Desert Sand Dunes


Sand dunes form some of the most spectacular land forms on earth. They are formed by small grains of sand accumulating. The move to a large extent through the force of the wind. Large sand dunes exist mainly in deserts but they can form along beaches and other places too, where there isn’t any vegetation that bind the sand granules together.

The Sahara Desert is the largest hot desert in the world (Antarctica is the largest cold desert and larger than Sahara). The northern part of Sahara was formed when the ice withdrew from Europe after the last ice age. Around 3,500 BC the monsoon moved south and the southern part of the Saharan desert was formed.

Sahara has large sand seas called ergs, but also gravel plains and salt flats and mountains. The sand dunes of all deserts move with the wind. The windward side has a gentle slope whereas the leeward side, the slip face, are steeper. You can see that on several of the photos in the gallery below. The sand dunes can move, often 10-15 metres per year.

I have photographed sand dunes in Sahara and Namibia but also to a small extent in the Gobi desert and in Argentina. Khongoryn Els in the Gobi Desert is famous for its singing dunes. When the wind blows, the sand granules move and create a singing sound.

In both Namibia and Sahara the sand contains a lot of iron giving it an orange or in Namibia even red colour. Namibia has some of the tallest sand dunes in the world reaching more than 300 metres up.


Leave a comment

Your email address will not be published. Required fields are marked *