 - Slide
You can
calculate
the
fall
and
gradient
between 2 points in a river (G121).
FALL & GRADIENT
Slide 30 - Slide
Today's goals
You can
explain
the relationship between
meanders
and the
flow speed
in the
Upper Plain
(W9, W10, G90).
You can
explain
in 3 steps how an
oxbow lake
is created (W11, G90).
You can
use
a map to show the
watershed
between two
catchment areas
(G120).
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 31 - Slide
Homework for next lesson
Make exercises 1, 2, 3, 5 & 6 of paragraph 3 in your workbook.
Slide 32 - Slide
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