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Glaciated Landscapes and Change

Erratics and reconstructing former ice movement

  • 3 things to know
  • Paper 1

Overview

Recall questions on using erratics, crag and tail, drumlin orientation and till fabric to work out where the ice came from.

What you need to know

Answer each one before you reveal it.

Your recallNot started
Key term

How is the elongated shape of a drumlin oriented relative to ice movement?

Key term

In a crag and tail landform, which feature is located on the up-glacier side?

Key term

How can erratics be used to reconstruct former glacial conditions?

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    What is an erratic?

    Model answer

    A rock transported by glacial ice and deposited in a location where it differs from the local bedrock, providing evidence of ice movement direction and provenance.

  2. 2

    Why must an erratic be a distinctive rock type to be useful evidence of ice movement?

    Model answer

    Only a distinctive rock can be matched to one known outcrop, which is what allows the direction and distance of ice transport to be traced.

  3. 3

    How can erratics be used to reconstruct former glacial activity?

    Model answer

    Erratics indicate provenance (source area) and transport direction because their rock type can be traced back to their origin, showing where ice came from and the path it travelled.

  4. 4

    What information about former ice sheets can be determined from the positions of moraines?

    Model answer

    Moraine positions show the extent of former ice coverage, with terminal moraines marking maximum advance and recessional moraines indicating stages of retreat.

  5. 5

    How does crag and tail orientation help reconstruct past glacial conditions?

    Model answer

    Crag and tail orientation shows ice flow direction, with the resistant crag on the upstream side and the tail of deposited material extending downstream in the direction of ice movement.

  6. 6

    What does the alignment of drumlin long axes reveal about former glaciation?

    Model answer

    Drumlin long axes align parallel to the direction of ice movement, with the steeper stoss end facing upstream and the gentler lee slope pointing downstream.

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