Why Do Salt Deserts Have Honeycomb Patterns?

Table of Contents (click to expand)

Beneath a salt desert surface lurk layers of water. The honeycomb patterns form when water in the soil flows in the form of convection “rolls” below the sandy crust. This mechanism is similar to how hot and cold water circulate in a pan when it’s being heated.

Have you ever seen this strange pattern that forms across salt deserts?

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The surreal honeycomb patterns that sprawl across Salar de Uyuni in Bolivia, the world’s biggest salt flat. (Photo Credit : -Sara Winter/Shutterstock)

It may look like a mysterious, alien landscape from a sci-fi movie, but this is a real location—a giant salt flat (also known as a salt pan), The Salar de Uyuni in Bolivia was even used in shooting the battle scene in Star Wars: The Last Jedi. The beauty of the salt deserts fascinate tourists, researchers and movie-makers alike.

But how does the “honeycomb” pattern form in salt deserts around the world?

To get to the bottom of this, first, we must understand what a salt flat is.


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What Is A Salt Desert Flat And How Is It Formed?

Natural salt pans are flat areas of land, usually found in deserts, covered in large expanses of salts and other minerals. Salt flats were once water bodies (e.g., lakes or ponds). Due to a lack of rain for several years, the ground gets hotter. The water that cannot seep into the ground evaporates. Only particles of minerals and salts remain.

A salt pan usually shines like a dry white sea under the sun. The vastness of the terrain itself fills viewers with awe. The honeycomb pattern on top of it adds to the wonder… and has caused quite a bit of head-scratching.

star wars
A still of the salt planet in Star Wars: The Last Jedi. (Photo Credit : Star Wars: Episode VIII – The Last Jedi (2017))

A salt desert may seem to be bone-dry, but you’ll be surprised if you dig deep with your bare hands. You’d quickly reach a layer of water that lies in the soil right beneath the crust. However, that water is so salty that you can’t drink it!

Also Read: A Desert Is Covered With Sand, But What Is Beneath It?

Previous Attempts To Figure Out The Honeycomb Pattern

Many early studies suggested that when the salt crust becomes too dry, it begins to grow cracks, which cause these patterns to form. Another explanation was that when the salt crust swells too much, it bends under strain, without having enough space to grow, and crumbles into a network of honeycomb-like ridges.

However, none of these hypotheses could explain why the series of polygonal shapes look so alike all over the world, particularly in terms of how uniform they are in size and shape (always 1-2 meters/3-6 feet) and the pace at which they form.

The pattern remains the same, regardless of the differences in their environmental, geological or chemical features.

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Also Read: Why Are Deserts Hot And How Are They Formed?

Breaking Fresh Ground

Recently, a new study revealed that the honeycomb pattern in salt deserts may be caused by how the salty water moves below the sandy surface in desert soil.

So, how does it work?

We should all be familiar with how heated water ‘rolls’ in a circular motion. When water is heated, the hot water particles that are less dense well up to the surface, while the cooler and more dense water particles sink to the bottom. This circulation of hot and cold water in a boiling pan is known as a convection current.

In a similar way, a convection ‘roll’ of salt and fresh water takes place directly below the salt pans. This is triggered by the contrast in salinity (the amount of salts dissolved in different layers).

Convection Flow Is The Driving Force: The Way Of Water

Saltwater, as we know, is more dense than freshwater. Saltier water becomes heavier than the layer of water that lies directly below the ground in these salt pans. At a certain point, the saltier water sinks to the bottom and the less dense freshwater rises up from below. Thus, many rolling plumes of water sweep across the whole area, creating a uniform texture in the salt flats.

Proposed dynamics of patterned salt crusts
Mechanism behind the mysterious honeycomb patterns. (photo Credit Physical Review)

But why a polygon? Why not a circle?

If only a single roll occurred, we’d find a circular shape, but many such convection rolls happen next to each other at the same time. As a result, they are “squeezed” together, pushing one another into developing these hexagonal salt patterns. The salty water then sinks down along the edges of these structures.

In a salt desert, every one of these rolls or coils is 1-2 meters deep. That explains why the polygon-shaped structures have a diameter of 1-2 meters each.

In places where the salt content is very high, salt crystals are more prominent on the surface.

A Final Word

From Badwater Basin in California’s Death Valley National Park, Bonneville Salt Flats in Utah, to the Makgadikgadi Pan in Botswana, these surreal patterns of hexagonal shapes are a common feature. For years, it seemed like one of Mother Nature’s mysteries that couldn’t be cracked.

Looking at them, we can’t but wonder how nature creates such regularity and uniformity, even in the most barren and inhospitable lands. Now, it seems, we are much closer to the answer!


References (click to expand)
  1. Lasser, J., Nield, J. M., Ernst, M., Karius, V., Wiggs, G. F. S., Threadgold, M. R., … Goehring, L. (2023, February 24). Salt Polygons and Porous Media Convection. Physical Review X. American Physical Society (APS).
  2. Physical Geography | How Salt Shapes Our Lives. Saltassociation.co.uk
  3. M Buchanan. Why Death Valley Is Full of Polygons. American Physical Society
  4. Bonneville Salt Flats | Utah.com. Utah
  5. Death Valley - National Park Service. National Park Service
About the Author

Sudeshna is an English Literature Graduate from the University of Calcutta. She loves exploring the world through the lens of science. When not busy writing or pondering over cosmic quandaries, she can be found blithely catching some sun in her small backyard garden with her artist spouse and their fur baby, an Indie doggo.

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