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Glacial Systems and Landscapes

Moraines, Till and Fluvioglacial Landforms

  • 3 things to know
  • Component 1

Overview

Recall questions on lateral, medial, terminal, recessional and ground moraines, till plains and till, and on meltwater channels, kames, kame terraces, eskers and outwash plains, and how fluvioglacial deposits differ from till.

What you need to know

Answer each one before you reveal it.

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Key term

Distinguish a recessional moraine from a terminal moraine.

Key term

Name three types of meltwater channel based on their position relative to the ice.

Key term

Where does the meltwater that forms an esker flow?

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    Where does a lateral moraine form?

    Model answer

    At the margins (sides) of a valley glacier, from debris falling from valley walls and material pushed aside by the ice.

  2. 2

    How does a medial moraine originate?

    Model answer

    When two glaciers merge, their adjacent lateral moraines combine to form a single ridge of debris running down the centre of the enlarged glacier.

  3. 3

    What does a terminal moraine indicate about former ice extent?

    Model answer

    It marks the maximum advance of the glacier, where debris accumulated at the ice front.

  4. 4

    Distinguish a recessional moraine from a terminal moraine.

    Model answer

    A recessional moraine forms during pauses in glacial retreat, whereas a terminal moraine marks the furthest advance of the ice.

  5. 5

    Where is ground moraine deposited?

    Model answer

    Beneath the glacier, spread across the valley floor as the ice melts.

  6. 6

    Define a till plain.

    Model answer

    An extensive flat area of ground moraine deposited as a sheet of unsorted glacial sediment beneath or at the margin of an ice sheet.

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