Ganymede and Callisto: Ice Worlds
Ganymede is the solar system's largest moon -- larger than the planet Mercury.
It consists of about half ice and half rock and metal. Grooves and ridges that
crisscross its surface indicate that it has undergone great changes over the
eons.
During several passes, the Galileo spacecraft saw mountains
of ice, plus sheets of ice that erupted from volcanoes. It also saw deep canyons
and broad, smooth plains created by the motions of Ganymede's crust.
Callisto
Like Europa, Callisto's icy surface may conceal an ocean. The case
for an ocean is more tentative, but it is bolstered by a huge basin on one
side of the moon. It was created by a powerful impact billions of years ago.
But there is no jumble
of rocks and mountains on the opposite side of Callisto, as there is with big
impact basins on our own moon. A deep ocean could have cushioned the impact,
preventing shock waves from piling up rocks half a world away.
Keywords
Galileo to Jupiter
Jupiter
Jupiter's Great Red Spot
Jupiter's Moons
Planetary Rings
Voyager Probes
This document was last modified: September 13, 2008
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