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Rivers begin in upland areas and flow downhill,
becoming deeper and wider until they reach the sea. Opposite is a
typical diagram of a drainage basin and it shows its main feature.
A drainage basin is part of the water cycle where
water is transferred in a continuous cycle between the sea, atmosphere
and the land.
As the river flows downstream its characteristics
change through the three main sections of
The Upper Course
the Middle Course
The Lower Course |