April 2, 2015 report
Jupiter moon Ganymede found to have a large bulge at equator
Ganymede was first observed by Galileo Galilei in 1610—since that time more has been learned about its characteristics—it is bigger than either Pluto or Mercury, for example, and nearly ¾ the size of Mars, which means were it to orbit the sun instead of a planet, it would be categorized as a planet itself. Scientists have also found that it has a metal core, covered by a rock mantle which is itself covered by a very thick sheet of ice. In this new observation, as Schenk was studying data from NASA's Galileo space probe—he noticed an unusual and previously unknown bulge on the moon's equator.
The researchers proposed at the conference that the bulge came about due to polar wandering—where ice built up at one of the poles and then slid over the top of an ocean below, to the equator, which provides more evidence for the existence of such an ocean (another team announced just two weeks ago that study of the moon's auroras had provided evidence of an ocean)—polar wandering can only happen if an ice cap sits atop something slippery, like an ocean—if that explanation holds true, than other researchers have pointed out that another similar bulge should exist on the other side of the moon, but we will not know if that is true until another space craft makes its way to the moon.
Ganymede was named after the boy (disguised to look like an eagle) carried to Olympus by Zeus, henceforth known as the cupbearer to the Olympian gods. Its discovery was among those that led to the idea that the planets orbit the sun, including ours, rather than the sun orbiting us.
© 2015 Phys.org