Question

Difficulty: EasyLandform Development by Wind Action and Glaciation

Arrange the stages of barchan dune formation in an arid environment in sequential order from initial sand accumulation to the fully developed landform.

  1. 1Sand grains moving by saltation encounter an obstacle on a flat desert floor and begin to deposit.
  2. 2Sand accumulates into a mound featuring a gentle windward slope and a steep leeward slip face.
  3. 3Wind eddies around the edges of the mound advance sand faster at the margins, creating two horns pointing downwind.
  4. 4A mature crescent-shaped dune migrates continuously across the desert in the direction of the prevailing wind.

Answer

The correct sequence begins with sand encountering an obstacle and depositing, followed by the formation of a sand mound with a leeward slip face, the extension of lateral horns downwind by wind eddies, and finally the migration of a mature crescent-shaped barchan dune.
The correct sequence follows the physical progression of aeolian deposition: wind-blown sand first accumulates around an obstacle, forms an asymmetrical sand mound with a leeward slip face, develops two downwind-pointing horns as marginal sand moves faster than the center, and ultimately becomes a mobile crescent barchan dune.

Step-by-Step Solution

1
Identify the initial trigger for wind deposition.
Sand carried by saltation is trapped by an obstacle on the desert surface.
Aeolian deposition requires a physical barrier or reduction in wind energy.
2
Determine the initial structural dune development.
Sand accumulates into an asymmetrical mound with a gentle windward side and steep leeward slip face.
Sand accumulates on the windward slope and avalanches down the leeward side when it exceeds the angle of repose.
3
Trace the development of characteristic lateral features.
Lighter sand loads at the lateral margins move faster downwind, forming two pointed horns.
Eddy currents and lower resistance at the edges push the sides forward faster than the thick central core.
4
Identify the final landform state.
A fully formed crescent-shaped barchan dune migrates in the direction of the prevailing wind.
Ongoing wind action continually recycles sand over the crest, causing the entire dune to advance.

Key Concept

Barchan Dune Formation and Aeolian Deposition Processes
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