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L02 The Shape of the River

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CIE IGCSE
Geography
The Shape of the River
Recap
1. Label the letters A-F.
2. Label the drainage basin features shown on photos A-D.
A
C
B
D
3. Key Words
a. What is an input? …………………………………………………………………………………………………………………………………………….
b. Give an example. …………………………………………………………………………………………………………………………………………….
c. What is a store? ………………………………………………………………………………………………………………………………………………
d. Give an example. …………………………………………………………………………………………………………………………………………….
Task
Use the key words below to complete the table to work out what each definition means.
Cross sectional area / Depth / Discharge / Velocity / Wetted perimeter / Width
Key Term/Characteristic
Definition
River A
River B
The distance from bank to bank
of the surface of the water of the
river.
Narrow / wide
Narrow / wide
How far down the water goes.
This usually varies across a river,
so an average is taken of several
measurements.
Shallow / deep
Shallow / deep
Slow / fast
Slow / fast
Low / high
Low / high
Small / large
Small / large
Low / high
Low / high
The speed at which the river is
flowing. This varies with width.
The length of the wet part of the
channel cross-section containing
flowing water.
The area of flowing water when
measured from bank to bank.
The amount of water flowing in a
channel. This is calculated by
multiplying cross-sectional area
by velocity.
A
Source
B
The Long and Cross Profile
One of the most significant changes is to a river from source to mouth is its ……….……….………. ……….……….………. .
The long profile shows the ……….……….………. of a river as it journeys from source to mouth. It is a way of displaying
the channel slope (gradient) of a river along its entire length. Therefore, it shows how a river loses height with
increasing distance towards the sea. The diagram below shows the cross profile of the River Tees and some of its
features.
High Fell, source of the River Tees
Cauldron Snout
High Force waterfall
Barnard Castle
River Tees close to Darlington
Meanders south east of Darlington
Stockton on Tees
Tees Mouth
As you can see the gradient of the river is very steep in its upper course. You will also notice several steep drops in
the gradient at around 16 km from the source, then again at around 26 km. These are where waterfalls occur along
the River Tees. You will also notice a flat section in the upper course indicating the location of Cow Green reservoir.
Between 40 to 80km from the source the gradient contains to fall, though less rapidly. This is the middle course.
From 80 km to the source (160 km) the gradient is very gentle in the lower course.
The Cross Profile
Not only does the long profile of the river change from source to mouth, so does the ……….……….……….
……….……….………. ……….……….………. . River valley cross profiles show you a cross-section, taken sideways, of a river
valley at certain points in the river’s course.
Each section of a river, the upper, middle and lower course, has their own valley cross-profile features.
Valley Cross Profiles
The upper course typically has V-shaped valleys. The river usually
occupies most of the narrow valley floor. Vertical erosion creates Vshaped valleys as water flows around interlocking spurs (fingers of
land that jut out into the river valley that streams and rivers are forced
to flow around). In the upper course, the river erodes its bed by
hydraulic action and abrasion (note from Miss Starling: we will cover
this in the next few lessons!).
As more tributaries join the river the volume of water increases, as
does its erosive power. In the middle course the river valley becomes
wider due to the increase in lateral (sideways) erosion.
V-shaped valley with interlocking spurs in the
upper course of a river
In the lower course the river tends to be wider and deeper as the
gradient becomes gentler leading to less vertical erosion. This part
of the river can be tidal.
Images and text source
Task
1. Explain the difference between the long profile and the valley cross profile. Space has been provided to include a
diagram to support your answer.
……………………………………………………………………………………………………………………………………………………………………………….
……………………………………………………………………………………………………………………………………………………………………………….
……………………………………………………………………………………………………………………………………………………………………………….
……………………………………………………………………………………………………………………………………………………………………………….
2. Complete the table below to describe the characteristics of the long profile and the valley cross profile for each
stage of the River Tees.
Long profile
Upper
Course
Middle
Course
Lower
Course
Valley cross profile
3. Look at the photos below. Decide whether they show the upper or lower course of the river. Justify your decision (gives reasons for why you think this).
Photo A: Upper / lower
Photo B: Upper / lower
I think this because
I think this because
………………………………………………………………
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Photo B: Upper / lower
……………………………………………………………..
Photo C: Upper / lower
Photo D: Upper / lower
I think this because
I think this because
………………………………………………………………
………………………………………………………………
……………………………………………………………..
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