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The Changing Landscapes of the UK

How the UK’s upland and lowland landscapes were formed

  • 3 things to know
  • Paper 1

Overview

What ice did to the mountains, corries, U-shaped valleys and till, freeze-thaw and chemical weathering, climate differences between west and east, rivers and slope processes since, and how farming, forestry and building altered the land.

What you need to know

Answer each one before you reveal it.

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Key term

What material did the ice sheets dump across lowland Britain?

Key term

How does building a town or city alter the surface of the land?

Key term

What shape is a valley left behind by a glacier, and how does it differ from one cut by a river?

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    What did moving ice do to the mountains of Britain during the last glacial period?

    Model answer

    It scoured out deep, steep-sided valleys with flat floors, and gouged hollows and knife-edged ridges into the high ground.

  2. 2

    Describe a corrie and say how ice made it.

    Model answer

    It is an armchair-shaped hollow high on a mountainside, deepened as ice rotated within it, plucking rock from the back wall and grinding the floor.

  3. 3

    What shape is a valley left behind by a glacier, and how does it differ from one cut by a river?

    Model answer

    A glacier leaves a broad U-shape with steep sides and a wide flat floor, while a river cuts a narrow V-shape.

  4. 4

    What material did the ice sheets dump across lowland Britain?

    Model answer

    Till, an unsorted mix of clay, sand and boulders dropped straight from the ice, together with sands and gravels sorted by meltwater streams.

  5. 5

    Explain freeze–thaw weathering and say where in Britain it is most active.

    Model answer

    Water seeps into a crack, freezes and expands, prising the crack wider until fragments snap off, and it works hardest on exposed mountain summits where temperatures cross 0°C often.

  6. 6

    How does rainwater chemically attack limestone and chalk?

    Model answer

    Rain is slightly acidic, so it dissolves the calcium carbonate, opening up joints into caves, gorges and underground passages.

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