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River Landscapes and Processes

The long profile of a river and the effect of UK weather

  • 3 things to know
  • Paper 1 section A

Overview

How height, valley shape, channel size, gradient, discharge, velocity and sediment change from source to mouth, what storms, dry spells, seasons and the wetter west do to a river's energy, and how geology maps explain the steeper sections of a long profile.

What you need to know

Answer each one before you reveal it.

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Key term

What does a river's long profile show, why is the upper valley V-shaped, and how and why does discharge change downstream?

Key term

What does the long profile of a river show?

Key term

What shape is the valley in the upper course, and why does it take that shape?

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    What does the long profile of a river show?

    Model answer

    How the height of the channel falls from source to mouth, steep near the source and almost flat near the sea.

  2. 2

    What shape is the valley in the upper course, and why does it take that shape?

    Model answer

    A narrow V-shape, because the river erodes vertically downwards while weathering and mass movement bring the steep sides into the channel.

  3. 3

    How has the cross profile of the valley changed by the lower course?

    Model answer

    It is wide with a broad, almost flat floor, because sideways erosion and deposition have widened it over time.

  4. 4

    What happens to the width and depth of the channel as you move downstream?

    Model answer

    Both increase, because tributaries add water and the larger volume needs a bigger channel to carry it.

  5. 5

    Describe how gradient changes between the source and the mouth.

    Model answer

    It is at its steepest near the source and becomes progressively gentler, so the lower course is nearly level.

  6. 6

    What is discharge, and in what units is it measured?

    Model answer

    The volume of water passing a given point every second, measured in cubic metres per second (m³ s⁻¹).

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