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River Landscapes and Processes

River landforms from source to mouth

  • 3 things to know
  • Paper 1 section A

Overview

Interlocking spurs, waterfalls, plunge pools and gorges, river cliffs, flood plains, levees and point bars, how meanders develop into oxbow lakes and meander scars, and how valleys, meanders, flood plains and waterfalls are recognised on OS maps.

What you need to know

Answer each one before you reveal it.

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Key term

Explain how a difference in rock hardness produces a waterfall.

Key term

Explain how a waterfall retreats upstream and leaves a gorge behind it.

Key term

Explain how repeated flooding builds up a flood plain.

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    What are interlocking spurs and where are they found?

    Model answer

    Ridges of higher land that jut into the valley from alternate sides in the upper course, where the river winds between them instead of cutting through.

  2. 2

    Why does a river wind around spurs rather than remove them in its upper course?

    Model answer

    It has little energy left over after cutting downwards, so it takes the easiest route around resistant obstacles rather than eroding sideways through them.

  3. 3

    Explain how a difference in rock hardness produces a waterfall.

    Model answer

    The river cuts quickly through weaker rock downstream but barely touches a harder band, leaving a step over which the water falls.

  4. 4

    How is a plunge pool created at the foot of a waterfall?

    Model answer

    Falling water and the rocks it carries attack the bed by hydraulic action and abrasion, hollowing out a deep basin.

  5. 5

    Explain how a waterfall retreats upstream and leaves a gorge behind it.

    Model answer

    Splashback undercuts the softer rock beneath the hard cap until the unsupported overhang collapses; repeated over time this moves the fall upstream and leaves a steep-sided narrow valley in its place.

  6. 6

    What is a river cliff and how is one cut?

    Model answer

    A steep bank on the outer side of a bend, undercut by the fastest flow through hydraulic action and abrasion until the material above collapses.

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