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Glaciated Landscapes

Characteristic glaciated landscapes and how they change over time

  • 2 things to know
  • Component 01

Overview

Recall questions on the landform assemblages of glaciated uplands and ice-sheet lowlands, the Helvellyn area of the Lake District, the Laurentide Ice Sheet with the Canadian Shield, Long Island and the Finger Lakes, change over seconds, seasons and millennia, varves, and Britain's relict glaciated landscape.

What you need to know

Answer each one before you reveal it.

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Key term

Which landforms would you expect to find together in an upland shaped by valley glaciers?

Key term

Which landforms characterise a lowland shaped by an ice sheet?

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    What is meant by a characteristic glaciated landscape?

    Model answer

    It is an assemblage of landforms that occur together and share a common origin, so the landscape as a whole can be read as the product of one system.

  2. 2

    Which landforms would you expect to find together in an upland shaped by valley glaciers?

    Model answer

    Corries, arêtes and pyramidal peaks on the high ground, with troughs, truncated spurs, hanging valleys, ribbon lakes and moraines below.

  3. 3

    Which landforms characterise a lowland shaped by an ice sheet?

    Model answer

    Till sheets and drumlin swarms, ice-scoured knock and lochan surfaces, scattered erratics and long, low moraine ridges.

  4. 4

    Explain why corries, arêtes and pyramidal peaks are described as inter-related.

    Model answer

    They are produced by the same process of corrie back wall retreat, and each develops out of the others as more corries cut into a single mountain.

  5. 5

    How are a corrie and a ribbon lake connected within one upland landscape system?

    Model answer

    The corrie fed ice into the trough below, and that ice over-deepened the rock basin the ribbon lake now occupies.

  6. 6

    Name three features of the Helvellyn area of the Lake District that show it was shaped by valley glaciers.

    Model answer

    Red Tarn in its corrie, the arêtes of Striding Edge and Swirral Edge, and the trough now filled by Ullswater.

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AThe lower quartile is the 2nd value, 11 cm.
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