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Liquid lake on Mars might be evidence the Red Planet is still volcanically active


Last year we got some big news from the Red Planet – a huge lake of liquid water was apparently found beneath the ice at the Martian south pole. Building on that, a new study has now examined how it might have gotten there, and concluded that there has to be an underground heat source for water to pool there. For that to happen, Mars must have had volcanic activity much more recently than is normally believed, and may even still be active today.

Discovered using radar instruments onboard the Mars Express orbiter, the liquid lake sits under 1.5 km (0.9 mi) of solid ice, and stretches 20 km (12.4 mi). It's far from fresh though: huge amounts of sodium, magnesium and calcium salts are thought to be dissolved in it, which keeps it in a liquid state at temperatures well below water's usual freezing point.

But, the new study suggests, salt alone can't be solely responsible – there must have been some source of heat for the lake to form in the first place. And buried under that much ice, the heat could really only come from below. Here on Earth, liquid water pools under ice sheets thanks to heat from magma under the crust.

Decades of observations have shown that Mars was once a very volcanically active place, but it's generally believed to have been pretty quiet for the last few million years. For a lake of that size to still be present today, the researchers calculated that there must have been volcanic activity within the last 300,000 years or so, with magma collecting in a chamber some 10 km (6.2 mi) below the surface. And with activity that recently, geologically speaking, there's a chance it's still happening now.

"This would imply that there is still active magma chamber formation going on in the interior of Mars today and it is not just a cold, sort of dead place, internally," says Ali Bransom, co-lead author of the study.

Of course, the team acknowledges that the original discovery of the lake may have been the result of misinterpreted data, so there's a possibility that there is no water down there at all. But for the new work the researchers started by assuming there was, then working backwards to determine the conditions necessary for it to exist. And they are plausible.

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