A long profile shows how the gradient of the river channel changes from the river's source to its mouth. It does this by showing the height of the river bed above base level (the lowest point the river can erode to) for the whole length of the river.
The total amount of erosion and deposition along the full course of a river are balanced, but the rates of erosion and deposition change along its course. This results in landforms such as waterfalls, making the profile uneven.
Upper course: steep gradient, high above sea level, lots of potential energy
Middle course: gradient decreases, potential energy converted to kinetic energy
Lower course: little potential energy, lots of kinetic energy
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