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In the upper course, the river is high above seal level.
This gives the river a lot of potential energy. The river is trying to cut
down to its base level or downwards so it mainly does this through
vertical erosion. This creates the classic feature known as a V-shaped
valley - seen below.
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The main
characteristics of a
V - shaped valley and its river:
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The valley is narrow with a narrow, shallow river
channel
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The valleys have steep sides
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The channel has a steep gradient with features such
as pot holes, rapids and waterfalls
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The water is mainly slow flowing as most of the
rivers energy is used to overcome the friction of the river bed &
obstructions
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The load is mainly large, angular and rough
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Click on the image for an animation
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