Anomaly•Registry
AR-0163

Booming Sand Dunes

Partially explained
Date Described for centuries. Studied scientifically since 1888; the mechanism has been disputed in print since 2007.
Location At least 40 desert dune sites worldwide, including sites in Morocco, Chile, China and California

Summary

Some desert dunes give out a loud, low hum when sand avalanches down their steep slip faces: a single note between about 70 and 110 hertz that can last for minutes. The groups that have measured it agree the avalanche makes the sound; they disagree, in print, about what sets the note.

One side says the pitch is fixed by the grains. The other says it is fixed by the layered structure of the dune. Each has published evidence against the other.

one note, 70 to 110 Hz. two published answers to what sets it THE GRAINS Andreotti 2004 Douady et al. 2006 Dagois-Bohy et al. 2012 pitch set by the grains: their size and how fast they slide past each other 2012: sang with no dune THE DUNE Vriend et al. 2007 Hunt and Vriend 2010 Vriend et al. 2015 pitch set by the depth of the loose surface layer: a waveguide note tracks layer depth THE AVALANCHE IS AGREED. THE NOTE IS NOT. 2008 comment: in the 2007 data the measured note does not track the predicted resonance. the 2007 authors replied. the registry found no study that settles it.
Figure Drawn by Anomaly Registry from Andreotti (2004), Douady et al. (2006), Vriend et al. (2007), the 2008 comment by Andreotti, Bonneau and Clément, Hunt and Vriend (2010), Dagois-Bohy et al. (2012) and Vriend et al. (2015). It sets the two published explanations of what fixes the note side by side: the grains, or the dune's loose surface layer.

What is documented

The sound. In a 2010 review, Melany Hunt and Nathalie Vriend of the California Institute of Technology describe dunes with "a remarkable capacity to produce sounds that are comparable with those from a stringed instrument." The sound follows an avalanche of sand down the slip face, the steep lee side of the dune. It occurs at "at least 40 sites around the world", has a dominant frequency between 70 and 110 hertz with higher harmonics, and, depending on the location and time of year, can continue for several minutes, even after the sand has stopped moving. The avalanche can be natural, or set off by people sliding down the slope.

The old accounts. Physicists writing on the subject usually begin with Marco Polo. Vriend's 2010 thesis quotes a translation of his account of desert spirits: "Even in the daytime their voices can sometimes be heard, or there is a clash of arms, a roll of drums or the sound of different musical instruments." The same thesis quotes a Chinese description of the Dunhuang district, dated to around 800, of a "Hill of Sounding Sand".

The first physics. Scientific explanations began in 1888, when Carus-Wilson attributed the sound to friction between grains and Bolton and Julien to a vibrating film of air (Vriend, 2010). In 1966 Ralph Bagnold, author of The Physics of Blown Sand and Desert Dunes, published "The shearing and dilatation of dry sand and the 'singing' mechanism" in the Proceedings of the Royal Society, tying the sound to the shearing of dry grains.

The grain explanation. In 2004 Bruno Andreotti, who had recorded booming at 100 hertz on a barchan dune in Morocco, proposed in Physical Review Letters that the note arises from "wave-particle mode locking" between the moving grains and elastic waves at the sand surface. In 2006 Stéphane Douady and colleagues compared several singing dunes, in Morocco and Chile, with two controlled avalanche experiments, one in the laboratory and one in the field. They concluded that "the frequency of the sound is the frequency of the relative motion of the sand grains", and that "the sound is produced because some moving grains synchronize their motions." In 2012 Simon Dagois-Bohy, Sylvain Courrech du Pont and Douady reported singing avalanches of sieved grains flowing down hard plates in the laboratory, with no dune beneath them, and concluded that a dune is not needed to produce the sound.

The dune explanation. In 2007 Vriend, Hunt and colleagues at Caltech published "Solving the mystery of booming sand dunes" in Geophysical Research Letters, based on field measurements at booming dunes in California. Their paper "challenges earlier reports that the dunes' frequency is a function of average grain size." They argued that the dune acts as a natural waveguide: the booming frequency "is fixed by the depth of the surficial layer of dry loose sand that is sandwiched between two regions of higher compressional body wave velocity." In 2015 Vriend, Hunt and Robert Clayton described booming as sound waves trapped in the dune's surface layer.

