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Hot Desert Systems and Landscapes

Deflation Hollows, Yardangs and Zeugen

  • 3 things to know
  • Component 1

Overview

Recall questions on how deflation strips fine sediment to form deflation hollows and desert pavements, on ventifacts, and on the differential erosion of softer and harder rock that shapes yardangs and undercuts zeugen beneath their cap rock.

What you need to know

Answer each one before you reveal it.

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Key term

What process removes loose, fine-grained sediment from the desert surface to form deflation hollows?

Key term

What is a desert pavement?

Key term

What role does harder rock play in yardang development?

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    What process removes loose, fine-grained sediment from the desert surface to form deflation hollows?

    Model answer

    Wind erosion removes fine particles from the surface.

  2. 2

    Why does coarser material remain at the surface during deflation hollow formation?

    Model answer

    Coarser material is too heavy for the wind to transport.

  3. 3

    How does a deflation hollow change over time as wind erosion continues?

    Model answer

    The depression deepens over time as more fine material is removed.

  4. 4

    What is a desert pavement?

    Model answer

    A surface of closely packed stones left behind after wind removes finer material, creating a protective armour layer.

  5. 5

    What are ventifacts?

    Model answer

    Rocks shaped and polished by wind-blown sand abrasion, often developing flat faces (facets) oriented toward prevailing winds.

  6. 6

    In yardang formation, what happens to softer rock compared to harder rock?

    Model answer

    Softer rock is eroded more rapidly than harder rock.

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AThe horns have less sand volume, so they move more quickly.
BSand is transported up the gentle windward slope via saltation.
CSand accumulates at the crest.

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Weathering means breakdown of rock in place.
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