Scientists Just ‘Looked’ Inside Mars. Here’s What They Found


InSight and Perseverance have sent back unprecedented data on everything from marsquakes to the Red Planet’s inner layers.

WHILE HUMANS HAVE been struggling to control the Covid-19 pandemic, baking in record heat, and trying to figure out how not to run out of water, our spacecraft on Mars have been enjoying a rather more tranquil existence. (Not needing to breathe helps.) Parked on the Martian surface, the InSight lander is listening for marsquakes, while the Perseverance rover is rolling around in search of life.

This week, scientists are dropping an Olympus Mons of findings from the two brave robots. In three papers published today in the journal Science—each authored by dozens of scientists from around the world—researchers detail the clever ways they used InSight’s seismometer to peer deep into the Red Planet, giving them an unprecedented understanding of its crustmantle, and core. It’s the first time scientists have mapped the interior of a planet other than Earth. And yesterday, another group of scientists held a press conference to announce early research results from Perseverance, and the next steps the rover will take to explore the surface of Jezero Crater, once a lake that could have been home to ancient microbial life.

Scientists still have a lot to learn about the Red Planet. “It’s built from similar building blocks as our own planet, but Mars looks very different,” says University of Cambridge global seismologist Sanne Cottaar, who penned a perspective paper in Science on the three new studies. “There’s lots of evidence that its evolution has been very different. And now forming this image of the layering of the planet will give us the tools to work out how this formed, how Mars came to be.”

Curiosities abound when comparing the two. Why, for instance, does Earth have a magnetic field, but Mars’ seems to have disappeared? Why are so many volcanoes spread all over Earth, while volcanoes are more localized—and bigger—on Mars? (At 374 miles in diameter and 16 miles high, Olympus Mons is the biggest known volcano in the solar system.) Its formation must have been cataclysmic, but the surface of Mars is now quiet; unlike Earth, it doesn’t seem to be volcanically active. (In May, though, scientists presented evidence of what they say is recent activity.) Only by peeking under the surface can scientists better understand these planetary oddities—and in doing so, better understand Earth’s own quirks as a fellow rocky planet.

But before we dive into today’s avalanche of scientific literature, we need a crash course on the workings of both Mars and its InSight observer. Compared to Earth, the Red Planet is geologically quite calm. Because our planet has plate tectonics—huge slabs of land that shift over the underlying mantle—the surface is positively popping with activity like volcanoes and catastrophic earthquakes. Mars lacks plate tectonics; it doesn’t have a plated surface, because its core formed and cooled off rapidly during its early days. Today it shakes with much smaller quakes that may come from the contracting of the planet as it continues to cool.

Critically, these S-waves are slower than P-waves, so when a quake pops off, they arrive at InSight’s seismometer a bit later. “This difference between the arrival of the P and S waves can give you an idea about what’s the location of the quake; how far it was away from your station,” says Knapmeyer-Endrun. The waves also differ in what mediums they can travel through, versus which ones they bounce off of. P-waves move through solids, liquids, and gases, while S-waves only travel through solids.

By analyzing the waves that reach InSight’s seismometer, scientists can get an idea of the composition of Mars’ insides. Since S-waves can’t travel through the liquid core, all of their energy bounces off the boundary between core and mantle. Think of it like binary code for computers: Just as two elements—ones and zeros—can combine to produce extremely complex programming, so too can two kinds of waves combine to produce a sophisticated picture of the Red Planet’s guts. “We also look at differences in arrival times, and then we can say, ‘OK, this tells us something about the thickness of the layer,’” says Knapmeyer-Endrun.

Using this technique, she and her colleagues were able to estimate the thickness of the crust. Previously, scientists had used satellites flying overhead to measure the differences in gravity and topography across the planet, and they had taken a stab at the crust’s thickness that way, landing on an estimate of a global average of 110 kilometers. “Now, with our measurements from inside, we can say that that’s definitely too much,” says Knapmeyer-Endrun. They now think the maximum figure for average thickness is 72 kilometers.

The researchers reckon that the crust is made of two or three layers. There’s a topmost layer that’s 10 kilometers thick, which InSight’s measurements revealed to be unexpectedly light, perhaps because it’s made of fractured rock left over from meteorite impacts. The layer below that goes down to about 20 kilometers. “Unfortunately, we are not sure what follows next, if it’s already the mantle or if we have a third layer in the crust. There’s some ambiguities that we haven’t resolved,” says Knapmeyer-Endrun. “We can definitely say that the crust is not as thick as has been predicted previously, and it has a lower density.”

Planetary seismologist Simon Stähler of ETH Zürich led the effort to characterize the hottest and innermost chunk of Mars’ interior—its core. Though they lack the ability to actually see inside the planetary center, Stähler’s team was able to extract some information just by analyzing the S-waves that bounce off the core-mantle boundary. These rumblings, unable to penetrate the liquid core, find their way back up to the Martian surface, where they are picked up by InSight’s receivers. “It takes a good 10 minutes,” Stähler says, from the time of the quake to the detection of the signal reflected by the core. By measuring this interval, his team was able to deduce how deep into the planet the waves are traveling, thus measuring the depth of the core itself: around 1,550 kilometers from the surface.

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