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Dryland Landscapes

Wadis, canyons, pedestal rocks, ventifacts and desert pavements

  • 3 things to know
  • Component 01

Overview

Recall questions on how wadis and canyons form and stay steep, the Grand Canyon and the Colorado River, pedestal rocks and the processes that undercut them, ventifacts and dreikanters, and the competing explanations for desert pavements.

What you need to know

Answer each one before you reveal it.

Your recallNot started
Key term

How is a wadi both deepened and widened?

Key term

What is a canyon?

Process

Explain two processes that combine to undercut a pedestal rock.

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    What is a wadi?

    Model answer

    A wadi is a steep-sided, flat-floored desert valley that carries a stream only during and shortly after rainfall.

  2. 2

    How is a wadi both deepened and widened?

    Model answer

    Flash floods armed with coarse debris scour the bed by abrasion and undercut the valley sides, and the unsupported walls then collapse, so the channel widens as well as deepens.

  3. 3

    What kind of sediment is found on a wadi floor?

    Model answer

    It is poorly sorted and angular, ranging from boulders down to silt, because transport is short-lived and violent and gives the grains little time to be rounded or separated by size.

  4. 4

    What is a canyon?

    Model answer

    A canyon is a deep, narrow valley with very steep or vertical walls, cut by a river into rock strong enough to stand as cliffs.

  5. 5

    Why do canyon walls stay steep instead of being worn back to a gentle slope?

    Model answer

    Rainfall is far too low for widespread slope wash and soil creep, so the river incises downwards much faster than the valley sides can retreat.

  6. 6

    Name a canyon cut by an exotic river and give its approximate maximum depth.

    Model answer

    The Grand Canyon in Arizona, cut by the Colorado River, is up to about 1,800 m deep.

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