The dispute. Within weeks of the paper's publication, Andreotti and his colleagues Bonneau and Clément had posted a comment, published in the same journal in 2008. It states that the model Vriend's group used to analyse its seismic data "does not apply to the surface layer of sand dunes", that the frequency of booming avalanches "is not controlled by any resonance", and that Vriend's own data show no correlation between the measured frequency and the predicted resonant one. Vriend's group published a reply.

Leading explanations

Avalanching grains make the sound (agreed by all the groups cited here; established). Douady and colleagues summarise the older findings: the sound is "not due to the air flow around the dunes but to the motion of an avalanche", and comes from the grains' relative motion rather than from an acoustic excitation of the grains. Vriend's group agrees that the sound is produced by avalanching along the dune surface.

The grains set the pitch (Andreotti; Douady and colleagues; peer-reviewed, contested). On this view the frequency is set by how fast the grains in the flowing layer move past one another, which depends on grain size and gravity. The two groups differ on how the grains lock together: through surface waves, for Andreotti, and through a resonance within the flowing layer, for Douady. Their evidence includes the laboratory avalanches that sang without a dune.

The dune sets the pitch (Vriend, Hunt and colleagues; peer-reviewed, contested). On this view the avalanche is the source, but the dune's layered interior selects and sustains the note, as a waveguide or a resonating body would. Their evidence is field measurements of layer depth, wave speed and frequency at booming dunes, and the observation that the frequency varies with the layering from place to place and season to season.

What the popular version gets wrong

"The wind makes the dunes sing." The sound comes from sand moving down the slip face, after a natural slump or when people slide down the slope. Douady and colleagues state that it is not due to air flowing around the dunes.

"Marco Polo described singing sand dunes." The passage usually cited, in the translation physicists quote, attributes the voices, the clash of arms, the drums and the musical instruments to desert spirits, not to moving sand. Reading it as an account of booming dunes is a later interpretation, though one the physicists who study them make themselves.

"Scientists solved the mystery in 2007." A 2007 paper was titled "Solving the mystery of booming sand dunes". Within weeks a competing group had challenged its model, and in 2012 researchers on the grain side published avalanches that sang with no dune beneath them. There are two published solutions, and they rest on different causes.

Current status

Partially explained. What is settled: booming is produced by avalanching dry sand, as a single note of about 70 to 110 hertz with harmonics, and it needs neither wind nor spirits. What is not settled is what selects and sustains that note: the grains and the rate at which the flowing layer shears, or the structure of the dune beneath. Both explanations are published in peer-reviewed journals, and each side has published evidence against the other. The registry has found no later study, up to September 2026, that resolves the dispute. Measurements of grain size, layering and frequency made together, at the same dunes and across seasons, would be the kind of evidence that could.

Sources

  • Hunt, M. L. and Vriend, N. M. (2010). "Booming Sand Dunes." Annual Review of Earth and Planetary Sciences 38, 281 to 301.
  • Vriend, N. M., Hunt, M. L., Clayton, R. W., Brennen, C. E., Brantley, K. S. and Ruiz-Angulo, A. (2007). "Solving the mystery of booming sand dunes." Geophysical Research Letters 34(16).
  • Andreotti, B., Bonneau, L. and Clément, E. (2008). "Comment on 'Solving the mystery of booming sand dunes' by Nathalie M. Vriend et al." Geophysical Research Letters 35(8). Preprint arXiv:0710.1815.
  • Douady, S., Manning, A., Hersen, P., Elbelrhiti, H., Protière, S., Daerr, A. and Kabbachi, B. (2006). "Song of the Dunes as a Self-Synchronized Instrument." Physical Review Letters 97, 018002. Preprint arXiv:nlin/0412047.
  • Andreotti, B. (2004). "The Song of Dunes as a Wave-Particle Mode Locking." Physical Review Letters 93, 238001.
  • Dagois-Bohy, S., Courrech du Pont, S. and Douady, S. (2012). "Singing-sand avalanches without dunes." Geophysical Research Letters 39(20).
  • Vriend, N. M., Hunt, M. L. and Clayton, R. W. (2015). "Linear and nonlinear wave propagation in booming sand dunes." Physics of Fluids 27(10), 103305.
  • Bagnold, R. A. (1966). "The shearing and dilatation of dry sand and the 'singing' mechanism." Proceedings of the Royal Society of London, Series A 295(1442), 219 to 232.
  • Vriend, N. M. (2010). Booming Sand Dunes. PhD thesis, California Institute of Technology.

Last reviewed: September 2026. Records are provisional. Where the evidence changes, the entry changes. Found an error? Tell us.

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