Proof is mounting {that a} secret lies beneath the dusty crimson plains of Mars, one that might redefine our view of the crimson planet: an enormous reservoir of liquid water, locked deep within the crust.
Mars is roofed in traces of historic our bodies of water. However the puzzle of precisely the place all of it went when the planet turned chilly and dry has lengthy intrigued scientists.
Our new examine might provide a solution. Utilizing seismic knowledge from NASA’s InSight mission, we uncovered proof that the seismic waves decelerate in a layer between 5.4 and eight kilometers under the floor, which might be due to the presence of liquid water at these depths.
The Thriller of the Lacking Water
Mars wasn’t at all times the barren desert we see at the moment. Billions of years in the past, throughout the Noachian and Hesperian durations (4.1 billion to three billion years in the past), rivers carved valleys and lakes shimmered.
As Mars’ magnetic subject pale and its environment thinned, most floor water vanished. Some escaped to area, some froze in polar caps, and a few was trapped in minerals, the place it stays at the moment.

4 billion years in the past (prime left), Mars might have hosted an enormous ocean. However the floor water has slowly disappeared, leaving solely frozen remnants close to the poles at the moment. Picture Credit score: NASA
However evaporation, freezing, and rocks can’t fairly account for all of the water that should have lined Mars within the distant previous. Calculations counsel the “lacking” water is sufficient to cowl the planet in an ocean at the very least 700 meters deep, and maybe as much as 900 meters deep.
One speculation has been that the lacking water seeped into the crust. Mars was closely bombarded by meteorites throughout the Noachian interval, which can have shaped fractures that channelled water underground.
Deep beneath the floor, hotter temperatures would hold the water in a liquid state—not like the frozen layers nearer the floor.
A Seismic Snapshot of Mars’ Crust
In 2018, NASA’s InSight lander touched down on Mars to hearken to the planet’s inside with a super-sensitive seismometer.
By finding out a selected form of vibration known as “shear waves,” we discovered a major underground anomaly: a layer between 5.4 and eight kilometers down the place these vibrations transfer extra slowly.
This “low-velocity layer” is most certainly extremely porous rock crammed with liquid water, like a saturated sponge. One thing like Earth’s aquifers, the place groundwater seeps into rock pores.
We calculated the “aquifer layer” on Mars might maintain sufficient water to cowl the planet in a world ocean 520–780 meters deep—a number of occasions as a lot water as is held in Antarctica’s ice sheet.
This quantity is appropriate with estimates of Mars’ “lacking” water (710–920 meters), after accounting for losses to area, water sure in minerals, and trendy ice caps.
Meteorites and Marsquakes
We made our discovery thanks to 2 meteorite impacts in 2021 (named S1000a and S1094b) and a marsquake in 2022 (dubbed S1222a). These occasions despatched seismic waves rippling by way of the crust, like dropping a stone right into a pond and watching the waves unfold.
InSight’s seismometer captured these vibrations. We used the high-frequency alerts from the occasions—consider tuning right into a crisp, high-definition radio station—to map the crust’s hidden layers.
We calculated “receiver features,” that are signatures of those waves as they bounce and reverberate between layers within the crust, like echoes mapping a cave. These signatures allow us to pinpoint boundaries the place rock modifications, revealing the water-soaked layer 5.4 to eight kilometers deep.
Why It Issues
Liquid water is important for all times as we all know it. On Earth, microbes thrive in deep, water-filled rock.
Might comparable life, maybe relics of historic Martian ecosystems, persist in these reservoirs? There’s just one solution to discover out.
The water could also be a lifeline for extra complicated organisms, too—reminiscent of future human explorers. Purified, it might present consuming water, oxygen, or gasoline for rockets.
In fact, drilling kilometers deep on a distant planet is a frightening problem. Nonetheless, our knowledge, collected close to Mars’ equator, additionally hints at the opportunity of different water-rich zones—such because the icy mud reservoir of Utopia Planitia.
What’s Subsequent for Mars Exploration?
Our seismic knowledge covers solely a slice of Mars. New missions with seismometers are wanted to map potential water layers throughout the remainder of the planet.
Future rovers or drills might someday faucet these reservoirs, analyzing their chemistry for traces of life. These water zones additionally require safety from Earthly microbes, as they might harbor native Martian biology.
For now, the water invitations us to maintain listening to Mars’ seismic heartbeat, decoding the secrets and techniques of a world maybe extra like Earth than we thought.
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