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Dozens of active dust devils caught swirling across Mars canyon system

The European Space Agency's Mars Express has captured images of dozens of active dust devils in the Mamers Valles region of Mars. Dust devils on Mars form when the surface warms in sunlight, creating swirling columns of air that lift dust into the atmosphere. These phenomena are similar to terrestrial dust devils but much larger, reaching heights of up to 8 kilometers and speeds of 45 meters per second. The Mars Express uses its High Resolution Stereo Camera to detect movement by combining images from multiple camera channels.

Dust devils galore: Mars Express visits Mamers Valles on Mars. Credit: ESA/DLR/FU Berlin

The European Space Agency's Mars Express has captured part of Mars's Mamers Valles, a fascinating valley system speckled with brief, tornado-like whirlwinds known as dust devils.

Dust devils form as parts of Mars warm in the sun, causing the air just above the surface to swirl upward and carry dust with it. Mars's dust devils are similar to those seen in dry, dusty landscapes on Earth, but far larger. They tower up to 8 kilometers (5 miles) high, rove about for kilometers at a time, and reach top speeds of 45 meters per second. They play a key role in moving dust across the planet.

Mars Express is uniquely equipped to spot these mini whirlwinds. To form a single image using its High Resolution Stereo Camera—the instrument responsible for these new snapshots—the spacecraft combines sequential views from up to nine separate camera channels (which look at Mars in a different color, from a different direction, or a mix of the two). If nothing changes on the Martian surface while these are being taken, the multiple perspectives align—but if something is moving about, it stands out clearly from its surroundings.

In this new set of images, Mars Express captures not one but dozens of active dust devils. Click on the image below to see more than 30 circled, each visible as a small yellow dot with a pinkish trailing "shadow."

The alignment and combination of Mars Express's various camera channels also allow scientists to figure out the direction and speed of Mars's dust devils . This is something scientists have done using data from both Mars Express and ESA's ExoMars Trace Gas Orbiter, revealing how more than 1,000 of these tornado-like storms move—and tracing how winds sweep around the planet.

Topographic map of Mamers Valles on Mars. Credit: ESA/DLR/FU Berlin

Canyons and channels

Mamers Valles is a vast, broken-up, labyrinthine system of canyons and valleys etched into Mars's surface. The feature was named in 1976 based on the ancient Oscan language of pre-Roman Italy, with "Mamers" meaning "Mars" and "Valles" meaning "Valley."

These channels stretch out for around 1,000 km, crossing from Mars's ancient southern highlands into the planet's northern lowlands , and in places measure up to 25 km wide and 1.2 km deep (as shown most clearly in the associated topographical map below).

Surrounding these channels are various features: steep, flat hills known as mesas, sheer cliffs, and debris-covered glaciers. These glaciers contain water ice buried beneath a cover of rock and dust, and can be seen building up at the base of the steep slopes pictured here. All of these landforms come together to form fragmented or "fretted" terrain .

Bird’s-eye view of Mamers Valles. Credit: ESA/DLR/FU Berlin

Patches of dark material can also be seen lining a couple of the valleys—likely volcanic sands that either formed in place or were swept in by winds.

Many of the features seen here are signs of past activity related to water, lava or ice, all of which once flowed across this terrain and carved out telltale marks.

For instance, the valley floors are marked by long ridges and textures that formed as debris-covered glaciers slid down both sides of the valley, ultimately meeting in the middle. These same icy signatures line the steep cliffs and hillsides, too. Although water ice isn't stable on Mars's surface today, it has managed to survive here because it was covered by rocky material, which has stopped it from escaping to the Martian atmosphere.

Mamers Valles

Mars Express has visited this region of Mars before, imaging the areas surrounding both Mamers Valles (2008) and the neighboring Deuteronilus Mensae (2019).

The region dates to around 3.8 billion years ago, to a part of Martian history known as the late Noachian period . This era is significant because it marks when Mars began to transition from a warmer, wetter, more geologically active world to the cold, arid one seen today.

Decades of Mars exploration

This image comes courtesy of the HRSC camera, one of eight instruments aboard Mars Express. Mars Express has been capturing and exploring Mars's many landscapes since it launched in 2003. The orbiter has mapped the planet's surface at unprecedented resolution , in color and in three dimensions for more than two decades, returning insights that have drastically changed understanding of our planetary neighbor.

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Citation :

Dozens of active dust devils caught swirling across Mars canyon system (2026, June 17)

retrieved 17 June 2026

from https://phys.org/news/2026-06-dozens-devils-caught…

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Source document: European Space Agency (ESA)

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Phys.orgIndependentCenter4 days ago
Dozens of active dust devils caught swirling across Mars canyon system

The European Space Agency's Mars Express has captured images of dozens of active dust devils in the Mamers Valles region of Mars. Dust devils on Mars form when the surface warms in sunlight, creating swirling columns of air that lift dust into the atmosphere. These phenomena are similar to terrestrial dust devils but much larger, reaching heights of up to 8 kilometers and speeds of 45 meters per second. The Mars Express uses its High Resolution Stereo Camera to detect movement by combining images from multiple camera channels.

Bias read (Center): The article discusses scientific observations of natural phenomena on Mars, focusing on technical details of the Mars Express mission and the behavior of dust devils. There is no political framing, ideological emphasis, or biased language present. The content is purely descriptive and factual.

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