Are sand dunes really alive?

National Parks Image Gallery Sand dunes aren't living things, but they have some characteristics that make them seem quite lively. See more amazing landscapes in these pictures of national parks.
Frans Lemmens/Getty Images

As Marco Polo crossed the Gobi Desert in the 13th century, he began to hear something -- and it seemed to be coming from the sand. When he was unable to come up with a logical explanation for the whistling, humming and booming sounds that haunted his ears, he blamed the noise on evil spirits. I mean, who else?

But Polo wasn't just hearing things. Sand dunes do sing. They also grow, migrate and reproduce. This behavior can make these otherwise colorless piles of grains seem almost lifelike.

A sand dune forms when wind blows a large amount of loose sand into an obstacle, like a rock or a tree. The heaviest grains of sand settle against the obstacle and start to form a small ridge or bump. The lighter grains deposit themselves on the other side of the obstacle, or the slip face. As long as the wind blows, the ridge of sand will continue to build until it becomes a dune. To learn more about this process, read How Sand Dunes Work.

Sand comes from rocks. When rocks erode over time, their pieces are picked up by wind, water or ice (as in glaciers). The most common ingredient in sand is quartz, also called silica. The makeup of sand will vary from place to place, too, depending on the makeup of the local rocks.

The question is, how could broken down rock come alive in the desert? Find out on the next page.

Sand Dune Singing, Breeding and Migrating

If this woman slid down the dune, perhaps it would sing for her.
If this woman slid down the dune, perhaps it would sing for her.
Martin Ruegner/Getty Images

Just like us, sand dunes grow. A sand dune can start out as small as a few hundred grains of sand settled against a pebble. And, with the right wind conditions, it can grow to several hundred feet tall. Depending on wind direction and velocity, a sand dune can spread out to form lovely ripples and patterns.

The wind also causes some dunes to migrate. That's right -- a sand dune can actually change locations. The air must be moving at at least 15 miles per hour (24 kpm) in order to transport sand grains. The grains bounce along the ground and bump into each other, moving themselves along. As sand piles up on a dune, eventually the dune becomes so steep that it collapses under its own weight. The sand at the top begins to avalanche down the dune's slip face. Once it slides down the face, it piles up anew on the other side. In this way, a sand dune can actually roll along while maintaining its original shape. Scientists call these dunes migrating dunes, and they're still trying to understand the exact physics behind them. Because migrating dunes can creep up and eventually envelop an entire village, it's important to know how they work.

Sand dunes, like us, can also reproduce. Of course, they don't need flowers and a romantic dinner to get things started. They just need wind. As sand dunes slowly move along, sometimes they cross paths and come together in a low-speed collision. And we mean it when we say "low speed" -- a collision can take up to an entire year to occur. If a small crescent-shaped dune collides with a bigger crescent-shaped dune, the smaller one may pass through and then break into two even smaller dunes on the other side. Researchers call this process breeding. Breeding happens when the dune is unstable -- the horns at the ends of a crescent-shaped dune will simply break off to become new baby dunes.

If you're still wondering why anyone would think a sand dune is alive, look no further than the phenomenon of booming dunes. People have reported hearing sand dunes sing, croak, burp, bark and moan. How does this happen? It's actually pretty simple. The noise we're hearing is the sound of sand grains rubbing against each other. The quality of sound produced depends on the size and texture of the grains.

For sand to make loud booming or humming noises, the grains must all be similar in size, rounded, dry and free of other particles. As we mentioned before, when sand accumulates at the top of a dune, it eventually reaches a tipping point and slides down the other side of the dune in a sand avalanche. The face of the dune acts like a speaker, amplifying the sound of the grains colliding. As the sand passes over itself, it produces vibrations that result in sounds like a cello or didgeridoo. Researchers have measured the noise levels, and some booming dunes reach up to 110 decibels -- as loud as a snow blower or motorcycle!

A sand dune breaks into song on its own as these sand avalanches occur, but you can also make a desert sand dune sing by sliding down its slope. You may even have heard sand squeak under your feet as you walk on the beach -- this is the same phenomenon but on a smaller scale.

For more information on sand dunes and other formations, visit the links on the following page.


Related HowStuffWorks Articles

More Great Links


  • Armstrong, Wayne P. "The Life & Love of Sand Dunes." Desert USA. 2008. (Oct. 15, 2008)
  • "How do sand dunes move?" White Sands National Monument. Dec. 22, 2004. (Oct. 27, 2008)
  • Inman, Mason. "The Secret of the Booming Dunes." Seed Magazine. July 26, 2006. (Nov. 3, 2008)
  • O'Connor, Anahad. "When Sand Dunes Collide, Sometimes They Mate and Multiply." NY Times. Dec. 23, 2003. (Oct. 15, 2008)
  • "Recipe for noisy sands." NOVA: Science Now. January 2005. (Oct. 27, 2008)
  • Schirber, Michael. "Singing Sand Dunes: The Mystery of Desert Music." Live Science. Jan. 11, 2005. (Nov. 3, 2008)
  • "What is sand made of?" SEED Science Center. 2008. (Oct. 15, 2008)