Massive Unseen Structures Found Beneath Mars' Surface

Challenging what we thought we knew about planetary geology

There’s a weird kind of silence happening on Mars. Researchers are seeing massive, unseen structures under the planet’s surface, but the top layer above them looks strangely undisturbed, like the ground never got the memo.

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That mismatch is throwing a wrench into the usual story of Mars as a “done” planet, with its volcanic era long over. The Tharsis region, home to towering volcanoes, is resurfaced relatively recently, and now a team led by Bart Root at Delft University of Technology thinks something deep is slowly pushing upward. At the same time, the study flags gravitational anomalies under Mars’ northern polar plains, buried beneath sediment tied to an ancient ocean floor.

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If Mars has been hiding active forces this whole time, Tharsis might not be finished.

Curiously, there’s no trace of those deep structures on the overlying surface, which implies that impactors didn’t form them.

That’s a significant finding. Until now, Mars has primarily been considered a dormant planet, with its volcanic activity long gone. But this new evidence suggests that something could still be bubbling beneath the crust, especially in the Tharsis region, which geologically resurfaced not so long ago (in planetary terms, at least), possibly within the last few tens of millions of years.

The team behind the research, led by Bart Root from Delft University of Technology, believes the structure is slowly pushing its way upward.

“A plume head is currently flowing upward towards the lithosphere to generate active volcanism in the geological future,” they explain.Curiously, there’s no trace of those deep structures on the overlying surface, which implies that impactors didn’t form them.Root et al.
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The whole thing gets stranger when those deep structures show up in the data, yet the surface above Tharsis refuses to show the usual impact-style fingerprints.

If this plume reaches the surface, it could eventually trigger new volcanic eruptions on Mars. And that’s not just speculation; the fact that Tharsis Montes is significantly more elevated than the surrounding regions hints that something deep underground is physically pushing it up.

This directly contradicts a long-standing idea in planetary geology known as flexural isostasy, which suggests that the weight of such prominent features should cause the crust to bend and sink, not rise.

“This means we need to rethink how we understand the support for the big volcano and its surroundings,” the researchers note.

And Tharsis isn’t the only place where strange phenomena are occurring beneath the Martian crust. The study also points to gravitational anomalies under Mars’ northern polar plains.

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These dense features are buried beneath what is believed to be sediment from an ancient ocean floor and are about 300 to 400 kg/m³ denser than the surrounding materials.

Then Bart Root’s team points to a plume head flowing toward the lithosphere, which would mean future volcanism could be brewing under the same mountains that already tower over everything.

Geological Implications

The Tharsis mystery also echoes how an AI firm refused a Pentagon contract over potential US military use.

Colourised Mars: Tharsis Montes trio with Olympus Mons to the northwest.

Similar gravitational anomalies have been linked to huge impact basins on Earth's Moon. The theory is that the asteroids or comets that created those basins were made of denser material than the Moon, and their remnants now sit below the surface. However, no trace of impact features above these new anomalies is visible on Mars.

“These dense structures could be volcanic in origin or could be compacted material due to ancient impacts,” said Dr. Root. Interestingly, one of the 20 features they identified even “resembles the shape of a dog.”“There seems to be no trace of them at the surface,” he continued. “However, through gravity data, we have a tantalizing glimpse into the older history of the northern hemisphere of Mars.”Colourised Mars: Tharsis Montes trio with Olympus Mons to the northwest.Arizona State University

And it gets personal for the geology, because the uplift story clashes with flexural isostasy, the idea that the crust should bend and sink under heavy features instead of rising.

Still, even with these exciting clues, researchers say they are only scratching the surface. They'll need better data to understand what’s going on down there; for that, they’re hoping to launch a new mission.

The proposed project is called Martian Quantum Gravity, or MaQuIs. It would use the same advanced gravitational mapping technology already employed on missions to study the Moon and Earth to get a clearer picture of what lies beneath Mars’ surface. “This would help us find out more about these mysterious hidden features and study ongoing mantle convection, as well as understand dynamic surface processes like atmospheric seasonal changes and the detection of groundwater reservoirs.”

Meanwhile, the northern polar plains add a second plot twist, with denser buried material tied to gravitational anomalies, like Mars is running two different hidden mysteries at once.

So, what does all this mean for Mars? It’s still too early to say for sure. But if the planet has an active mantle plume, or several, it could change everything we thought we knew about its geology, history, and future.

The revelation of massive, unseen structures beneath the surface of Mars signifies a transformative juncture in our understanding of planetary science. This unexpected find compels researchers to adopt a collaborative approach, merging insights from geology, geophysics, and astrobiology to unravel the mysteries surrounding these dense formations. The implications of this discovery could extend beyond Mars, as they may reshape our comprehension of planetary evolution and the conditions that could foster life.

As exploration efforts intensify, it is essential for scientists to prioritize transparency and communication in their research. Sharing findings not only enhances collective knowledge but also lays the groundwork for future explorations that may fundamentally alter our perception of Mars and its geological narrative.

Mars might be quiet on top, but something underneath is actively rearranging the rules.

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