SUMMARY: When Galileo went past Jupiter's moon Io, it found parts of it reached temperatures as high as 1,610 degrees Celsius (2,910 Fahrenheit). The moon is so hot because it's continually being squeezed by Jupiter's immense gravity - the friction from the tidal interaction keeps it warm. Observations from Galileo and Earth-based telescopes have seen that the volcanoes are so hot they're vapourizing sodium, potassium, silicon and iron into the moon's atmosphere.
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