In geography, Barchans (also spelled Barkhans) are a specific and highly recognizable type of sand dune found in arid desert regions around the world. They are formed by the erosional and depositional action of wind.
Barchans are not just found on Earth! Satellites have photographed thousands of massive, perfect Barchan dunes on the surface of Mars, proving that the red planet has steady winds that shape its sandy surface.
A Barchan is a crescent-shaped (moon-shaped) sand dune.
If you look at a Barchan from above, it looks exactly like a crescent moon or the letter 'C'.
Barchans form in flat, dry deserts where the wind blows steadily from one constant direction and there is a limited supply of sand.
This is a classic geography exam question: Which way do the horns of a barchan point?
Answer: The horns always point downwind (in the direction the wind is blowing). If you are lost in the desert and see a barchan with its horns pointing South, you know the wind is blowing from North to South.
Barchans are found in almost all major deserts on Earth, including:
They are highly mobile dunes. A Barchan can 'walk' across the desert floor as the wind constantly moves sand from its back to its front, migrating several meters a year.
If the supply of sand increases, individual barchan dunes will merge together side-by-side to form long, wavy ridges of sand called **Barchanoid ridges** or Transverse dunes.
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