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Dryland Landscapes

Barchans, linear dunes, star dunes, alluvial fans and bajadas

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  • Component 01

Overview

Recall questions on the conditions, shape and migration of barchans, slip faces, linear dunes and star dunes, alluvial fans and their sorting, bajadas, and fieldwork methods for measuring dune shape, barchan migration, fan sorting and geo-spatial mapping.

What you need to know

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Key term

Describe the form of a linear dune.

Key term

What conditions produce a barchan dune?

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    What conditions produce a barchan dune?

    Model answer

    A limited supply of sand lying on a firm, flat surface, combined with winds blowing consistently from a single direction, produces barchans.

  2. 2

    Describe the shape of a barchan.

    Model answer

    A barchan is crescent-shaped, with a gentle convex windward slope, a steep concave slip face on the lee side, and two horns extending downwind.

  3. 3

    Why do the horns of a barchan point downwind?

    Model answer

    The sand is thinner at the edges of the dune, so those parts are driven forward faster than the thicker, higher centre and become trailing horns.

  4. 4

    State the typical angle of a dune slip face.

    Model answer

    A slip face typically stands at about 32 to 34°, the angle of repose of dry sand.

  5. 5

    How does a barchan migrate?

    Model answer

    Sand saltates up the gentle windward slope to the crest and then avalanches down the lee slip face, so the whole dune advances downwind while keeping its shape.

  6. 6

    Why do smaller barchans migrate faster than larger ones?

    Model answer

    A small barchan contains far less sand, so the same rate of transfer across its crest shifts the whole dune further; small barchans may advance tens of metres a year while large ones move only a few.

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