Kit Roberts
Scientists have found an interesting set of structures buried beneath the surface of Mars.
Now before you get too excited, no these are not 'structures' as in an alien colosseum or some sort of giant underground temple complex.
These are not artificial structures, but geological structures which formed over millions and millions of years.
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So if you were worried about a War of the Worlds style invasion or some sort of Alien vs Predator complex for extraterrestrials to do battle, you can relax.
But while the discovery by China's Zhurong rover may not be in the realms of science fiction, it does reveal some interesting details about Mars' past.
They might seem like innocuous structures, but bear with me as they are rather interesting.
So what are these weird structures found beneath the planet's surface?
Well, there are 16 polygonal structures. But what's interesting about the shapes is that scientists think that they were formed as a result of several 'freeze-thaw' cycles.
And if you're thinking that this suggests the substance doing the freezing and thawing was water, then you'd be correct.
Not only that, but the discovery could suggest that the process of sublimation, going directly from a solid to a gas, and freezing had been going on for millions of years.
The formation itself was around 35 metres beneath the surface of the Red Planet.
This suggested that there could have been floods in the area quite a long time ago.
We are talking a VERY long time here as well by the way, as in not even millions of years but billions of years.
Around three billion years to be precise, or as precise as that could be.
While the team of investigators wasn't sure precisely where the structure came from, they became confident that it would be formed by thermal processes caused by varying climates.
This is the main implication of the study, as freeze and thaw cycles imply that Mars had a potentially quite varied climate at one point.
The study authors said: “Occurring at low latitudes (∼25° N), the polygonal terrain, which is interpreted as having most likely formed by thermal contraction cracking, makes a compelling case for the high obliquity of early Mars.
"The subsurface structure with the covering materials overlying the buried palaeo-polygonal terrain suggests that there was a notable palaeoclimatic transformation some time thereafter."