But the cold-ice-on-hot-planet phenomenon isn't as strange as our solar system diagrams might have us believe: Proximity to the sun doesn't fully determine planetary heat. Venus, second rock from the sun, is actually the one that takes "hottest planet" honors. And that's because Venus also has an atmosphere -- something Mercury lacks. And an atmosphere, Universe Today explains -- particularly one, like Venus's, that is enriched with lots of carbon dioxide -- acts like a planetary blanket, trapping heat under its mantle.

Which isn't to say that Mercury isn't also hot. Temperatures on the planet can reach a balmy 800 degrees Fahrenheit (427 degrees Celsius). But another thing that Mercury isn't is monolithic. Like Earth, its temperatures vary considerably according to, among other things, their orientation to the sun. And while the side of the planet that faces the sun can be sweltering, the side that faces away from it can drop to as low as 100 Kelvin, or -173 degrees Celsius. And the poles of the planet are permanently shielded from the sun's heat.

Ergo: ice. Lots of it, apparently. Evidence of large swaths of the substance is visible from a latitude of 85 degrees north up to Mercury's north pole, with smaller deposits scattered as far away as 65 degrees north. And there's a chance there's more where that came from. So NASA, Messenger instrument scientist Gregory Neumann said today, will direct Messenger's observation toward that area in the coming months -- when, that is, the angle of the sun allows. There's a further good chance that there's ice on the south pole of the planet, too. For now, though, Neumann put it, "there is an ongoing campaign, when the spacecraft permits, to look further northward."

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