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Glaciated Landscapes

Glacial landscape suites and change over time

  • 2 things to know
  • Component 1 Section A

Overview

Suite of landforms typical of a highland glaciated landscape, suite of landforms typical of a lowland glaciated landscape and knock and lochan topography.

What you need to know

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Key term

Describe the suite of landforms typical of a highland glaciated landscape.

Key term

Describe the suite of landforms typical of a lowland glaciated landscape.

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    Describe the suite of landforms typical of a highland glaciated landscape.

    Model answer

    Highland areas carry cirques, arêtes, pyramidal peaks, glacial troughs, hanging valleys and truncated spurs. Ribbon lakes occupy the over-deepened trough floors.

  2. 2

    Describe the suite of landforms typical of a lowland glaciated landscape.

    Model answer

    Lowlands carry till plains, drumlin swarms, terminal and recessional moraines and erratics. Fluvioglacial eskers, kames and outwash plains lie among them.

  3. 3

    Why is erosion dominant in the highlands and deposition in the lowlands?

    Model answer

    Steep gradients confine and accelerate mountain ice, so erosion dominates there. Ice spreading onto a lowland slows and thickens with debris, so material is released.

  4. 4

    Contrast the landscape left by an ice sheet with that left by a valley glacier.

    Model answer

    An ice sheet scours a wide area evenly and leaves ice-moulded knock and lochan terrain or till plains. A valley glacier is confined and cuts a single deep trough with cirques above it.

  5. 5

    What is knock and lochan topography?

    Model answer

    Knock and lochan is a landscape of ice-scoured rock knolls separated by small lake-filled hollows. North-west Scotland around Assynt is the classic British example.

  6. 6

    Why do valley glaciers produce sharper relief than ice sheets?

    Model answer

    Confined ice concentrates erosion into a narrow trough while the peaks above stay exposed to frost shattering. An ice sheet buries the whole landscape and smooths it instead.

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